In current usage, the term remote sensing generally refers to the use of satellite- or aircraft-based sensor technologies to detect and classify objects on Earth. It includes the surface and the atmosphere and oceans, based on propagated signals (e.g. electromagnetic radiation). It may be split into "active" remote sensing (when a signal is emitted by a satellite or aircraft to the object and its reflection is detected by the sensor) and "passive" remote sensing (when the reflection of sunlight is detected by the sensor). (Full article...)
Image 2
A yarder is piece of logging equipment that uses a system of cables to pull or fly logs from the stump to a collection point. It generally consists of an engine, drums, and spar, but has a range of configurations and variations, such as the swing yarder. (Full article...)
Image 3
Site index is a term used in forestry to describe the potential for foresttrees to grow at a particular location or "site". Site is defined as "The average age of dominate and/or codominate trees of an even-aged, undisturbed site of intolerant trees at a base age"; furthermore, the word site is used in forestry to refer to a distinct area where trees are found. Site index is used to measure the productivity of the site and the management options for that site and reports the height of dominant and co-dominant trees in a stand at a base age such as 25, 50 and 100 years. For example, a red oak with an age of 50 years and a height of 70 feet (21 m) will have a site index of 70. Site index is species specific. Common methods used to determine site index are based on tree height, plant composition and the use of soil maps. (Full article...)
Some creosote types were used historically as a treatment for components of seagoing and outdoor wood structures to prevent rot (e.g., bridgework and railroad ties, see image). Samples may be found commonly inside chimney flues, where the coal or wood burns under variable conditions, producing soot and tarry smoke. Creosotes are the principal chemicals responsible for the stability, scent, and flavor characteristic of smoked meat; the name is derived from Greekκρέας (kreas) 'meat' and σωτήρ (sōtēr) 'preserver'.
The two main kinds recognized in industry are coal-tar creosote and wood-tar creosote. The coal-tar variety, having stronger and more toxic properties, has chiefly been used as a preservative for wood; coal-tar creosote was also formerly used as an escharotic, to burn malignant skin tissue, and in dentistry, to prevent necrosis, before its carcinogenic properties became known. The wood-tar variety has been used for meat preservation, ship treatment, and such medical purposes as an anaesthetic, antiseptic, astringent, expectorant, and laxative, though these have mostly been replaced by modern formulations.
Varieties of creosote have also been made from both oil shale and petroleum, and are known as oil-tar creosote when derived from oil tar, and as water-gas-tar creosote when derived from the tar of water gas. Creosote also has been made from pre-coal formations such as lignite, yielding lignite-tar creosote, and peat, yielding peat-tar creosote. (Full article...)
Image 5
Tree planting is the process of transplanting tree seedlings, generally for forestry, land reclamation, or landscaping purposes. It differs from the transplantation of larger trees in arboriculture and from the lower-cost but slower and less reliable distribution of tree seeds. Trees contribute to their environment over long periods of time by improving air quality, climate amelioration, conserving water, preserving soil, and supporting wildlife. During the process of photosynthesis, trees take in carbon dioxide and produce oxygen.
In silviculture, the activity is known as "reforestation", or "afforestation," depending on whether the area being planted has recently been forested or not. It involves planting seedlings over an area of land where the forest has been harvested or damaged by fire, disease, or human activity. Trees are planted in many different parts of the world, and strategies may differ widely across nations and regions and among individual reforestation companies. Tree planting is grounded in forest science and, if performed properly, can result in the successful regeneration of a deforested area. However a planted forest rarely replicates the biodiversity and complexity of a natural forest.
Because trees remove carbon dioxide from the air as they grow, tree planting can be used to help limit climate change. Desert greening projects are also motivated by improved biodiversity and reclamation of natural water systems, as well as improved economic and social welfare due to an increased number of jobs in farming and forestry. (Full article...)
It allowed the United States General Land Office (GLO) to hire employees for the necessary administrative tasks and opened the reserves for public use.
It specifically stated the criteria for new forest reserve designations, which were timber production, watershed protection and forest protection.
This last item gave two separate branches of the Department of Interior responsibility-The GLO for the sale, claims and administration of the reserves and the USGS for the drawing of boundaries and land maps.
According to the Organic Act, the intention of the forest reservations was "to improve and protect the forest within the reservation, ... securing favorable conditions of water flows, and to furnish a continuous supply of timber for the use and necessities of citizens of the United States."
This law is one of two of the most important legislative events in US Forest Service history (the other being the Transfer Act of 1905). The nation now had forest reserves and the means to protect and manage them. The basic elements of federal forestry were now established. (Full article...)
Foresters work for the timber industry, government agencies, conservation groups, local authorities, urban parks boards, citizens' associations, and private landowners. The forestry profession includes a wide diversity of jobs, with educational requirements ranging from college bachelor's degrees to PhDs for highly specialized work.
Industrial foresters plan forest regeneration starting with careful harvesting. Urban foresters manage trees in urban green spaces. Foresters work in tree nurseries growing seedlings for woodland creation or regeneration projects. Foresters improve tree genetics. Forest engineers develop new building systems. Professional foresters measure and model the growth of forests with tools like geographic information systems. Foresters may combat insect infestation, disease, forest and grasslandwildfire, but increasingly allow these natural aspects of forest ecosystems to run their course when the likelihood of epidemics or risk of life or property are low. Increasingly, foresters participate in wildlife conservation planning and watershed protection. Foresters have been mainly concerned with timber management, especially reforestation, forests at prime conditions, and fire control.
Many people confuse the role of the forester with that of the logger, but most foresters are concerned not only with the harvest of timber, but also with the sustainable management of forests. The forester Jack C. Westoby remarked that "forestry is concerned not with trees, but with how trees can serve people". (Full article...)
Image 8
Dendrology (Ancient Greek: δένδρον, dendron, "tree"; and Ancient Greek: -λογία, -logia, science of or study of) or xylology (Ancient Greek: ξύλον, ksulon, "wood") is the science and study of woody plants (trees, shrubs, and lianas), specifically, their taxonomic classifications. There is no sharp boundary between plant taxonomy and dendrology; woody plants not only belong to many different plant families, but these families may be made up of both woody and non-woody members. Some families include only a few woody species. Dendrology, as a discipline of industrial forestry, tends to focus on identification of economically useful woody plants and their taxonomic interrelationships. As an academic course of study, dendrology will include all woody plants, native and non-native, that occur in a region. A related discipline is the study of sylvics, which focuses on the autecology of genera and species.
In the past, dendrology included the study of the natural history of woody species in specific regions, but this aspect is now considered part of ecology. The field also plays a role in conserving rare or endangered species. (Full article...)
In addition to wood fiber and plastic, WPCs can also contain other ligno-cellulosic and/or inorganic filler materials. WPCs are a subset of a larger category of materials called natural fiber plastic composites (NFPCs), which may contain no cellulose-based fiber fillers such as pulp fibers, peanut hulls, coffee husk, bamboo, straw, digestate, etc.
Chemical additives provide for integration of polymer and wood flour (powder) while facilitating optimal processing conditions. (Full article...)
Image 10
Stand density index (SDI; also known as Reineke's Stand Density Index after its founder) is a measure of the stocking of a stand of trees based on the number of trees per unit area and diameter at breast height (DBH) of the tree of average basal area, also known as the quadratic mean diameter. It may also be defined as the degree of crowding within stocked areas, using various growing space ratios based on crown length or diameter, tree height or diameter, and spacing. Stand density index is usually well correlated with stand volume and growth, and several variable-density yield tables have been created using it. Basal area, however, is usually satisfactory as a measure of stand density index and because it is easier to calculate it is usually preferred over SDI. Stand density index is also the basis for Stand density management diagrams. (Full article...)
Image 11
The Rainforest Alliance is an international non-governmental organization (NGO) with staff in more than 20 countries and operations in more than 70 countries. It was founded in 1987 by Daniel Katz, an American environmental activist, who serves as the chair of the board of directors. The NGO states that its mission is "to create a more sustainable world by using social and market forces to protect nature and improve the lives of farmers and forest communities." Its work includes the provision of an environmental certification for sustainability in agriculture. In parallel to its certification program, the Rainforest Alliance develops and implements long-term conservation and community development programs in a number of critically important tropical landscapes where commodity production threatens ecosystem health and the well-being of rural communities. (Full article...)
Image 12
The idea of an international organization for food and agriculture emerged in the late 19th and early 20th century, advanced primarily by Polish-born American agriculturalist and activist David Lubin. In May–June 1905, an international conference was held in Rome, Italy, which led to the creation of the International Institute of Agriculture (IIA) by the King of Italy, Victor Emmanuel III.
The IIA was the first intergovernmental organization to deal with the problems and challenges of agriculture on a global scale. It worked primarily to collect, compile, and publish data on agriculture, ranging from output statistics to a catalog of crop diseases. Among its achievements was the publication of the first agricultural census in 1930.
World War II effectively ended the IIA. During the war, in 1943, United States President Franklin D. Roosevelt called a League of Nations Conference on Food and Agriculture, which brought representatives from forty-four governments to The Omni Homestead Resort in Hot Springs, Virginia, from 18 May to 3 June to attend the Hot Springs Conference. The main impetus for the conference was the British-born Australian economist Frank L. McDougall, who since 1935 had advocated for an international forum to address hunger and malnutrition.
The Conference ended with a commitment to establish a permanent organization for food and agriculture, which was achieved on 16 October 1945 in Quebec City, Canada, following the Constitution of the Food and Agriculture Organization. The first session of the FAO Conference began the same day in the Château Frontenac in Quebec City and ended on 1 November 1945. This was led by Sir John Boyd Orr where his work on ending world hunger and creation of FAO resulted in him winning the Nobel Peace Prize in 1949.
After the war, the IIA was officially dissolved by resolution of its Permanent Committee on 27 February 1948. Its functions, facilities, and mandate were then transferred to the newly established FAO, which maintained its headquarters in Rome.
The FAO's initial functions supported agricultural and nutrition research and provided technical assistance to member countries to boost production in agriculture, fishery, and forestry. Beginning in the 1960s, it focused on efforts to develop high-yield strains of grain, eliminate protein deficiency, promote rural employment, and increase agricultural exports. The FAO recognized the decrease of these resources as an urgent problem in 1961 and created a joint collaboration with the International Biological Program (IBP) in 1967. To that end, it joined the UN General Assembly in creating the UN World Food Programme, the largest humanitarian organization addressing hunger and promoting food security.
The FAO launched what would become the FAO Money and Medals Programme (MMP) in 1968. FAO issued collector art medals in various series to bring attention to FAO's goals and missions. This program was responsible for over a hundred medal designs issued to the collecting public. A thirtieth anniversary medal of the MMP was issued in 1998.
In 1974, in response to famine in Africa, the FAO convened the first World Food Summit to address widespread hunger, malnutrition, and food insecurity. The meeting resulted in a proclamation that "every man, woman, and child has the inalienable right to be free from hunger and malnutrition to develop their physical and mental faculties" and a global commitment to eradicate these issues within a decade. A subsequent summit in 1996 addressed the shortcomings in achieving this goal while establishing a strategic plan for eliminating hunger and malnutrition into the 21st century.
Every year, FAO publishes a number of major 'State of the World' reports related to food, agriculture, forestry, fisheries and natural resources. (Full article...)
Image 13
Stephen C. Sillett (born March 19, 1968) is an American botanist specializing in old growth forest canopies. As the first scientist to enter the redwood forest canopy, he pioneered new methods for climbing, exploring, and studying tall trees. Sillett has climbed many of the world's tallest trees to study the plant and animal life residing in their crowns and is generally recognized as an authority on tall trees, especially redwoods (Sequoia sempervirens).
In forestry, thinning is the selective removal of trees, primarily undertaken to improve the growth rate or health of the remaining trees. Overcrowded trees are under competitive stress from their neighbors. Thinning may be done to increase the resistance of the stand to environmental stress such as drought, insect infestation, extreme temperature, or wildfire. (Full article...)
Image 15
Tree planting is the process of transplanting tree seedlings, generally for forestry, land reclamation, or landscaping purposes. It differs from the transplantation of larger trees in arboriculture and from the lower-cost but slower and less reliable distribution of tree seeds. Trees contribute to their environment over long periods of time by improving air quality, climate amelioration, conserving water, preserving soil, and supporting wildlife. During the process of photosynthesis, trees take in carbon dioxide and produce oxygen.
In silviculture, the activity is known as "reforestation", or "afforestation," depending on whether the area being planted has recently been forested or not. It involves planting seedlings over an area of land where the forest has been harvested or damaged by fire, disease, or human activity. Trees are planted in many different parts of the world, and strategies may differ widely across nations and regions and among individual reforestation companies. Tree planting is grounded in forest science and, if performed properly, can result in the successful regeneration of a deforested area. However a planted forest rarely replicates the biodiversity and complexity of a natural forest.
Because trees remove carbon dioxide from the air as they grow, tree planting can be used to help limit climate change. Desert greening projects are also motivated by improved biodiversity and reclamation of natural water systems, as well as improved economic and social welfare due to an increased number of jobs in farming and forestry. (Full article...)
Image 16
Haulage is the business of transporting goods by road or rail between suppliers and large consumer outlets, factories, warehouses, or depots. This includes everything humans might wish to move in bulk – from vegetables and other foodstuffs, to clothes, ore, coal, and other supplies. Haulage also involves the transportation of chemicals in large sealed containers, and the removal of waste. As the word implies, goods are loaded into large trailers or carriages and hauled between different locations. Traditionally, this was by large animals such as horses or oxen – where the practice may also be called cartage or drayage. However, in the modern age, this act is mostly performed by trains or trucks – with large shipping vessels acting as intermediaries for crossing oceans. Truck drivers on haulage shifts are typically male, and often work long and difficult hours with few breaks – regularly sleeping in their vehicles overnight and eating/showering at rest stops. It is expected that Vehicular automation will largely render human drivers obsolete within a few decades.
Haulage is also known as 'horizontal transport'. This contrasts with 'vertical transport' of the same such materials with cranes, known as hoisting. (Full article...)
The equivalent material in the sulfite process is usually called brown liquor, but the terms red liquor, thick liquor and sulfite liquor are also used. (Full article...)
Image 18
Resource Extraction Monitoring (REM) is a non-profit organisation that provides independent monitoring to ensure that laws relating to the extraction of natural resources are enforced. It was founded in 2003 by experts with over 15 years of monitoring experience. The head office is in the UK, with local offices in countries where major projects are taking place.
The organisation bridges the gap between governments, environmental and human rightsNGOs and local communities, donors and the private sector by providing objective and timely information on natural resource allocation and use. REM is not a lobbying organisation and has no political agenda, but is pro-active in researching and presenting the issue of governance and transparency during project implementation. (Full article...)
The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location. The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.
The general effect of elevation depends on atmospheric physics. However, the specific climate and ecology of any particular location depends on specific features of that location. This article provides a list of life zones by region, in order to illustrate the features of life zones for regions around the globe. (Full article...)
Taiga Rescue Network (TRN) was an international network of more than 200 non-governmental organizations, indigenous peoples and individuals working to defend the world's boreal forests, also known as Taiga. TRN was established in 1992 to give a voice to support, link and publicize local struggles fighting for the boreal forests and its peoples. TRN no longer exists. In 2010, TRN held its last conference in Sweden. The website remained online until April 2013. (Full article...)
High lead logging is a method of cable logging using a spar, yarder and loader. It was developed by Oscar Wirkkala. It is accomplished with two lines (cables) and two winches (or cable drums). The mainline or yarding line extends out from one winch, while a second usually lighter line called the haulback line extends out from the other winch to a 'tail block' or pulley at the tail (back) end of the logging site, and passes through the tail block and connects to the main line. Butt rigging is installed where the two lines join and the logs are hooked to the butt rigging with chokers. The procedure is to wind up the main line and the logs are pulled in, wind up the haulback and the butt rigging is pulled out for more logs or another 'turn'.
The "high lead" feature is added by elevating both lines near the winch or 'head' end. This is accomplished by running the lines through a block (pulley) called the "head block" because it is on the head end of the project. Early on, it was customary to trim and top a tree making it into a 'spar pole' or 'spar tree' for the purpose of supporting the head blocks but gradually the use of wooden spars gave way over the 20th century to the use of steel spars stood up for the purpose. In any event the spars are supported by a number of guy wires.
The reason for elevating the lines (cables) at the head end is to assist in pulling the logs free of obstructions on the ground. Also if the trees are being partially lifted as they are transported it is less disruptive to the ground which can be an environmental issue.
High lead is a popular method of logging on the West Coast of America.
The Forestry Library of the FAO Forestry Department, located at FAO headquarters in Rome and now part of the David Lubin Memorial Library, is a specialized library that holds approximately 6,000 books and over 600 current periodical titles, yearbooks and other serial titles on forestry and related areas. It also has a large collection of grey literature - including documentation on FAO forestry projects and papers and reports from various FAO Forestry meetings - much of which is not readily available anywhere else. (Full article...)
The RSPO was established following concerns raised by non-governmental organizations about environmental impacts resulting from palm oil production.
51,999,404 metric tonnes of palm oil produced in 2016 was RSPO certified. Products containing Certified Sustainable Palm Oil (CSPO) can carry the RSPO trademark. Members of the RSPO include palm oil producers, environmental groups, and manufacturers who use palm oil in their products. In 2014, Indonesia accounted for 40% of global palm oil production and 44% of the total RSPO-certified areas.
After the meeting in 2009, a number of environmental organisations were critical of the scope of the agreements reached. Palm oil growers who produce CSPO have been critical of the organization because, though they have met RSPO standards and assumed the costs associated with certification, the market demand for certified palm oil remains low. Even though deforestation has decreased in RSPO-certified oil palm plantations, peatlands continue to be drained and burned for the creation of new RSPO-certified palm plantations. Additionally, no mention to well-documented health effects of palm oil is made by the organization. (Full article...)
Image 6
The conservation movement, also known as nature conservation, is a political, environmental, and social movement that seeks to manage and protect natural resources, including animal, fungus, and plant species as well as their habitat for the future. Conservationists are concerned with leaving the environment in a better state than the condition they found it in. Evidence-based conservation seeks to use high quality scientific evidence to make conservation efforts more effective.
The early conservation movement evolved out of necessity to maintain natural resources such as fisheries, wildlife management, water, soil, as well as conservation and sustainable forestry. The contemporary conservation movement has broadened from the early movement's emphasis on use of sustainable yield of natural resources and preservation of wilderness areas to include preservation of biodiversity. Some say the conservation movement is part of the broader and more far-reaching environmental movement, while others argue that they differ both in ideology and practice. Conservation is seen as differing from environmentalism and it is generally a conservative school of thought which aims to preserve natural resources expressly for their continued sustainable use by humans. (Full article...)
Image 7
Forest Peoples Programme (FPP) advocates an alternative vision of how forests should be managed and controlled, based on respect for the rights of the people who know them best. FPP works with forest peoples in South America, Africa, and Asia, to help them secure their rights, build up their own organisations and negotiate with governments and companies as to how economic development and conservation are the best achieved on their lands.
Forests cover 31% of total land area of the planet. Of that, 12% are designated for the conservation of biological diversity and nearly all are inhabited. Many of the peoples, who live in and have customary rights to their forests, have developed ways of life and traditional knowledge that are attuned to their forest environments. Yet, forest policies commonly treat forests as empty lands controlled by the state and available for ‘development’ – colonisation, logging, plantations, dams, mines, oil wells, gas pipelines and agribusiness. These encroachments often force forest peoples out of their forest homes. Many conservation schemes to establish wilderness reserves also deny forest peoples’ rights. (Full article...)
Image 8
Water purification is the process of removing undesirable chemicals, biological contaminants, suspended solids, and gases from water. The goal is to produce water that is fit for specific purposes. Most water is purified and disinfected for human consumption (drinking water), but water purification may also be carried out for a variety of other purposes, including medical, pharmacological, chemical, and industrial applications. The history of water purification includes a wide variety of methods. The methods used include physical processes such as filtration, sedimentation, and distillation; biological processes such as slow sand filters or biologically active carbon; chemical processes such as flocculation and chlorination; and the use of electromagnetic radiation such as ultraviolet light.
Water purification can reduce the concentration of particulate matter including suspendedparticles, parasites, bacteria, algae, viruses, and fungi as well as reduce the concentration of a range of dissolved and particulate matter.
The standards for drinking water quality are typically set by governments or by international standards. These standards usually include minimum and maximum concentrations of contaminants, depending on the intended use of the water.
A visual inspection cannot determine if water is of appropriate quality. Simple procedures such as boiling or the use of a household point of use water filter (typically with activated carbon) are not sufficient for treating all possible contaminants that may be present in water from an unknown source. Even natural spring water—considered safe for all practical purposes in the 19th century—must now be tested before determining what kind of treatment, if any, is needed. Chemical and microbiological analysis, while expensive, are the only way to obtain the information necessary for deciding on the appropriate method of purification. (Full article...)
Image 9
Forests have always been important for economic development and environmental maintenance. In 1890, the International Agriculture and Forestry Congress in Vienna, Austria, proposed to establish a "central organ" for applied forest research in the European countries. As a consequence, the “International Union of Forest Experiment Organizations” was founded in Eberswalde, Germany, in 1892. Originally, only Austria, Germany and Switzerland agreed that their forest experiment stations would join the Union. By the beginning of World War I, stations from 22 countries, including USA, Canada and Japan, had become members.
During World War I international cooperation stopped, as did forest research in many of the countries involved in the war. The Union only fully resumed its activities in 1929 when the new name “International Union of Forestry Research Organizations” was adopted. In the years to follow, the organization lost its Central European character as more representatives from Africa, Asia and the Americas joined.
World War II reduced the activities of the Union to a minimum. Cooperation continued only between individuals, and not on an institutional basis. In 1949 the newly established Food and Agriculture Organization of the United Nations (FAO) declared its readiness to make available to IUFRO a secretariat at FAO’s own Headquarters in Rome. IUFRO has played a role in establishing standards and harmonizing field investigations in forest research. In 1903, the Union initiated international forestry bibliographies that did not exist earlier. Gradually the development led to the well-known Oxford System of Decimal Classification (ODe) for Forestry in the 1950s
The 1950s and 1960s were a period of steady growth. The XV IUFRO World Congress in Gainesville, USA, in 1971 was the first Congress held outside Europe. For the first time, it was referred to as a “World Congress,” and a Congress title was introduced: “The Role of Research in the Intensification of Forestry Practices and Activities.”
In the 1980s, IUFRO started to increasingly address forest-related social, economic, and ecological problems of global importance. The XVIII World Congress held in Ljubljana, Yugoslavia, in 1986 was the first to take place in Eastern Europe.
Since the 1990s the focus of the community of forest policymakers, economists and managers has changed. This is as societal expectations regarding forests broadened to include enhanced production of forest goods, social benefits, and environmental services through sustainable management of trees and forests. IUFRO responded to these challenges by adapting its scientific structure, expanding strategic partnerships and engaging more at the science/policy interface.
The XXI IUFRO World Congress in Kuala Lumpur, Malaysia, in 2000 was the first IUFRO World Congress to be held in a developing country. In 2000 the name of the Union was changed once more into “International Union of Forest Research Organizations”. The year 2000 also marked the first time in IUFRO´s history that gender issues were formally addressed. Over the last ten years, IUFRO undertook efforts to expand the scope of work beyond ‘traditional’ sectoral and disciplinary boundaries. At the 125th Anniversary Congress in 2017 in Freiburg, Germany, the slogan “Interconnecting Forests, Science and People” was adopted as part of the logo. (Full article...)
FSC is a global forest certification system established for forests and forest products. According to the council, the use of the FSC logo signifies that a product comes from environmentally, socially, and economically responsible sources. In addition to its global certification standard, FSC develops national standards in selected countries. The FSC has 10 Principles and associated Criteria (FSC P&C) that form the basis for all FSC standards and certification.
The Korea Forest Service is a central administrative agency under the Ministry of Agriculture, Food and Rural Affairs (MAFR), responsible for protecting and nurturing forests, increasing forest resources, developing forest products, conducting research on forest management and improvement, and is located in Daejeon Government Complex. In the past, during the national forestation campaign from 1973 to 1986, it was temporarily under the Ministry of Home Affairs (now the Ministry of the Interior and Safety), but returned to the Ministry of Agriculture, Forestry and Fisheries in 1987. However, as the agency's work was focused solely on maintaining and managing successful national forestation policies, questions were raised about its necessity for a period of time. Currently, the agency has transformed its identity into one that strives to generate continuous income through forest resources.
It is one of the government agencies that is highly likely to expand in the event of future North-South unification. In North Korea, there are many mountains, and it is expected that regional forest offices will be expanded to promote afforestation projects centering around Mount Mindungsan.
The Korea National Park Service, which is under the Ministry of Environment, had a long-standing conflict with the Korea Forest Service. Both agencies are in charge of forest-related work, but there were frequent conflicts due to differences in specific business objectives. While the Korea Forest Service also invests in forest development to promote forestry, the Korea National Park Service's primary objective is forest protection. Therefore, in 2012, an article was published between the two organization called "Let's Get Along."
Furthermore, it has a cooperative relationship with the Cultural Heritage Administration. High-quality lumber is essential for restoring, maintaining, and repairing traditional cultural properties, and in particular, Korean pine, also known as the "Geumgang Pine," is still a rare species. Therefore, the Korea Forest Service and the Cultural Heritage Administration are working together to create and manage Geumgang Pine plantations.
The current head of the organization is Nam Sung-hyun, who began his term in May 2022. (Full article...)
It allowed the United States General Land Office (GLO) to hire employees for the necessary administrative tasks and opened the reserves for public use.
It specifically stated the criteria for new forest reserve designations, which were timber production, watershed protection and forest protection.
This last item gave two separate branches of the Department of Interior responsibility-The GLO for the sale, claims and administration of the reserves and the USGS for the drawing of boundaries and land maps.
According to the Organic Act, the intention of the forest reservations was "to improve and protect the forest within the reservation, ... securing favorable conditions of water flows, and to furnish a continuous supply of timber for the use and necessities of citizens of the United States."
This law is one of two of the most important legislative events in US Forest Service history (the other being the Transfer Act of 1905). The nation now had forest reserves and the means to protect and manage them. The basic elements of federal forestry were now established. (Full article...)
Image 15
Tree planting is the process of transplanting tree seedlings, generally for forestry, land reclamation, or landscaping purposes. It differs from the transplantation of larger trees in arboriculture and from the lower-cost but slower and less reliable distribution of tree seeds. Trees contribute to their environment over long periods of time by improving air quality, climate amelioration, conserving water, preserving soil, and supporting wildlife. During the process of photosynthesis, trees take in carbon dioxide and produce oxygen.
In silviculture, the activity is known as "reforestation", or "afforestation," depending on whether the area being planted has recently been forested or not. It involves planting seedlings over an area of land where the forest has been harvested or damaged by fire, disease, or human activity. Trees are planted in many different parts of the world, and strategies may differ widely across nations and regions and among individual reforestation companies. Tree planting is grounded in forest science and, if performed properly, can result in the successful regeneration of a deforested area. However a planted forest rarely replicates the biodiversity and complexity of a natural forest.
Because trees remove carbon dioxide from the air as they grow, tree planting can be used to help limit climate change. Desert greening projects are also motivated by improved biodiversity and reclamation of natural water systems, as well as improved economic and social welfare due to an increased number of jobs in farming and forestry. (Full article...)
Image 16
The log scaler is an occupation in the timber industry. The Log Scaler measures the cut trees to determine the scale (volume) and quality (grade) of the wood to be used for manufacturing. When logs are sold, in order to determine the basis for a sale price in a standard way, the logs are "scaled" which means they are measured, identified as to species, and deductions for defects assigned to produce a net volume of merchantable wood. There are several different scales or rules that are used to determine the volume of wood. Scribner Decimal C rule is based on diagrams of circles that show the number of boards that will be utilized from the diameters of logs. The cubic rule, often called Metric in Canada, determines the cubic volume of the log material. The logs are recorded as gross scale (actual log measurements, length and diameter) and net scale (volume after deductions for defects are taken out). This occupation is usually performed by a third party organization qualified to "scale" government timber. Since internal defects are determined by external indications, scaling is not an exact science and is subject to interpretation of log scaling rules. The log scaler is subject to random "check scales" in which another scaler rescales exactly the same logs and the results are compared. The log scaler must be within + or - 1% of the gross scale and + or - 2% of the net scale to keep their certification to scale. The scale is used for payment, quality control and inventory purposes. (Full article...)
Image 17
Paperboard is a thick paper-based material. While there is no rigid differentiation between paper and paperboard, paperboard is generally thicker (usually over 0.30 mm, 0.012 in, or 12 points) than paper and has certain superior attributes such as foldability and rigidity. According to ISO standards, paperboard is a paper with a grammage above 250 g/m2, but there are exceptions. Paperboard can be single- or multi-ply.
Paperboard can be easily cut and formed, is lightweight, and because it is strong, is used in packaging. Another end-use is high quality graphic printing, such as book and magazine covers or postcards. Paperboard is also used in fine arts for creating sculptures.
Sometimes it is referred to as cardboard, which is a generic, lay term used to refer to any heavy paper pulp–based board, however this usage is deprecated in the paper, printing, and packaging industries as it does not adequately describe each product type. (Full article...)
Image 18
The mean annual increment (MAI) or mean annual growth refers to the average growth per year a tree or stand of trees has exhibited/experienced up to a specified age. For example, a 20-year-old tree that has a stem volume of 0.2 m3 has an MAI of 0.01 m3/year. MAI is calculated as where = yield at time . For a stand of trees the total stem volume (m3) per area (ha) is typically calculated. Because the typical growth pattern of a forest is sigmoidal, the MAI starts out small, increases to a maximum value as the trees mature, then declines slowly over time as some trees' canopies face competition for sunlight and older trees die off.
Throughout this, the MAI always remains positive. MAI differs from periodic annual increment (PAI) in that the PAI is the growth for one specific year or any other specified length of time. The point where the MAI and PAI meet is at the point of maximum MAI and is typically referred to as the biologically optimal rotation age. This is the age at which the tree or stand would be harvested if the management objective is to maximize long-term yield. The proof of this definition is shown by differentiating with respect to , and is shown by Husch, Miller, and Beers. (Full article...)
The success of agriculture during the Estado Novo (New State), with Getúlio Vargas, led to the expression, "Brazil, breadbasket of the world".
The southern one-half to two-thirds of Brazil has a semi-temperate climate, higher rainfall, more fertile soil, more advanced technology and input use, adequate infrastructure and more experienced farmers. This region produces most of Brazil's grains, oilseeds, and agriculture exports.
The drought-ridden northeast region and Amazon basin lack well-distributed rainfall, good soil, adequate infrastructure and development capital. Although mostly occupied by subsistence farmers, both regions are increasingly important as exporters of forest products, cocoa and tropical fruits. Central Brazil contains substantial areas of grassland. Brazilian grasslands are far less fertile than those of North America, and are generally suited only for grazing.
A forwarder is a forestry vehicle that carries big felledlogs cut by a harvester from the stump to a roadside landing for later acquisition. Forwarders can use rubber tires or tracks. Unlike a skidder, a forwarder carries logs clear of the ground, which can reduce soil impacts but tends to limit the size of the logs it can move. Forwarders are typically employed together with harvesters in cut-to-length logging operations. Forwarders originated in Scandinavia. (Full article...)
Biologic carbon sequestration is a naturally occurring process as part of the carbon cycle. Humans can enhance it through deliberate actions and use of technology. Carbon dioxide (CO 2) is naturally captured from the atmosphere through biological, chemical, and physical processes. These processes can be accelerated for example through changes in land use and agricultural practices, called carbon farming. Artificial processes have also been devised to produce similar effects. This approach is called carbon capture and storage. It involves using technology to capture and sequester (store) CO 2 that is produced from human activities underground or under the sea bed.
Plants, such as forests and kelp beds, absorb carbon dioxide from the air as they grow, and bind it into biomass. However, these biological stores may be temporary carbon sinks, as long-term sequestration cannot be guaranteed. Wildfires, disease, economic pressures, and changing political priorities may release the sequestered carbon back into the atmosphere.
Carbon dioxide that has been removed from the atmosphere can also be stored in the Earth's crust by injecting it underground, or in the form of insolublecarbonate salts. The latter process is called mineral sequestration. These methods are considered non-volatile because they not only remove carbon dioxide from the atmosphere but also sequester it indefinitely. This means the carbon is "locked away" for thousands to millions of years.
To enhance carbon sequestration processes in oceans the following chemical or physical technologies have been proposed: ocean fertilization, artificial upwelling, basalt storage, mineralization and deep-sea sediments, and adding bases to neutralize acids. However, none have achieved large scale application so far. Large-scale seaweed farming on the other hand is a biological process and could sequester significant amounts of carbon. The potential growth of seaweed for carbon farming would see the harvested seaweed transported to the deep ocean for long-term burial. The IPCC Special Report on the Ocean and Cryosphere in a Changing Climate recommends "further research attention" on seaweed farming as a mitigation tactic. (Full article...)
Image 22
The Global Positioning System (GPS), originally Navstar GPS, is a satellite-based radio navigation system owned by the United States Space Force and operated by Mission Delta 31. It is one of the global navigation satellite systems (GNSS) that provide geolocation and time information to a GPS receiver anywhere on or near the Earth where there is an unobstructed line of sight to four or more GPS satellites. It does not require the user to transmit any data, and operates independently of any telephone or Internet reception, though these technologies can enhance the usefulness of the GPS positioning information. It provides critical positioning capabilities to military, civil, and commercial users around the world. Although the United States government created, controls, and maintains the GPS system, it is freely accessible to anyone with a GPS receiver. (Full article...)
The largetooth cookiecutter shark (Isistius plutodus) is a rare species of squaliform shark in the familyDalatiidae, reported from depths of 60–200 m (200–660 ft) at scattered locations in the Atlantic and Pacific Oceans. As its common name suggests, it is similar in appearance to the cookiecutter shark (I. brasiliensis) but has much larger lower teeth. This species reaches a maximum known length of 42 cm (17 in). The largetooth cookiecutter shark feeds by gouging out chunks of flesh from larger animals, including bony fishes, sharks, and marine mammals, and is able to take larger bites than I. brasiliensis. Little is known of its life history; it is thought to be a weaker swimmer than I. brasiliensis, and is presumably aplacental viviparous like the rest of its family. This shark is an infrequent bycatch of commercial trawl and longlinefisheries, but is not thought to be much threatened by these activities. (Full article...)
The Burmese bamboo shark, Chiloscyllium burmensis, is an extremely rare bamboo shark in the familyHemiscylliidae. The first specimen was caught in 1963 off the coast from Rangoon in Myanmar (known as Burma at the time) in a depth of 29 – 33 m. This holotype is an adult male, 57 cm long and kept in the National Museum of Natural History, Smithsonian Institution, Washington DC. Later, three more specimens, two males and one female, were recorded in 2018 from the Bangladesh Fisheries Development Corporation Fish Landing Center of Cox’s Bazar. (Full article...)
Image 5
The Carolina hammerhead (Sphyrna gilberti) is a species of hammerhead shark, and part of the familySphyrnidae, found in the western Atlantic Ocean. Their pupping grounds are in nearshore waters off the southeastern U.S. with the highest concentrations found in Bulls Bay, South Carolina. The Carolina hammerhead has also been found in nearshore waters off of Brazil. It was formally described in 2013. It is currently classified as Vulnerable (VU) on the IUCN Red List due to overfishing and habitat degradation.
Little is known about the habits of the species. It is a sister species to S. lewini. The Carolina hammerhead is named in honor of Carter Gilbert, who unknowingly recorded the first known specimen of the shark off Charleston, South Carolina, in 1967. Dr. Gilbert, who was the curator of the Florida Museum of Natural History from 1961 to 1998, caught what he believed was an anomalous scalloped hammerhead shark with 10 fewer vertebrae than a typical scalloped hammerhead. It was not confirmed to be a different species altogether until Quattro's discovery in 2013. The general diet of the Carolina hammerheads consists of bony fishes and cephalopods such as squids, octopuses, and cuttlefishes. They also feed on shrimps, lobsters, crabs, and other smaller sharks and rays. (Full article...)
The bigeyed sixgill shark (Hexanchus nakamurai) is a cow shark of the familyHexanchidae. Its dorsal surface has a brownish-gray color, and is sharply separated from the light coloring of its ventral surface. The eyes are a fluorescent green while the shark is alive. The body of this shark is small, slim, and fusiform in shape. As the name suggests, this shark has six gill slits, unusual among most shark species. The head is narrow and somewhat flattened, and the mouth contains 5 rows of large, comb-shaped teeth. This shark's single dorsal fin is pushed back towards the caudal fin, and is behind the pelvic fins. The upper caudal fin is much longer than the lower, with a deep notch near the tip. All fins have thin white margins on the edge. In juveniles, the upper caudal fin has a black tip. (Full article...)
Image 8
The bull shark (Carcharhinus leucas), also known as the Zambezi shark (informally zambi) in Africa and Lake Nicaragua shark in Nicaragua, is a species of requiem shark commonly found worldwide in warm, shallow waters along coasts and in rivers. It is known for its aggressive nature, and presence mainly in warm, shallow brackish and freshwater systems including estuaries and (usually) lower reaches of rivers. Their aggressive nature has led to ongoing shark-culling efforts near beaches to protect beachgoers, which is one of the causes of bull shark populations continuing to decrease. Bull sharks are currently listed as vulnerable on the IUCN Red List.
Bull sharks are euryhaline and can thrive in both salt and fresh water. They are known to travel far up rivers, and have been known to travel up the Mississippi River as far as Alton, Illinois, about 1,100 kilometres (700 mi) from the ocean, but few freshwater interactions with humans have been recorded. Larger-sized bull sharks are probably responsible for the majority of nearshoreshark attacks, including many incidents of shark bites attributed to other species.
Unlike the river sharks of the genus Glyphis, bull sharks are not true freshwater sharks, despite their ability to survive in freshwater habitats.
The longhead catshark or smoothbelly catshark (Apristurus longicephalus) is a species of shark, familyPentanchidae, the deepwater catsharks. This shark has a patchy distribution in the Indo-Pacific from Mozambique to southern Japan to northern Australia. It is found in water between 500 and 1,140 m (1,640 and 3,740 ft) deep. This species grows to 59 cm (23 in) long and is characterized by its extremely long and narrow snout, short abdomen, and long anal and caudal fins. In addition, a large area of the anterior ventral portion of its body lacks dermal denticles. The longhead catshark is oviparous and the only known cartilaginous fish that is normally hermaphroditic, with the majority of individuals having both the functional reproductive organs of one sex and the undeveloped reproductive organs of the opposite sex. (Full article...)
Image 11
The broadnose catshark (Apristurus investigatoris) is a shark of the familyPentanchidae, the deepwater catsharks. The holotype and only specimen being found in deep water in the Andaman Sea in the Indian Ocean between 16 and 10°N. Its length is around 26 cm, although this measurement was taken from an immature specimen. The reproduction of this catshark is oviparous. The threats are not exactly known but it may be deepwater fisheries. (Full article...)
The whitetail dogfish is a rare species known only from a few specimens taken by tunalongliners and trawlers. The dorsal fins are small, the pectoral fins are angular, and there is an asymmetric caudal fin with a dark-tipped upper lobe. Coloration is grey and white, mottled with large brown or black spots, the tail mostly white with black tips.
The splendid lanternshark (Etmopterus splendidus) is a shark of the familyEtmopteridae found in the western Pacific at depths between 120 and 210 m. Through the classification of Etmopterus species into several clades based on the positioning of their bioluminescent photophores, the splendid lanternshark can be considered a member of the Etmopterus pusillus clade.
Squalidae, more commonly known as dogfish, dog sharks, or spiny dogfish, are one of several families of sharks categorized under Squaliformes, making it the second largest order of sharks, numbering 119 species across 7 families. Having earned their name after a group of fishermen reportedly observed the species chasing down smaller fish in dog-like packs, dogfish have slender, streamlined bodies, usually more compact in comparison to other species, and a pointed snout. Dogfish likewise have two dorsal fins, each with smooth spines, but no anal fin, and their skin is generally rough to the touch. As the species reaches adulthood, males usually measure a maximum of 100 cm (39 inches), while females typically measure 125 cm (49 inches) long. The species therefore exhibits female-dominant sexual dimorphism.
Dogfish sharks have slate-grey or grey-brown skin with white dots that becomes paler (almost white) around the belly region. These sharks are characterized by teeth in upper and lower jaws similar in size; a caudal peduncle with lateral keels; the upper precaudal pit usually is present; and the caudal fin is without a subterminal notch.
They are carnivorous, principally preying upon organisms smaller than themselves. Some of their prey include herring, mackerel, and capelin. In special cases, they may consume jellyfish and squid. Even at a young age, spiny dogfish pups may hunt fish two or three times their size. Unlike virtually all other shark species, dogfish sharks possess venom which coats their dorsal spines; this venom is mildly toxic to humans and would be harmful if the shark were to be mishandled. The livers and stomachs of the Squalidae contain the compound squalamine, which possesses the property of reduction of small blood vessel growth in humans. Dogfish sharks use their strong jaw and sharp teeth to consume their prey.
The spiny dogfish has broken several records in the areas of migration and gestation. This shark tends to be a highly migratory species: one shark was recorded as travelling 8,000 km (5,000 miles) after being tagged in Washington state, United States, and found again later in Japan. In addition to its long distance migration, the spiny shark holds the record for longest gestation period of any other vertebrate at 22–24 months. Females produce eggs and give birth to live young that measure to be 20–33 cm (8–13 inches). The mating cycle of Squalidae consists of multiple paternity, where multiple males can fertilize a single litter. This allows for increased genetic variation, which is essential for the conservation of the species, given their susceptibility to fishing. (Full article...)
Image 16
The necklace carpetshark (Parascyllium variolatum), also known as the varied carpetshark, is a carpetshark of the familyParascylliidaeendemic to the waters off Australia's southern coast between latitudes37°S and 41°S. It is found near the ocean floor over sand, rock, coral reefs, and kelp and seagrass beds at depths down to 180 m (590 ft). It is almost exclusively seen at night and spends the day hidden in caves or camouflaged on the ocean floor.
With a slender, elongated body and a maximum length of only 91.0 cm TL, it is harmless to humans. The tail is long, but difficult to tell apart from the rest of the shark. Its body is grey to brown in color with a broad black collar, from which it gets its name, and white spots along its body. It has small spiracles and nostrils with short barbels, likely used for sensory purposes. It is often mistaken for a species of catshark, despite being more closely related to wobbegongs and nurse sharks.
It is a nocturnalpredator and feeds mostly on shellfish. Reproduction is oviparous with females laying eggs with curled tendrils that anchor them to the ocean floor. The embryos feed on yolk. (Full article...)
Image 17
The longfin mako shark (Isurus paucus) is a species of mackerel shark in the family Lamnidae, with a probable worldwide distribution in temperate and tropical waters. An uncommon species, it is typically lumped together under the name "mako" with its better-known relative, the shortfin mako shark (I. oxyrinchus). The longfin mako is a pelagic species found in moderately deep water, having been reported to a depth of 220 m (720 ft). Growing to a maximum length of 4.3 m (14 ft), the slimmer build and long, broad pectoral fins of this shark suggest that it is a slower and less active swimmer than the shortfin mako.
Longfin mako sharks are predators that feed on small schoolingbony fishes and cephalopods. Whether this shark is capable of elevating its body temperature above that of the surrounding water like the other members of its family is uncertain, though it possesses the requisite physiological adaptations. Reproduction in this species is aplacental viviparous, meaning the embryos hatch from eggs inside the uterus. In the later stages of development, the unborn young are fed nonviable eggs by the mother (oophagy). The litter size is typically two, but may be as many as eight. The longfin mako is of limited commercial value, as its meat and fins are of lower quality than those of other pelagic sharks; however, it is caught unintentionally in low numbers across its range. The International Union for Conservation of Nature has assessed this species as endangered due to its rarity, low reproductive rate, and continuing bycatch mortality. In 2019, alongside the shortfin mako, the IUCN listed the longfin mako as "Endangered". (Full article...)
Image 18
The nervous shark (Carcharhinus cautus) is a species of requiem shark, and part of the family Carcharhinidae, so named because of its timid behavior in regard to humans. It is common in shallow, coastal waters off northern Australia, Papua New Guinea, and the Solomon Islands. A small brownish or grayish shark typically measuring 1.0–1.3 m (3.3–4.3 ft) long, this species has a short, blunt snout, oval eyes, and a relatively large second dorsal fin. The leading margins of most fins are finely edged with black, and the lower caudal fin lobe is black-tipped.
The collared carpetshark (Parascyllium collare) is a poorly understood species of carpetshark of the familyParascylliidaeendemic to the waters of eastern Australia between latitudes26°S and 38°S. It is typically found 55–128 m (180–420 ft) in depth near the floor of rocky reefs on the continental shelf, though its depth range can extend between 20 and 230 m (66 and 755 ft). At a maximum length of only 85 cm (2.79 ft), it poses no threat to humans. It is common within its range and is not targeted species. This, combined with high survival rates after discardment and a significant portion of habitat untouched by fishing are why it is listed as Least Concern by the International Union for Conservation of Nature (IUCN). Reproduction is oviparous and embryos feed solely on yolk. (Full article...)
Image 21
The Australian grey smooth-hound or also known as the grey gummy shark (Mustelus ravidus) is a species of houndshark classified under the large family Triakidae. It is one of the twenty-eight species belonging to the genus Mustelus, which are often small in length. While members of the genus Mustelus may be found globally in tropical and temperate waters, the grey gummy shark in particular is native to the Pacific Ocean and Indian Ocean waters surrounding Australia and is particularly widespread in deep coastal waters. The grey gummy shark is known to be a viviparous species and gives birth to live young. With little data available, it is regarded to have a relatively stable population and possesses little threat to humans. (Full article...)
Image 22
Scyliorhinus meadi, the blotched catshark, is a little-known species of catshark, and part of the family Scyliorhinidae, found in the western central Atlantic Ocean. It inhabits banks of deep-sea coral at depths of 329–548 m (1,079–1,798 ft), feeding on cephalopods, shrimp, and bony fishes. This species can be identified by its wide body and head, and the dark saddle-like markings on its back. It also has small spots that fluoresce yellow under a blue light. Adult blotched catsharks have not been observed; the largest immature specimen is 49 cm (19 in) long. Like other catsharks, it is believed to be oviparous. This species is not dangerous to humans and has no commercial significance. (Full article...)
Image 23
The megamouth shark (Megachasma pelagios) is a species of deepwater shark. Rarely seen by humans, it measures around 5.2 m (17 ft) long and is the smallest of the three extantfilter-feeding sharks alongside the relatively larger whale shark and basking shark. According to Sharkman's World Organization a total of 286 specimens have been observed or caught since its discovery in 1976. Like the other two planktivorous sharks, it swims with its mouth wide open, filtering water for plankton and jellyfish. It is recognizable from its large head with rubbery lips. The megamouth is so unlike any other type of shark that it is usually considered to be the sole extant species in the family Megachasmidae, though some scientists have suggested it may belong in the family Cetorhinidae. (Full article...)
Image 24
The blotchy swellshark or Japanese swellshark (Cephaloscyllium umbratile) is a common species of catshark, belonging to the familyScyliorhinidae. The Blotchy swellshark is found at depths of 90–200 m (300–660 ft) in the northwestern Pacific Ocean, from Japan to Taiwan. It is benthic in nature and favors rocky reefs. Reaching 1.4 m (4.6 ft) in length, this thick-bodied shark has a broad head, large mouth, and two unequally-sized dorsal fins positioned far back past the pelvic fins. It can be identified by its dorsal coloration, consisting of seven brown "saddles" and extensive darker mottling on a light tan background. This species has often been confounded with the draughtsboard shark (C. isabellum) and the Sarawak pygmy swellshark (C. sarawakensis) in scientific literature.
Voracious and opportunistic in feeding habits, the blotchy swellshark is known to consume numerous types of fishes and invertebrates, including an unusually high diversity of cartilaginous fishes. Like other Cephaloscyllium species, it is capable of rapidly inflating its body as a defense against predators. This species is oviparous, with females laying encapsulated eggs two at a time. There is no well-defined breeding season and reproduction occurs year-round. The eggs hatch after approximately one year. The blotchy swellshark is harmless and fares well in captivity. It is caught as bycatch in commercialbottom trawls, though its population does not seem to have suffered from fishing activity. (Full article...)
The Lamnidae are the family of mackerel sharks known as white sharks. They are large, fast-swimming predatory fish found in oceans worldwide, though they prefer environments with colder water. The name of the family is formed from the Greek word lamna, which means "fish of prey", and was derived from the Greeklegendary creature, the Lamia.
These sharks have pointed snouts, spindle-shaped bodies, and large gill openings. The first dorsal fin is large, high, stiff and angular or somewhat rounded. The second dorsal and anal fins are minute. The caudal peduncle has a couple of less distinct keels. The teeth are gigantic. The fifth gill opening is in front of the pectoral fin and spiracles are sometimes absent. They are powerful, heavily built sharks, sometimes weighing nearly twice as much as other sharks of comparable length from other families. Many sharks in the family are among the fastest-swimming fish, although the massive great white shark is slower due to its large size. (Full article...)
The floral banded wobbegong (Orectolobus floridus) is a recently described species of carpet shark found in the Indian Ocean, at depths of 42 to 85 meters, off southwestern Australia. With a maximum length of up to 75 cm (30 in), it is among the smallest wobbegongs. The physical characteristics consist of a striking color pattern of yellowish-brown bands, blotches, spots, and reticulations. (Full article...)
Image 5
The blacktip reef shark (Carcharhinus melanopterus) is a species of requiem shark, in the family Carcharhinidae, which can be easily identified by the prominent black tips on its fins (especially on the first dorsal fin and its caudal fin). Among the most abundant sharks inhabiting the tropicalcoral reefs of the Indian and Pacific Oceans, this species prefers shallow, inshore waters. Its exposed first dorsal fin is a common sight in the region. The blacktip reef shark is usually found over reef ledges and sandy flats, though it has also been known to enter brackish and freshwater environments. It typically attains a length of 1.6 m (5.2 ft). Like other sharks, the females are larger than the males.
The blacktip reef shark has extremely small home ranges and exhibits strong site fidelity, remaining within the same local area for up to several years at a time. It is an active predator of small bony fish, cephalopods, and crustaceans, and has also been known to feed on sea snakes and seabirds. Accounts of the blacktip reef shark's life history have been variable and sometimes contradictory, in part reflecting geographical differences within the species. Like other members of its family, this shark is viviparous, with females giving birth to two to five young on a biennial, annual, or possibly biannual cycle. Reports of the gestation period range from 7–9, through 10–11, to possibly 16 months. Mating is preceded by the male following closely behind the female, likely attracted by her chemical signals. Newborn sharks are found further inshore and in shallower water than adults, frequently roaming in large groups over areas flooded by high tide.
Timid and skittish, the blacktip reef shark is difficult to approach and seldom poses a danger to humans unless roused by food. However, people wading through shallow water are at risk of having their legs mistakenly bitten. This shark is used for its meat, fins, and liver oil, but is not considered to be a commercially significant species. The International Union for Conservation of Nature has assessed the blacktip reef shark as Vulnerable. Although the species as a whole remains widespread and relatively common, overfishing of this slow-reproducing shark has led to its decline at a number of locales. (Full article...)
Image 6
The sicklefin lemon shark (Negaprion acutidens) or sharptooth lemon shark is a species of requiem shark belonging to the family Carcharhinidae, widely distributed in the tropical waters of the Indo-Pacific. It is closely related to the better-known lemon shark (N. brevirostris) of the Americas; the two species are almost identical in appearance, both being stout-bodied sharks with broad heads, two dorsal fins of nearly equal size, and a plain yellow-tinged coloration. As its common name suggests, the sicklefin lemon shark differs from its American counterpart in having more falcate (sickle-shaped) fins. This large species grows up to 3.8 m (12 ft) long. It generally inhabits water less than 92 m (302 ft) deep in a variety of habitats, from mangroveestuaries to coral reefs.
A slow-moving predator feeding mainly on bony fishes, the sicklefin lemon shark seldom travels long distances and many individuals can be found year-round at certain locations. Like other members of its family, this species is viviparous, with females giving birth to no more than 13 pups every other year, following a gestation period of 10–11 months. Although they are potentially dangerous to humans and known to respond vigorously to any provocation, under normal circumstances, sicklefin lemon sharks are cautious and tend to retreat if approached. The IUCN has assessed this species as Endangered; its low reproductive productivity and rate of movement limits the capacity of depleted stocks to recover. Off India and Southeast Asia, this species has been severely depleted or extirpated by unregulated exploitation for its meat, fins, and liver oil. (Full article...)
Image 7
The smalldorsal cat shark (Apristurus micropterygeus) is a species of shark belonging to the familyPentanchidae, the deepwater catsharks. This shark is found in the South China Sea, at depths to 915 m. It can grow up to 37 cm. A. micropterygeus is unique among its species in having a narrow and sharply pointed first dorsal fin. However, Nakaya and Sato (2000) recommended that the status of the species be reviewed once additional specimens are available, citing the possibility that the dorsal fin of the holotype may have been malformed. The reproduction of the smalldorsal catshark is oviparous. (Full article...)
Image 8
The filetail catshark (Parmaturus xaniurus) is a species of shark belonging to the familyPentanchidae, the deepwater catsharks. This species is an Eastern Pacific endemic deepwater catshark ranging along the west coast of North America from Washington to the Gulf of California. Its name is for the toothlike projections on its skin. Nothing was known of its abundance or population structure as of 2003, but it was reported to be fairly common, being one of the most commonly encountered cartilaginous fishes in the annual West Coast Grounfish Bottom Trawl Survey from 2003 to 2011.
Adults are epibenthic and found near areas of rocky vertical relief over soft mud bottoms on the outer continental shelf and upper slope at depths of 91 to 1,251 m. Juveniles are mesopelagic, found around 500 m off the bottom in waters over 1,000 m deep. They have been seen at the Lasuen Knoll during ROV expeditions at roughly 300 m deep. Reaches a maximum size of 61 cm TL.
An oviparous species, females deposit eggcases throughout the year with concentrated reproductive output July through September. It is not targeted by commercial fisheries or utilized for human consumption, but is known to be incidental catch in longline and bottom trawl fisheries. (Full article...)
Image 9
The beige catshark (Dichichthys bigus), or beige bristle shark, is a bristle shark of the familyDichichthyidae, The first recorded specimen was a female recorded off the coast of Queensland, Australia around Lord Howe Island. Its length was 72 cm.
Recently, a number of both male and female specimens (unpublished data) were captured in the waters off New Zealand, at the edge of the EEZ (exclusive economic zone). In 2024, the first footage of this shark was captured by the ROV SuBastian during Coral Sea surveys at Southern Small Detached Reef, Queensland. To date, very little is known about the ecology of this species. Scientists are currently studying the sensory systems of this catshark in order to reveal information about its ecology and ultimately behaviour. The reproduction of the beige catshark is oviparous. (Full article...)
The western spotted catshark (Asymbolus occiduus) is a species of shark belonging to the familyPentanchidae, the deepwater catsharks. This species is found only around southwestern Australia, at depths between 100 and 400 m (330 and 1,310 ft). Males can grow up to 60 cm (24 in) in length, while females have a maximum length of 53 cm (21 in). The western spotted catshark reproduces via oviparity. (Full article...)
The night shark (Carcharhinus signatus) is a species of requiem shark, in the familyCarcharhinidae, found in the temperate and tropical waters of the Atlantic Ocean. An inhabitant of the outer continental shelf and upper continental slope, this shark most commonly occurs at depths of 50–600 m (160–1,970 ft) and conducts a diel vertical migration, spending the day in deeper water and moving into shallower waters at night. Off northeastern Brazil, large numbers congregate around seamounts of varying depths. A slender, streamlined species, the night shark typically reaches a length of 2 m (6.6 ft). It can be identified by its long, pointed snout and large, green eyes (when alive), and is dark grayish blue or brown above and white below.
Night sharks are quick, nocturnally active, schooling predators that feed mainly on small bony fishes and squid. Reproduction is viviparous as with the other members of its family; females mate during the summer and give birth to litters of usually 12–18 pups after a gestation period of a year. This deepwater species is not known to pose a danger to humans. It is caught incidentally by commercialtuna and swordfishlongline fisheries in the western Atlantic, and also by a targeted longline fishery operating off northeastern Brazil. The night shark is highly valued for its fins, and additionally as a source of meat, liver oil, and fishmeal. However, most sharks caught off northeastern Brazil have been found to contain unsafe concentrations of mercury.
Because of its low reproductive rate and historically documented declines in areas such as the Caribbean, the night shark has been assessed as vulnerable by the American Fisheries Society. A population assessment has indicated that this species is secure in the waters off the United States, but this may not be true elsewhere. (Full article...)
Image 16
The blackbelly lanternshark or lucifer shark (Etmopterus lucifer) is a shark of the familyEtmopteridae found around the world in tropical and temperate seas at depths between 150 and 1,250 meters – the mesopelagic zone. Compared to other mesopelagic fish predators and invertebrates, the blackbelly lanternshark is thought to reside in shallower, more southern waters. E. lucifer can reach up to 47 centimeters in length and consumes mesopelagic cephalopods, fish, and crustaceans. Blackbelly lanternsharks are bioluminescent, using hormone controlled mechanisms to emit light through ventral photogenic organs called photophores and are presumed to be ovoviviparous. The blackbelly lanternshark has been classified as "Not Threatened" within the New Zealand Threat Classification System. (Full article...)
Image 17
The whitespotted bamboo shark (Chiloscyllium plagiosum) is a species of carpet shark with an adult size that approaches one metre in length. This small, mostly nocturnal species is harmless to humans. The whitespotted bamboo shark is occasionally kept as a pet in larger home aquaria. It can grow up to 93 centimetres (37 in) long. (Full article...)
Image 18
The largespine velvet dogfish (Scymnodon macracanthus) is a shark of the familySomniosidae, found on the lower continental slopes between latitudes50°S and 54°S in the southeast Pacific Ocean from the Straits of Magellan, and the southwest Pacific from New Zealand, at depths of between 650 and 920 m (2,130 and 3,020 ft). Its length is up to 68 cm (27 in). It was originally in the genus Centroscymnus because of the shape of its dermal denticles and dorsal fin spines but some argued to put it in the genus Scymnodon because of its shape of dermal denticles. While some wanted to allocate these in Centroscymnus because of the shape of its lower teeth but later it was allocated to a distinct genus called Proscymnodon. (Full article...)
Image 19
The smooth hammerhead (Sphyrna zygaena) is a species of hammerhead shark, and part of the family Sphyrnidae. This species is named "smooth hammerhead" because of the distinctive shape of the head, which is flattened and laterally extended into a hammer shape (called the "cephalofoil"), without an indentation in the middle of the front margin (hence "smooth"). Unlike other hammerheads, this species prefers temperate waters and occurs worldwide at medium latitudes. In the summer, these sharks migrate towards the poles following cool water masses, sometimes forming schools numbering in the hundreds to thousands.
The second-largest hammerhead shark after the great hammerhead shark, the smooth hammerhead can measure up to 5 m (16 ft) long. It is an active predator that takes a wide variety of bony fishes and invertebrates, with larger individuals also feeding on sharks and rays. As in the rest of its family, this shark is viviparous and gives birth to litters of 20–40 pups. A relatively common shark, it is captured, intentionally or otherwise, by many commercial fisheries throughout its range; its fins are extremely valuable for use in shark fin soup. This shark is potentially dangerous and has likely been responsible for a few attacks on humans, though it is less likely to encounter swimmers than other large hammerhead species due to its temperate habitat. (Full article...)
Image 20
The nursehound (Scyliorhinus stellaris), also known as the large-spotted dogfish, greater spotted dogfish or bull huss, is a species of catshark, belonging to the familyScyliorhinidae, found in the northeastern Atlantic Ocean. It is generally found among rocks or algae at a depth of 20–60 m (66–197 ft). Growing up to 1.6 m (5.2 ft) long, the nursehound has a robust body with a broad, rounded head and two dorsal fins placed far back. It shares its range with the more common and closely related small-spotted catshark (S. canicula), which it resembles in appearance but can be distinguished from, in having larger spots and nasal skin flaps that do not extend to the mouth.
Nursehounds have nocturnal habits and generally hide inside small holes during the day, often associating with other members of its species. A benthicpredator, it feeds on a range of bony fishes, smaller sharks, crustaceans, and cephalopods. Like other catsharks, the nursehound is oviparous in reproduction. Females deposit large, thick-walled egg cases, two at a time, from March to October, securing them to bunches of seaweed. The eggs take 7–12 months to hatch. Nursehounds are marketed as food in several European countries under various names, including "flake", "catfish", "rock eel", and "rock salmon". It was once also valued for its rough skin (called "rubskin"), which was used as an abrasive. The International Union for Conservation of Nature (IUCN) has assessed the nursehound as Vulnerable, as its population in the Mediterranean Sea seems to have declined substantially from overfishing. (Full article...)
Image 21
The Japanese catshark (Apristurus japonicus) is a shark of the familyPentanchidae, the deepwater catsharks, found in the northwest Pacific off Chiba Prefecture, Honshū, Japan, between 36 and 34°N. This shark has a relatively slender body, with the trunk tapering towards the head. Its snout is moderately long, bell-shaped, and broad; the preoral snout is about 7% to 8% of its total length. It has large gill slits, rather small eyes in adults, nostrils fairly broad, and a long broad, arched mouth. It is commonly taken by trawl off the type locality, and possibly used for oil, human consumption, and fishmeal or fish cakes locally. (Full article...)
Image 22
The sixgill sawshark, Pliotrema warreni is a sawshark of the familyPristiophoridae. Presence of six pairs of gill slits highlights this genus among sharks; outside Hexanchiformes order, Pliotrema is the only shark genus with more than five gill slits. Unlike other sawsharks, the barbs on this shark's rostrum continue onto the sides of the head. Its barbels are also closer to its mouth than in other species. At maximum, females can reach over 136 cm long, and males can reach over 112 cm long. (Full article...)
It is relatively small with skin of a light-brownish color, and it can be found in the Pacific Ocean. Not much is known about this species, and no attacks on humans from this animal have been recorded. It resembles the copper shark and a sand tiger shark, yet it is much smaller than both. It also has a small, slender body, and five gills in front of its pectoral fins. (Full article...)
The Cambodian Government sees the dam as an important potential source of income and if the dam is constructed, expects to sell 70% of the power generated to Vietnam and 10% to Thailand. The balance would be directed to domestic energy markets. The dam's construction is opposed by several non-governmental organizations and civil society groups. (Full article...)
Image 2
Lamaum Dam is a privately owned hydroelectric dam located on the Catumbela River in the Benguela province of central Angola. Initially completed in 1965, the dam played a crucial role in supplying electricity to the towns of supplying electricity to the towns of Lobito, Benguela and Huambo, with an initial power output of 20 megawatts (27,000 hp).
Destruction and Rehabilitation (1983–1987): In 1983, Lamaum Dam suffered severe damage when it was destroyed by UNITA(National Union for the Total Independence of Angola) after Angola gained independence. This destructive act led to widespread flooding, resulting in the tragic loss of ten lives. Recognizing the importance of this infrastructure, Portugal stepped in to provide credit for the rehabilitation of the dam in 1987.
Rehabilitation and Expansion Plans (2008–2011): In 2008, plans were set in motion for the rehabilitation and enlargement of Lamaum Dam to increase its capacity to 60 megawatts (80,000 hp). The anticipated completion date was targeted for 2011. However, the actual progress and completion of the project may have been subject to various factors, including funding, technical challenges, and other logistical considerations. (Full article...)
Image 3
The Bui Dam is a 400-megawatt (540,000 hp) hydroelectric project in Ghana. It is built on the Black Voltariver at the Bui Gorge, at the southern end of Bui National Park. The project was a collaboration between the government of Ghana and Sino Hydro, a Chinese state-owned construction company. Construction on the main dam began in December 2009. Its first generator was commissioned on 3 May 2013, and the dam was inaugurated in December of the same year.
Bui is the second largest hydroelectric generating plant in the country after the Akosombo Dam. The reservoir flooded about 20% of the Bui National Park and impacted the habitats for the rare black hippopotamus as well as a large number of wildlife species. It required the resettlement of 1,216 people, and affected the lives and livelihoods of many more. (Full article...)
Image 4
La Paloma Dam re-directs here.
La Paloma is an artificial lake located 27 kilometres (17 mi) southeast of the city of Ovalle, in the Coquimbo Region, Chile. Although its primary purpose is to provide water for irrigation, the reservoir is also a popular recreational spot for locals and visitors. It was first inaugurated in 1968. It has an altitude of 328 metres (1,076 ft) (Full article...)
Image 5
The Kapichira Power Station is a hydroelectric power plant at the Kapachira Falls on the Shire River in Malawi. It has an installed capacity of 128 megawatts (172,000 hp), enough to power over 86,000 homes, with four 32 megawatts (43,000 hp) generating sets. The power station was developed in stages, with the first phase involving the installation of the first two 32 megawatts-generating turbines. Phase I of the power station was officially opened in September 2000.
In January 2014, in a ceremony attended by the president of Malawi at that time, Joyce Banda, the second phase of the Kapichira hydropower project was switched on, doubling the hitherto 64 megawatts to the maximum capacity of 128 megawatts. (Full article...)
The dam was built in 1984–1986 with the assistance of the Soviet Union. The power plant became operational in 1988. The dam forms a man-made reservoir lake known as Trị An Lake. La Ngà village on the La Ngà River was created as a result of population displacement.
Khrami Hydro Power Cascades are large power plants in Georgia, They act as the nation's main regulatory power plant, consisting of 2 individual Dams that work independently, and it is located on river Khrami near the town of Tsalka, Construction of the first of two Hydropower plants “Khramhes I” began in 1938 and began exploitation in late 1947, for “KhramhesII” it was finished in 1963 and went in exploitation, the main substation was constructed in valley were old headstart of the river Khrami was. Both plants are located in the municipality of Tsalka, near town of Khramhesi. Power output Cascade is 110 Thousand 110 Kw (Full article...)
The King Talal Dam is a large dam in the hills of northern Jordan, across the Zarqa River. The dam was started in 1971, with the original construction being completed in 1978 at a height of 92.5 meters. The original dam cost $46 million and was partially funded by a $16.8 million loan from the Arab Fund for Economic and Social Development and a $5.6 million grant from the Abu Dhabi Fund. Energoprojekt of Yugoslavia was the consultant and Planum of Yugoslavia was the contractor.
In 1984, to meet the country's increased water demands, work to raise the dam to a height of 106 meters was begun, a project that was completed in 1988. The dam is named after king Talal of Jordan. The main purpose of the dam is to store winter rains and treated wastewater from Amman and Zarqa treated in the As Samra plant for irrigation in the Jordan Valley. The dam irrigates about 17,000 hectares and supports the livelihood of 120,000 people. (Full article...)
Mengkuang Dam is a dam in Central Seberang Perai District, Penang, Malaysia. It is the only dam situated in Seberang Perai (Penang Mainland) and the second dam built in Penang after Ayer Itam dam. It was officially opened by the former governor, Dr. Tun Awang bin Hassan in 1985. It has the water catchment area of 3.9 km2 (1.5 sq mi) and a gross storage capacity of 23.6 billion litres (5.2×109 imp gal; 6.2×109 US gal), making it the largest dam in Penang, almost 10 times the capacity of the Ayer Itam Dam. Mengkuang Dam closed to the public from August 1, 2011, until July 31, 2016, for enlargement and renovation. The US$200 million enlargement includes increasing the height of the dam by 11 m (36 ft) and its length 1.7 km (1.1 mi) to the west. A new intake and spillway will also be added. (Full article...)
The proposed dam became the rallying point for protest in 1986–87 by hundreds of thousands of Latvians resulting with the cancellation of the project, in spite of the vast expenditures already poured into the project. The protest was a precursor of the Latvian Third Awakening. (Full article...)
Image 18
The Gilgel Gibe I Dam is a rock-filled embankment dam on the Gilgel Gibe River in Ethiopia. It is located about 57 km (35 mi) northeast of Jimma in Oromia Region. The primary purpose of the dam is hydroelectric power production. The Gilgel Gibe I hydroelectric powerplant has an installed capacity of 184 MW, enough to power over 123,200 households. The dam is 1,700 m (5,600 ft) long and 40 m (130 ft) tall. Construction on the dam began in 1988 but work was halted in 1994. In 1995 construction restarted with a new construction firm. The power station was commissioned in 2004.
Water from the dam is diverted through a 9.2 km (5.7 mi) long tunnel to an underground power station downstream. After power generation, the water is discharged back into the Gilgel Gibe River to flow downstream northwards for roughly 2 km, only to enter a 26 km (16 mi) long tunnel through a mountain ridge to an underground power station (Gilgel Gibe II Power Station) at the lower-lying Omo River. (Full article...)
Image 19
Lake Cachi (Spanish: Lago de Cachí) is an artificial lake in central Costa Rica created by the Cachí Dam (Represa de Cachí), an arch dam north of Tapantí National Park, to the east-southeast of Cartago in Cartago Province. The main town is Cachí, away from the east bank of the lake. Built in the 1970s, it was one of the first hydroelectric projects in Costa Rica. It has an installed capacity of 102 MW with three units of 34 MW capacity each (Vertical Francis turbines).
The project became operational with the first unit commissioned in 1966, the second unit in 1967, and the third unit in 1978. The Reventazon River provides multiple benefits through the three dams built on it. Out of the three dams, Cachi Dam, not only provides power generation benefits but also controls floods, and offers recreational facilities in the Lake Cachi. The Rio Macho project on the upstream provides hydroelectric power and the downstream Birris power project also provides drinking water (40% of the metropolitan city’s water supply needs).
The reservoir, in the Rio Reventazón, is an important supplier of electrical power to Costa Rica. It is operated by Instituto Costarricense de Electricidad (ICE). (Full article...)
With a power of 977 MW, it is the largest hydroelectric power station in Sweden, and also the fourth largest in the Nordic countries. The name means "Hare Run" in Swedish. This was also the name of the mighty rapids there, and the name was related to the sharp turns in the rapids, a little similar to the ones a hare does when fleeing. Normal year production is around 2131 GWh. Total fall height is around 107 m. (Full article...)
Image 22
The Nampho Dam or West Sea Dam, also known as the West Sea Barrage or West Sea Lock Gate,[a] is a tidal barrage located 15 km west of the special city of Nampho, North Korea. It is a large, eight-km-long system of dams, three lock chambers, and 36 sluices, allowing the passage of ships up to 50,000 tons. The dam closes the estuary of the Taedong River off from the Yellow Sea. It was built by the North Korean Army from 1981 to 1986, with the resources of the whole country directed to this main construction project. The West Sea Barrage Line runs over the dam.
The stated goal of the dam was:
The prevention of seawater intrusion into the fresh water, thus solving the water supply problem;
The irrigation of additional land, enlarging the arable territory of the region.
The dam is considered a major accomplishment of North Korea, and is a commonly seen backdrop for North Korean television news broadcasts from Korean Central News Agency. It is also a popular stop for tour groups of international tourists, for whom there is a visitor centre on P'i Do Island where films are shown about the construction of the dam and the locks.
The dam's estimated total cost was US$4 billion. (Full article...)
The Gariuai Hydroelectric Plant is a run-of-the-rivermicro hydro power plant located in the town of Gariuai in Baucau District, East Timor. It failed within months of its first startup, due to a landslide which took out the penstock. A subsequent effort to restore the penstock a few years later was inadequate, and the penstock failed yet again. This time due to a lack of welding between the pipes. The dams, transmission lines, power station and much of the penstock remain intact but the site has not been used for power generation since the last failure in 2008. It was the only operational hydroelectric power station in the country, and has operated for just a few months total. In order to reduce dependency on diesel generators, sites were surveyed in 2004 in Baucau District for a hydroelectric power plant. Two streams, Builai and Wainalale were selected to provide water to the power station. Construction began in 2006. A 2 m (6.6 ft) tall embankment dam was constructed on Builai stream and a second 1 m (3.3 ft) high dam was built on Wainalale stream. Connecting the dams to the power station is 2,200 m (7,200 ft) of penstock. A single 326 kW Pelton turbine-generator is located in the power station which was commissioned in November 2008. The elevation between the reservoirs and the power station affords a hydraulic head of 196 m (643 ft). The project cost US$1.4 million which was funded by a grant from the Norwegian Water Resources and Energy Directorate. (Full article...)
Image 2
The Tabqa Dam (Arabic: سَدُّ الطَّبْقَةِ, romanized: Sadd aṭ-Ṭabqah, Kurdish: Bendava Tebqa; Classical Syriac: ܣܟܪܐ ܕܛܒܩܗ, romanized: Sekro d'Tabqa), or al-Thawra Dam as it is also named (Arabic: سَدُّ الثَّوْرَةِ, romanized: Sadd aṯ-Ṯawrah, Kurdish: Bendava Tewra; Classical Syriac: ܣܟܪܐ ܕܬܘܪܗ, romanized: Sekro d'Ṯawra, literally "Revolution Dam"), most commonly known as Euphrates Dam (Arabic: سَدُّ الْفُرَاتِ, romanized: Sadd al-Furāt; Kurdish: Bendava Firatê; Classical Syriac: ܣܟܪܐ ܕܦܪܬ, romanized: Sekro d'Frot), is an earthen dam on the Euphrates, located 40 kilometres (25 mi) upstream from the city of Raqqa in Raqqa Governorate, Syria. The city of Al-Thawrah is located immediately south of the dam. The dam is 60 metres (200 ft) high and 4.5 kilometres (2.8 mi) long and is the largest dam in Syria. Its construction led to the creation of Lake Assad, Syria's largest water reservoir. The dam was constructed between 1968 and 1973 with help from the Soviet Union. At the same time, an international effort was made to excavate and document as many archaeological remains as possible in the area of the future lake before they would be flooded by the rising water. When the flow of the Euphrates was reduced in 1974 to fill the lake behind the dam, a dispute broke out between Syria and Iraq (which is downstream) that was settled by intervention from Saudi Arabia and the Soviet Union. The dam was originally built to generate hydroelectric power, as well as irrigate lands on both sides of the Euphrates. The dam has not reached its full potential in either of these objectives. (Full article...)
The dam was initially built to provide fresh water for the capital and its surroundings. It was designed in 1884 by the engineering firm of Cassaffousth, Bialet Massé and Dumesnil, finished in 1886, and inaugurated officially in 1890. Two years later the dam was suffering from a complete lack of maintenance, however, and a political scandal erupted.
The original dam was finally replaced by a newer one, located 150 m away, by an initiative of Governor Amadeo Sabattini, and completed in 1944. The newer dam was built to contain and control larger rises in water levels. When the engineers tried to demolish the original dam, the dynamite only blew the metal railing. The new dam was therefore built several meters in front of the old one. When the level of the lake is low, the upper part of the old construction can be seen. (Full article...)
Image 6
Starina reservoir is a water reservoir in eastern Slovakia, Snina District, located in the Poloniny National Park. It is the most important source of drinking water in the area, built on the headwaters of the river Cirocha. Building started in 1981. 3,463 inhabitants were evacuated from 769 dwellings from the 7 following villages (Starina, Dara, Ostrožnica, Smolník, Ruské, Veľká Poľana and Zvala). The total surface of the water reservoir Starina is 240 ha. The height of the water headbay is 50 m. This source of drinking water is very important because it supplies nearly all of East Slovakia with drinking water. There is a scenic viewpoint above the water reservoir Starina. (Full article...)
Image 7
The Batang Ai Dam (Malay: Empangan Batang Ai) is a concrete-face rock-fill dam in Batang Ai National Park in Sarawak, Malaysia. The power station comprises four 25 MWturbines, totalling the installed capacity to 100 MW. The station is operated by Sarawak Electricity Supply Corporation. Preparations for the dam began in 1975, before the design was published in 1977. Construction started in 1982 with the river diversion work and the last turbine completed in 1985. The Batang Ai project, a relatively modest dam financed by the Asian Development Bank, caused the displacement of approximately 3,000 people from 26 longhouses. These people have since been accommodated in the Batang Ai Resettlement Scheme to cultivate cocoa and rubber but the programme has not been successful. (Full article...)
It has a total installed capacity of 54 megawatts (72,000 hp), with two units equipped with francis turbines, and has an annual production of approximately 270 gigawatt-hours (970 TJ). The power station utilises the waterfalls between Meldal and Svorkmo on the Orkla river system, with a total head of 99 metres (325 ft). (Full article...)
Image 10
The Koudiat Acerdoune Dam is a gravity dam located 9.5 km (6 mi) southwest of Kadiria on the Isser River in Bouïra Province, Algeria. The dam was constructed between 2002 and 2008 with the roller-compacted concrete technique. It serves the purpose of providing water for industrial, irrigation and municipal uses. It retains a 640,000,000 m3 (518,856 acre⋅ft) capacity reservoir which supplies water for the irrigation of 20,000 ha (49,421 acres) of land along with providing the Algiers region with 178,000,000 m3 (144,307 acre⋅ft) of drinking water annually. (Full article...)
Aiviekste hydroelectric power station is the first hydroelectric power station constructed in Latvia. It is located on the Aiviekste River. The power station was commissioned in 1925 and until 1938 it was the largest in Latvia. The power station was decommissioned in 1969; however, in 1988 it was decided to restore it. In 1993, the power station restarted power generation.
The power station has total capacity of 0.8 MW. In 2007, it generated 3GWh of electricity. The power station is operated by Latvenergo.
The reconstruction of the hydropower plant was completed in 2022, and the plant’s capacity increased from 0.8 MW to 1.5 MW. The connection of Aiviekste HPP to the electricity network was also rebuilt. In 2023, 4.2 GWh of electricity were generated at Aiviekste HPP. (Full article...)
Image 13
Huai Kum Dam (Thai: เขื่อนห้วยกุ่ม, RTGS: Khuean Huai Kum, pronounced[kʰɯ̀a̯nhûa̯jkùm]), is on the Nam Phrom River in Kaset Sombun District, Chaiyaphum Province, Thailand. It consists of a rockfill dam with clay core (35.5 metres high and 282 metres long) and a 1.2 MW semi-underground powerhouse which rises four metres high from the ground and 11 metres beneath the surface. The dam forms a reservoir with a storage capacity of 22 million cubic metres to supply water for the downstream irrigation areas of Chulabhorn Dam in Chaiyaphum Province whereas the power plant provides two million kWh of electric energy per year. The king and the queen accompanied by Princess Maha Chakri Sirindhorn and Princess Chulabhorn presided over the inauguration ceremony on 19 December 1980. (Full article...)
Image 14
The Zuiderzee Works (Dutch: Zuiderzeewerken) is a system of dams and dikes, land reclamation and water drainage work, which was the largest hydraulic engineering project undertaken by the Netherlands during the twentieth century. The project involved the damming of the Zuiderzee, a large, shallow inlet of the North Sea, and the reclamation of land in the newly enclosed water using polders. Its main purposes are to improve flood protection and create additional land for agriculture.
The dam's reservoir has a total capacity of 300,000 m3. The water is transported to the powerhouse through a 12.04 km long tunnel and a 3.65 km long pressure tube. The plant has 3 × 30 MWPelton turbines, with a total installed capacity of 90 MW. The plant has a net level declination of 490.6 m, and a designed flow of 7.33 m3/s per unit.
The plant's total output between 1981 and 2006 was 6600.96 GWh, which amounts to an average annual electricity generation of 264 GWh. (Full article...)
The construction of the dam began in 1974 and was completed in 1979. Power is generated by fourteen Kaplanturbines, totaling the installed capacity to 1,890 MW (2,530,000 hp). The dam passes approximately 64,000 cubic metres (2,300,000 cu ft) of water per second, compared to the current average flow of the Uruguay River at 4,622 cubic metres (163,200 cu ft). The reservoir has a total area of 783 square kilometres (302 sq mi), while its maximum dimensions are 140 by 9 kilometres (87.0 mi × 5.6 mi). (Full article...)
The dam serves several purposes including irrigation in the Fergana Valley and hydroelectric power production. Water released from the dam can enter a canal on either side of the river downstream. The dam has two power stations located at its base, Andijan 1 and Andijan 2. The former contains four 35 MW turbine-generators and the latter contains two 25 MW Francis turbine-generators for a total installed capacity of 190 MW.
Construction on the dam began in 1969 and the generators at Andijan 1 were commissioned between 1974 and 1984. Construction at Andijan 2 began in 2007 and it was commissioned on 2 September 2010. It cost US$28.5 million of which US$15.93 million was provided by the Exim Bank of China.
The artificial lake created by this dam, the Andijan Reservoir, is fed by the Kara Darya and its tributaries Kurshab and Jazy. (Full article...)
{{ Transclude list item excerpts as random slideshow | List of mountain ranges | section=Mountain ranges on Earth }} Select from Earth section, avoiding Moon
The range is underlain principally by Mesozoic granitic rocks that are partly veneered by upper Cenozoic volcanic rocks of the Coso Volcanic Field. The volcanic units (in apparent decreasing age) include (1) widespread basaltic flows, (2) dacitic flows and tuff, and (3) rhyolitic domes and flows and basaltic cones and flows. These volcanic rocks are encompassed by an oval-shaped zone of late Cenozoic ring faulting that measures about 24 miles (39 km) east to west and 28 miles (45 km) north to south and that defines a structural basin. Most of the Coso Range and a slice of the adjacent Sierra Nevada lie within this ring structure. The youngest volcanic rocks are Pleistocene and, with associated active fumaroles, occupy a north-trending structural and topographic ridge about 11.2 by 6.2 miles (18 by 10 km) near the center of the basin. The ring structure and associated volcanic rocks suggest a large underlying magma chamber that has periodically erupted lava to the surface during the past few million years. (Full article...)
In the United States, these mountains are considered a subrange of the Rocky Mountains, whereas in Canada they are considered separate, as the northern border of the Rocky Mountains is considered to be the Liard River far to the south in the province of British Columbia.
Various historical records also referred to the range as the Arctic Mountains, Hooper Mountains, Meade Mountains and Meade River Mountains. The Canadian portion of the range is officially called the British Mountains. Ivvavik National Park is located in Canada's British Mountains. (Full article...)
Strandzha (Bulgarian: Странджа, also transliterated as Strandja, pronounced[ˈstrand͡ʒɐ]; Turkish: Istranca[ɯstɾand͡ʒa], or Yıldız[jɯɫdɯz]) is a mountain massif in southeastern Bulgaria and East Thrace, the European part of Turkey. It is in the southeastern part of the Balkans between the plains of Thrace to the west, the lowlands near Burgas to the north, and the Black Sea to the east. Its highest peak is Mahya Dağı (Bulgarian: Махиада, Mahiada) (1,031 m or 3,383 ft) in Turkey, while the highest point on Bulgarian territory is Golyamo Gradishte (Bulgarian: Голямо Градище) (710 m or 2,329 ft). The total area is approximately 10,000 km2 (3,861 sq mi). (Full article...)
The San Bernardino Mountains are a high and rugged mountain range in Southern California in the United States. Situated north and northeast of San Bernardino and spanning two California counties, the range tops out at 11,503 feet (3,506 m) at San Gorgonio Mountain – the tallest peak in Southern California. The San Bernardinos form a significant region of wilderness and are popular for hiking and skiing.
The mountains were formed about eleven million years ago by tectonic activity along the San Andreas Fault, and are still actively rising. Many local rivers originate in the range, which receives significantly more precipitation than the surrounding desert. The range's unique and varying environment allows it to maintain some of the greatest biodiversity in the state. For over 10,000 years, the San Bernardinos and their surroundings have been inhabited by indigenous peoples, who used the mountains as a summer hunting ground.
Spanish explorers first encountered the San Bernardinos in the late 18th century, naming the eponymous San Bernardino Valley at its base. European settlement of the region progressed slowly until 1860, when the mountains became the focus of the largest gold rush ever to occur in Southern California. Waves of settlers brought in by the gold rush populated the lowlands around the San Bernardinos, and began to tap the mountains' rich timber and water resources on a large scale by the late 19th century.
Recreational development of the range began in the early 20th century, when mountain resorts were built around new irrigation reservoirs. Since then, the mountains have been extensively engineered for transportation and water supply purposes. Four major state highways and the California Aqueduct traverse the mountains today; these developments have all had significant impacts on area wildlife and plant communities. (Full article...)
The mountains lie within the Ural geographical region and significantly overlap with the Ural Federal District and the Ural economic region. Their resources include metal ores, coal, and precious and semi-precious stones. Since the 18th century, the mountains have contributed significantly to the mineral sector of the Russian economy. The region is one of the largest centres of metallurgy and heavy industry production in Russia. (Full article...)
The municipality contains 77% of the 3,534 hectares (8,730 acres) Rio da Casca Ecological Station, a strictly protected conservation unit created in 1994. The municipal seat contains the 31 hectares (77 acres) Quineira State Park, created in 2006. (Full article...)
Image 16
The Sierra de San Borja, also known as Sierra La Libertad is a mountain range on the Baja California Peninsula of Mexico. It is one of the Peninsular Ranges which form the backbone of Baja California. The Sierra de San Borja is located between 28° North latitude (the border of the states of Baja California and Baja California Sur) and 29° North latitude (Highway 12). The highest point of the Sierra is Cerro La Sandia, 1,775 metres (5,823 ft) in elevation located at .
The Sierra de San Borja is nearly uninhabited. Desert vegetation prevails with only a few water sources. Tourists visit the San Francisco Borja Mission (founded 1762) and the extensive prehistoric rock art scattered throughout the mountains. (Full article...)
According to the USGS, the Cumberland Mountain range is 131 miles (211 km) long and 20 miles (32 km) wide, bounded by the Russell Fork on the northeast, the Pound River and Powell River on the southeast, Cove Creek on the southwest, and Tackett Creek, the Cumberland River, Poor Fork Cumberland River, and Elkhorn Creek on the northwest. The crest of the range forms the Kentucky and Virginia boundary from the Tennessee border to the Russell Fork River.
Variant names of the Cumberland Mountains include Cumberland Mountain, Cumberland Range, Ouasioto Mountains, Ouasiota Mountains, Laurel Mountain, and Pine Mountain. They are named for Prince William, Duke of Cumberland.
The Cumberland Mountains range includes Pine Mountain, Cross Mountain, Cumberland Mountain, Log Mountain, Little Black Mountain, and Black (Big Black) Mountain, as well as others. (Full article...)
Image 19
The Cape Fold Belt (CFB) is a 1,300 kilometres (810 mi) long fold-and-thrust mountain belt along the western and southern coastlines of Western Cape, South Africa. The Cape Fold Belt formed during the Permian period (300 to 250million years ago) in the late Paleozoic age, affecting the sequence of sedimentary rock layers of the siliciclastic Cape Supergroup with folding and faulted rocks, which were deposited in the Cape Basin in the southwestern corner of South Africa.
The Cape Fold Belt was once part of a larger orogenic belt with other mountain ranges that formed as part of the same tectonic event that originally extended from Argentina, across southern Africa, and into Antarctica. It included the Ventana Mountains near Bahía Blanca in Argentina, the Pensacola Mountains in East Antarctica, the Ellsworth Mountains in West Antarctica, and the Hunter–Bowen orogeny in eastern Australia. The rocks involved in this fold system are primarily sandstones and shales, with shales from the Bokkeveld Group persisting in valley floors, while the more erosion-resistant sandstones of the Peninsula Formation form the parallel ranges of the Cape Fold Mountains. The highest peak in the range is Seweweekspoortpiek, which reaches 2,325meters.
The Cape Fold Mountains form a series of parallel ranges that run along the south-western and southern coastlines of South Africa for 850 km from the Cederberg 200 km to the north of the Cape Peninsula, and then along the south coast as far as Port Elizabeth, 650 km to the east (see the two maps one above the other on the right). (Full article...)
The Livingston Range is a mountain range located primarily in Glacier National Park in the U.S. state of Montana, and in the extreme southeastern section of the Canadian province of British Columbia. The range is 36 miles (58 km) long and 28 miles (45 km) wide. Over 15 summits exceed 9,000 ft (2,700 m) above sea level, and the highest point is Kintla Peak at 10,101 feet (3,079 m). (While these elevations are not particularly high for North American mountains, they are high compared to the roughly 4,000 foot (1,200 m) elevation of the nearby valleys, making for particularly dramatic peaks.)
The Livingston Range was uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km) long over newer rocks of the cretaceous period. (Full article...)
The massif has a length of 25 kilometres (16 mi) from the northwest to the southeast and a width of 14 kilometres (8.7 mi). It is located east of the town Ștei, Bihor County and north of the town of Brad, Hunedoara County.
The highest peak is Cucurbăta Mare, with an elevation of 1,849 metres (6,066 ft); this also the highest peak of the Apuseni Mountains. Other high peaks are Buteasa (1,790 m), Cârligatele (1,694 m), Piatra Grăitoare (1,658 m), and Bohodei (1,654 m).
The Vlădeasa Massif [ro] is a volcanic range extension of the Bihor Mountains to the north, reaching a maximum height of 1,836 metres (6,024 ft). (Full article...)
Image 24
The Cordillera Central is a Bolivianmountain range that divides the three river basins in the country and also has the second highest peaks in Bolivia. It is rich in minerals and starts in the north with Chawpi Urqu and the three Palumanis that were in the south up to Zapaleri, forming a border with Chile and Argentina. The Cordillera Central is divided into three sections:
The northern section or Cordillera Real, with Chawpi Urqu and Palumani, also taking into account the most significant of Bolivia that you find near La Paz, Illimani, Illampu, Janq'u Uma, Mururata, and Huayna Potosí, all of which are more than 6,000 meters high. This section is famous because the highest meteorological observatory in the world can be found on Chacaltaya. Some of the highest ski slopes in the world can be found here also.
The central section contains Sumaq Urqu, with the Potosí mountain range and the Paso de Condor rail station, both situated at an elevation of 4,288 meters.
The southern section is characterized by its high rate of mineralization and large deposits of tin. Its highest summit is Zapaleri on the border with Chile and Argentina.
Cordillera Central can also be found between Cordillera Occidental and Cordillera Oriental
The Apennines or Apennine Mountains (/ˈæpənaɪn/AP-ə-nyne; Ancient Greek: Ἀπέννινα ὄρη or Ἀπέννινον ὄρος; Latin: Appenninus or Apenninus Mons– a singular with plural meaning; Italian: Appennini[appenˈniːni]) are a mountain range consisting of parallel smaller chains extending c. 1,200 km (750 mi) the length of peninsularItaly. In the northwest they join the Ligurian Alps at Altare. In the southwest they end at Reggio di Calabria, the coastal city at the tip of the peninsula. Since 2000 the Environment Ministry of Italy, following the recommendations of the Apennines Park of Europe Project, has defined the Apennines System to include the mountains of north Sicily, a total distance of 1,500 kilometres (930 mi). The system forms an arc enclosing the east of the Ligurian and Tyrrhenian seas.
The Apennines conserve some intact ecosystems that have survived human intervention. In these are some of the best-preserved forests and montane grasslands in Europe, now protected by national parks and, within them, a high diversity of flora and fauna. These mountains are one of the last refuges of the big European predators such as the Italian wolf and the Marsican brown bear, now extinct in the rest of Central Europe.
The mountains lend their name to the Apennine peninsula that forms the major part of Italy. They are mostly verdant, although one side of the highest peak, Corno Grande, is partially covered by Calderone glacier, the only glacier in the Apennines. The eastern slopes down to the Adriatic Sea are steep, whilst the western slopes form foothills on which most of the towns of peninsular Italy are located. The mountains tend to be named after the province or provinces in which they are located; for example the Ligurian Apennines are in Liguria. (Full article...)
The name Bukit Barisan actually means "row of hills" or "hills that make a row" in Malay, for the range stretches end to end along the island of Sumatra.
There are 35 active volcanoes in Bukit Barisan. The largest is the supervolcanoToba within the 100 km (62 miles) × 30 km (19 miles) Lake Toba, which was created after a caldera collapse (est. in 74,000 Before Present). The eruption is estimated to have been at level eight on the VEI scale, the largest possible for a volcanic eruption. (Full article...)
The Ore Mountains (German: Erzgebirge, Czech: Krušné hory) lie along the Czech–German border, separating the historical regions of Bohemia in the Czech Republic and Saxony in Germany. The highest peaks are the Klínovec in the Czech Republic (German: Keilberg) at 1,244 metres (4,081 ft) above sea level and the Fichtelberg in Germany at 1,215 metres (3,986 ft).
The Ore Mountains have been intensively reshaped by human intervention and a diverse cultural landscape has developed. Mining in particular, with its tips, dams, ditches and sinkholes, directly shaped the landscape and the habitats of plants and animals in many places. The region was also the setting of the earliest stages of the early modern transformation of mining and metallurgy from a craft to a large-scale industry, a process that preceded and enabled the later Industrial Revolution.
The higher altitudes from around 500 m above sea level on the German side belong to the Ore Mountains/Vogtland Nature Park – the largest of its kind in Germany with a length of 120 km. The eastern Ore Mountains are protected landscape. Other smaller areas on the German and Czech sides are protected as nature reserves and natural monuments. On the ridges there are also several larger raised bogs that are only fed by rainwater. The mountains are popular for hiking and there are winter sports areas at higher elevations. In 2019, the region became a UNESCOWorld Heritage Site. (Full article...)
The Cordillera Oriental or Eastern Cordillera is a set of parallel mountain ranges of the BolivianAndes, emplaced on the eastern and north eastern margin of the Andes. Large parts of Cordillera Oriental are forested and humid areas rich in agricultural and livestock products. Geologically, the Cordillera Oriental is formed by the Central Andean fold and thrust belt.
Owing to its high peaks Schweizerland is a popular climbing destination, together with the Watkins Range to the northeast and the Stauning Alps further north. Tasiilaq Heliport is located near the area of the range. (Full article...)
Image 11
The Hida Mountains (飛騨山脈, Hida Sanmyaku), or Northern Alps (北アルプス, Kita Arupusu), is a Japanese mountain range which stretches through Nagano, Toyama and Gifu prefectures. A small portion of the mountains also reach into Niigata Prefecture. William Gowland coined the phrase "Japanese Alps" during his time in Japan, but he was only referring to the Hida Mountains when he used that name. The Kiso and Akaishi mountains received the name in the ensuing years. (Full article...)
The Sayan Mountains' towering peaks and cool lakes southwest of Tuva give rise to the tributaries that merge to become one of Siberia's major rivers, the Yenisei River, which flows north over 3,400 kilometres (2000 mi) to the Arctic Ocean. This is a protected and isolated area, having been kept closed by the Soviet Union since 1944. (Full article...)
Its highest peak is the Feldberg with an elevation of 1,493 metres (4,898 ft) above sea level. Roughly oblong in shape, with a length of 160 kilometres (100 miles) and breadth of up to 50 km (30 mi), it has an area of about 6,009 km2 (2,320 sq mi).
Historically, the area was known for forestry and the mining of ore deposits, but tourism has now become the primary industry, accounting for around 300,000 jobs. There are several ruined military fortifications dating back to the 17th century. (Full article...)
Image 17
The Balkan mountain range is located in the eastern part of the Balkans in Southeastern Europe. The range is conventionally taken to begin at the peak of Vrashka Chuka on the border between Bulgaria and Serbia. It then runs for about 560 kilometres (350 mi), first in a south-easterly direction along the border, then eastward across Bulgaria, forming a natural barrier between the northern and southern halves of the country, before finally reaching the Black Sea at Cape Emine. The mountains reach their highest point with Botev Peak at 2,376 metres (7,795 ft).
In much of the central and eastern sections, the summit forms the watershed between the drainage basins of the Black Sea and the Aegean. A prominent gap in the mountains is formed by the predominantly narrow Iskar Gorge, a few miles north of the Bulgarian capital, Sofia. The karst relief determines the large number of caves, including Magura, featuring the most important and extended European post-Palaeolithic cave painting, Ledenika, Saeva dupka, Bacho Kiro, etc. The most notable rock formation are the Belogradchik Rocks in the west.
There are several important protected areas: Central Balkan National Park, Vrachanski Balkan, Bulgarka and Sinite Kamani, as well as a number of nature reserves. The Balkan Mountains are remarkable for their flora and fauna. Edelweiss grows there in the region of Kozyata stena. Some of the most striking landscapes are included in the Central Balkan National Park with steep cliffs, the highest waterfalls in the Balkans and lush vegetation. There are a number of important nature reserves such as Chuprene, Kozyata stena and others. Most of Europe's large mammals inhabit the area including the brown bear, wolf, boar, chamois and deer.
The mountains are the source of the name of the Balkans (sometimes considered as a distinct peninsula or region). In Bulgarian and Serbian the mountains are also known as Стара планинаStara planina (pronounced in Bulgarian as [ˈstarɐpɫɐniˈna] and in Serbian as [stâːraːplanǐna]), a term whose literal meaning is 'old mountain'. (Full article...)
Geologic evidence indicates that the mountains were formed during the break-up of the supercontinent of Gondwana. The mountains came along the west coast of India somewhere in the late Jurassic and early Cretaceous periods when India separated from the African continent. The mountains can be roughly divided into three parts: the northern section with an elevation ranging from 900–1,500 m (3,000–4,900 ft), the middle section starting from the south of Goa with a lower elevation of less than 900 m (3,000 ft), and the southern section where the altitude rises again. The Western Ghats have several peaks that rise above 2,000 m (6,600 ft), with Anamudi (2,695 m (8,842 ft)) being the highest peak. The average elevation is around 1,200 m (3,900 ft).
The Western Ghats form one of the major watersheds of India, feeding many perennial river systems that drain almost 40% of the land area of the country. Because of the higher elevation of the Deccan plateau on the west, most rivers flow from eastwards towards the Bay of Bengal, resulting in chiselled eastern slopes and steeper western slopes facing the Arabian Sea. The Western Ghats play an important role in determining the climate and seasons in India. It blocks the rain-bearing monsoon winds flowing eastward from the Arabian Sea, resulting in rainfall along the western coast. By the time the air rises above the mountains, it becomes dry, forming a rain shadow region with very little rainfall on the leeward side towards the interior of the Deccan plateau.
The Western Ghats region is a biodiversity hotspot. It contains a large number of different species of flora and fauna, most of which are endemic to this region. At least 325 globally threatened species occur in the Western Ghats. The region was declared as a UNESCOWorld Heritage Site in 2012. (Full article...)
The Wick Mountains are a range within New Zealand's Fiordland National Park, the country's biggest national park. Their highest peak is Mount Elliot 1,990 metres (6,530 ft), and this can be seen in fine weather from the Milford Track, a popular tourist walking track. (Full article...)
{{ Transclude list item excerpts as random slideshow | List of dams and reservoirs | section=Africa | sectiononly=yes }} Should pick only the international dams
Completed in 1981, it was originally envisaged to become part of the Eastern National Water Carrier, a scheme to supply water to Namibia's capital Windhoek from the Okavango River, 1,000 kilometres (620 mi) to the north on the Angolan border. The scheme was never completed. Omatako Dam today only contains floods and supplies water to the Von Bach Dam. As such, it is one of three dams supplying the capital Windhoek with water. (Full article...)
Located southwest of Harare, it provides the main water supply for the city. The lake was constructed over two-and-a-half years and opened to the public in 1952. The dam wall is 400 metres long.
The water is also used for irrigation purposes and commercial fishing. Some of the fishes that are found in the lake include common grass carp, tigerfish, black bream, Clarias gariepinus, yellowfish, and green-headed bream.
The lake and hinterland are protected as part of Lake Chivero Recreational Park. The lake was designated a Ramsar wetland of international importance on 3 January 2013.
Remembrance Island is a small island in the reservoir. (Full article...)
Constructed between 2011 and 2023, the dam's primary purpose is electricity production to relieve Ethiopia's acute energy shortage and to export electricity to neighbouring countries. With an installed capacity of 5.15 gigawatts, the dam is the largest hydroelectric power plant in Africa and among the 20 largest in the world.
The first phase of filling the reservoir began in July 2020 and in August 2020 the water level increased to 540 meters (40 meters higher than the bottom of the river which is at 500 meters above sea level). The second phase of filling was completed on 19 July 2021, with water levels increased to around 575 meters. The third filling was completed on 12 August 2022 to a level of 600 metres (2,000 ft). The fourth filling was completed on 10 September 2023 with water levels at around 625 metres (2,051 ft).
On 20 February 2022, the dam produced electricity for the first time, delivering 375 MW to the grid. A second 375 MW turbine was commissioned in August 2022. The third and fourth 400 MW turbines were commissioned in August 2024. (Full article...)
The Neckartal Dam, nicknamed the Desert Dragon, is a dam in the ǁKaras Region of southern Namibia. It is a curved gravity dam on the Fish River near Berseba, c. 40 kilometres (25 mi) northwest of the regional capital Keetmanshoop. Construction started in 2013 and was initially expected to finish in 2017. Since its completion in 2018, it is the largest dam in Namibia, more than three times the capacity of the Hardap Dam upstream. The dam's purpose is to support a 5,000 hectares (12,000 acres) irrigation scheme nearby. (Full article...)
The Kariba Dam is a double curvature concrete arch dam in the Kariba Gorge of the Zambezi river basin between Zambia and Zimbabwe. The dam stands 128 metres (420 ft) tall and 579 metres (1,900 ft) long. The dam forms Lake Kariba, which extends for 280 kilometres (170 mi) and holds 185 cubic kilometres (150,000,000 acre⋅ft) of water. (Full article...)
The plant was inaugurated by the Malian Prime Minister Abdoulaye Maïga in December 2022. It cost US$329 million and the 280 km (170 mi) of transmission lines cost US$65 million. The project received 85 percent of its funding from the Exim Bank of China along with US$1 million from the EU-Africa Infrastructure Trust Fund and US$1.4 million from the International Development Association and European Investment Bank.
It has an installed capacity of 140 megawatts (190,000 hp) and will use the outflows of the Manantali Dam upstream to regulation water flow into the plant. A 1,230 m (4,040 ft) long weir just above the water fall directs water into a channel which will feed the power house just downstream of the falls. The power house contains three 46.6 MW Kaplan turbine-generators. The difference in elevation the water fall and weir provides a hydraulic head (water drop) of 22.5 m (74 ft). (Full article...)
Image 13
The Rusumo Hydroelectric Power Station (Kinyarwanda: Urugomero rw'amashanyarazi rwa Rusumo, French: Centrale hydroélectrique de Rusumo), also known as the Rusumo Power Station, is an operational hydropower plant, with initial capacity installation of 80 megawatts (110,000 hp). The project involved the construction of a dam, with run of river design. A more expensive 90 megawatts (120,000 hp) reservoir design was considered before being abandoned in favor of an 80 MW project with a smaller environmental impact and an estimated cost of US$300 million compared to US$400 million for the bigger project.
The World Bank announced on 6 August 2013 that it had approved loans totaling US$340 million towards the US$468.60 million needed for the project. In November 2013, the African Development Bank approved a loan of US$113 million towards completion of the project. (Full article...)
The site for the dam at Bumbuna Falls was first identified in 1971, and construction was begun in 1975. Work was halted in May 1997, about 85% completed, due to the Sierra Leone Civil War, and did not restart until 2005. The project was completed and went online in 2009. Nearly a third of the dam's US$327 million cost ($103 million) was supplied by the African Development Bank. A 26 January 2005 report noted that 33 villages would be affected by the dam, although only one (of 16 households and 135 people) would require resettlement.
The dam has a maximum height of 87 metres (285 ft), a length of 400 metres (1,300 ft) at the crest and a volume of 2,500,000 cubic metres (88,000,000 cu ft). The volume of the reservoir created is 410,000,000 cubic metres (1.4×1010 cu ft), 428,000,000 cubic metres (1.51×1010 cu ft) or 480,000,000 cubic metres (1.7×1010 cu ft). There are two Francis turbines, each rated for 25 megawatts (34,000 hp).
After completion, the project has been plagued with problems, and barely produces 10 megawatts (13,000 hp) or 25 megawatts (34,000 hp) as of 2013.
A second phase is planned, for a 110-megawatt (150,000 hp) power station. In June 2011, the government announced it had awarded the $750 million Phase II project to Joule Africa, a UK-based company. This will entail a second dam and plant. Construction was set to begin in 2014 and continue on until at least 2017. (Full article...)
Bangala Dam lies in south-eastern Zimbabwe, south of Masvingo. It was built by Concor to provide irrigation water to the farming estates on the lowveld to the southwest, around the town of Triangle, where the main crop has been sugar cane.
Ayago Hydroelectric Power Station, also Ayago Power Station, is a planned 840 megawatt hydroelectric power project to be constructed in Uganda. If it is built, Ayago would be the largest power station in Uganda, based on generating capacity. (Full article...)
The Wadi Qattara Dam, also referred to as Gattara or Al-Qattarah, is a clay-fill embankment dam located on Wadi Al-Qattara, 33 km (21 mi) east of Benghazi in Libya. Together with a secondary dam located 10 km (6 mi) downstream at and seven drop structures, the scheme was constructed after floods damaged the Benghazi area in 1938 and 1954. They were also constructed for irrigation water supply. Construction of the dams began in 1968 and was completed in 1971. However, a flood in 1979 severely damaged the main dam and destroyed the secondary dam downstream. The main dam was rehabilitated and the secondary dam was replaced with a rock-fill dam between 2000 and 2004 at a cost of US$30 million. The main dam was heightened 7 m (23 ft) and its total discharge capacity was increased to 240 m3/s (8,476 cu ft/s). Both dams were designed by Coyne et Bellier. (Full article...)
Image 6
The Bujagali Power Station is a hydroelectric power station across the Victoria Nile that harnesses the energy of its namesake, the Bujagali Falls, in Uganda. Construction began in 2007 and concluded in 2012. It was officially inaugurated on 8 October 2012 by Ugandan President Yoweri Museveni and Aga Khan IV in the presence of African politicians and investors.
The 250-megawatt power station was the largest hydroelectric energy source in Uganda when it was commissioned. However, the planned Karuma and Ayago power stations would be larger. The funding for the station was a source of some concern, as investors joined and departed from the project. As of July 2014, the plant was managed by Bujagali Energy Limited, which selected Italian contractor Salini Impregilo to develop the project. (Full article...)
Image 7
The Gwenoro Dam is located inside Gwenoro Farm, an estate formerly owned by Ian Douglas Smith (1919-2007), a former Prime Minister of Rhodesia. The farm was seized in stages by the Government of Zimbabwe from Ian Smith and his family between 2002 and December 2012. The Gwenoro Dam supplies water to nearby Gweru and Shurugwi in Zimbabwe. The dam is constructed on the Runde River (formerly Lundi River; a medium density suburb in Gweru is named after the river (Lundi Park)). The name Gwenoro is derived from a wild animal found in the area known in the local language of Shona as Nhoro (gweNORO), which means a 'place inhabited by Nhoro'(kudu). The area is very beautiful and picturesque. The dam is full from January to June. Fish co-operatives are sprouting around the banks of this river. ZIMASCO used to run a mine club but has since stopped. What remains are only buildings. (Full article...)
Image 8
The Banieya Dam is an embankment dam on the Samou River in the Kindia Region of Guinea. It is located 16 km (9.9 mi) west of Kindia. The dam was completed by 1969 for the purpose of water supply. A hydroelectric power station of 5.2 megawatts (7,000 hp) was commissioned at the dam's toe in 1988. The Kale Dam, which also supports a hydroelectric power station, is located downstream. (Full article...)
Image 9
The Hassan II Dam, also known as the Sidi Said Dam, is a gravity dam on the Moulouya River about 13 km (8.1 mi) north of Midelt in Midelt Province, Morocco. It has a maximum storage capacity of 400 million cubic meters. The dam is used for potable water, irrigation and the protection of downstream areas and dams against floods and siltation. Construction of the dam began in February 2001 and it was completed in March 2005. (Full article...)
Image 10
The Gove Dam is an embankment dam on the Kunene River about 75 km (47 mi) south of Huambo in Huambo Province, Angola. The purpose of the dam is to control floods and generate hydroelectric power. It has a power generating capacity of 60 megawatts (80,000 hp) each) (three turbines of 20 megawatts (27,000 hp) each), enough to power over 30,000 homes. (Full article...)
Image 11
Mai Nefhi (Tigrigna for "Water-Distend?") is both a location near Asmara, Eritrea and the dam after which it was named. The Mai Nefhi dam was completed in 1970, during the reign of Haile Selassie, and remains the main water source for Asmara.
Abardae a town with a population of 3,000 residents is located nearby. Eritrea Institute of Technology, the only technical college in the country is located 500m away from Abardae-Mai Nefhi. (Full article...)
Image 12
The Kandadji Dam, is a large multipurpose dam under construction on the Niger River. The site is situated near the small town of Kandadji, Tillabéri Department, Tillabéri Region, Niger, 180 km northwest of the capital Niamey. It is being built by the Haut Commissariat à l'Aménagement de la Vallée du Niger (High Commission for Niger Valley), a public body under the Primer Minister's Office.
The dam will generate hydropower and is control the flow of the Niger River, holding water during the dry season to maintain a minimum flow and making downstream irrigation possible. The project is formally named the Kandadji Programme for Ecosystem Regeneration and Niger River Development (Programme Kandadji de Régénération des Ecosystèmes et de Mise en Valeur du Fleuve Niger). (Full article...)
The Neckartal Dam, nicknamed the Desert Dragon, is a dam in the ǁKaras Region of southern Namibia. It is a curved gravity dam on the Fish River near Berseba, c. 40 kilometres (25 mi) northwest of the regional capital Keetmanshoop. Construction started in 2013 and was initially expected to finish in 2017. Since its completion in 2018, it is the largest dam in Namibia, more than three times the capacity of the Hardap Dam upstream. The dam's purpose is to support a 5,000 hectares (12,000 acres) irrigation scheme nearby. (Full article...)
The Gilgel Gibe III Dam is a 250m high roller-compacted concrete dam with an associated hydroelectric power plant on the Omo River in Ethiopia. It is located about 62 km (39 mi) west of Sodo in the South Ethiopia Regional State. Once fully commissioned, it will be the third largest hydroelectric plant in Africa with a power output of about 1,870 Megawatt (MW), thus more than doubling Ethiopia's total installed capacity from its 2007 level of 814 MW. The Gibe III dam is part of the Gibe cascade, a series of dams including the existing Gibe I dam (184 MW) and Gibe II power station (420 MW) as well as the planned Gibe IV (1,472 MW) and Gibe V (560 MW) dams. The existing dams are owned and operated by the state-owned Ethiopian Electric Power, which is also the client for the Gibe III Dam.
The US$1.8 billion project began in 2006 and electricity generation started in October 2015. The remaining generators were operational by 2016. The project has experienced serious delays; in May 2012, full commissioning had been scheduled for June 2013. The dam was inaugurated by Prime Minister Hailemariam Desalegn on 17 December 2016.
Local and international environmental groups forecast major negative environmental and social impacts of the dam and criticized the project's environmental and social impact assessment as insufficient. Because of this and accusations that the entire approval process for the project was suspect, funding for the full construction cost was not secured, as the African Development Bank delayed a decision about a loan pending a review of the dam's environmental impact by its compliance review and mediation unit. This dates back to August 2009 when they accepted a call from NGOs for such a review. In August 2010 Ethiopian Prime Minister Meles Zenawi vowed to complete the dam "at any cost", saying the dam's critics "don’t want to see developed Africa; they want us to remain undeveloped and backward to serve their tourists as a museum." (Full article...)
Jeet Kune Do[pronunciation?] (Chinese: 截拳道; Jyutping: zit6 kyun4 dou6; lit. 'stop fist way or: way of the intercepting fist'; abbreviated JKD) is a hybrid martial art conceived and practiced by martial artist Bruce Lee. It was formed from Lee's experiences in unarmed fighting and self-defence—as well as eclectic, Zen Buddhist, Confucianist and Taoist philosophies—as a new school of martial arts thought.
At the heart of Jeet Kune Do lies the principle of intercepting the opponent's attacks, crafting responses or counterattacks that effectively target the adversary's offensive moves. JKD also incorporates a set of principles to help practitioners make instant decisions and improve the physical and mental self, being intended to have practical applications in life without the traditional routines and metaphysics of conventional martial arts. As an eclectic martial art, it relies on a fighting style heavily influenced by Wing Chun, Tai Chi, taekwondo, boxing, fencing and jujutsu.
Bruce Lee himself never formalized Jeet Kune Do before he died. This forced later JKD practitioners to rely upon their own interpretation of the philosophy created by Bruce Lee. (Full article...)
The Legend of Bruce Lee (Chinese: 李小龍傳奇) is a 2008 Chinese biographical television series based on the life story of martial artist and actor Bruce Lee. The 50-episode series was produced and broadcast by CCTV and began airing on October 12, 2008. It was intended to promote Chinese culture alongside the 2008 Beijing Summer Olympics.
It stars Hong Kong actor Danny Chan as Bruce Lee and American actress Michelle Lang as Lee's wife, Linda Lee Cadwell. The production period spanned nine months, with filming taking place in China, Hong Kong, Macau, the United States, Italy, and Thailand, and with a budget of 50 million yuan (US$7.3 million).
Chinese Gung Fu: The Philosophical Art of Self-Defense was published in early 1963 by Bruce Lee with the help of friend and fellow martial artist James Yimm Lee of Oakland, California. James had previously published books on the martial arts such as Modern Gung Fu, Karate: Iron, Poison Hand Training and Karate Oriental Self-Defense in 1957. In the book Remembering the Master: Bruce Lee, James Yimm Lee and the Creation of Jeet Kune Do by Sid Campbell and Greglon Yimm Lee (James Lee's son) it is stated the initial run was 1,500 copies. The book was sold through James Lee's company Oriental Book Sales at a price of $5. In addition to the book, a companion Chinese Gung Fu instruction chart was available for $1.
Following Bruce Lee's death, his estate commissioned writer John Little to edit and publish some of Lee's writings. Little included the content of Chinese Gung Fu: The Philosophical Art of Self-Defense as well as additional 1964 writings by Bruce Lee in the book Bruce Lee, The Tao of Gung Fu: Commentaries on the Chinese Martial Arts. (Full article...)
Image 6
Super Dragon: The Bruce Lee Story (Chinese: 一代猛龍) is a 1974 Bruceploitation film starring Bruce Lee impersonator Bruce Li. The film is a loose biopic about martial artist and actor Bruce Lee and centers on his supposed affair with actress Betty Ting-Pei. The film is notable for being the first biopic about Lee (it was released a year after his death), the debut film of Li as a Lee impersonator, and the first entry in the Bruceploitation genre. (Full article...)
Bruce Lee: The Lost Interview is the name given to the 9 December 1971 edition of The Pierre Berton Show, which featured martial artist/actor Bruce Lee in his only English speaking television interview. Its title is derived from its status; it was presumed lost for several years until its rediscovery and airing on 2 November 1994. Over the course of the interview, which was filmed in Hong Kong, Bruce Lee and Pierre Berton discuss Lee's career, various aspects of martial arts philosophy and the inherent problems faced by an Asian in pursuing stardom in Hollywood. A review of the interview by Bill Stockey said that Bruce Lee's "human side is exposed and he is portrayed as more approachable". (Full article...)
Brandon Bruce Lee (February 1, 1965 – March 31, 1993) was an American actor. Establishing himself as a rising action star in the early 1990s, he landed what was to be his breakthrough role as Eric Draven in the supernatural superhero film The Crow (1994). However, Lee's career and life were cut short by his accidental death during the film's production.
Transitioning to Hollywood productions, Lee first starred in the Warner Brosbuddy cop film Showdown in Little Tokyo (1991), co-starring Dolph Lundgren. While it did not do well with audiences and critics upon its release, it later became a cult film. This was followed by a leading role in Rapid Fire (1992), produced by 20th Century Fox. Lee, alongside Jeff Imada, is also credited for the fight choreography, which contained elements of Jeet Kune Do. Though the film was not well-received, critics praised Lee's onscreen presence. (Full article...)
Announced in July 2017, it is the first Tarantino film not to involve Bob and Harvey Weinstein, as Tarantino ended his partnership with the brothers following the sexual abuse allegations against Harvey Weinstein. After a bidding war, the film was distributed by Sony Pictures, which met Tarantino's demands, including final cut privilege. Pitt, DiCaprio, Robbie, Zoë Bell, Kurt Russell and others joined the cast between January and June 2018. Principal photography lasted from June through November around Los Angeles. Once Upon a Time in Hollywood is the final film to feature Luke Perry, who died on March 4, 2019, and it is dedicated to his memory.
Once Upon a Time in Hollywood premiered at the 2019 Cannes Film Festival on May 21, 2019, and was theatrically released in the United States on July 26, 2019, and in the United Kingdom on August 14. It grossed over $392 million worldwide and received acclaim from critics, although historical accuracies and artists were criticized. The National Board of Review and the American Film Institute named Once Upon a Time in Hollywood one of the top-ten films of 2019. Once Upon a Time in Hollywood was nominated for ten awards at the 92nd Academy Awards, winning two (Best Supporting Actor for Pitt and Best Production Design), and received numerous other accolades. A novelization, written by Tarantino in his debut as an author, was published in 2021. (Full article...)
Image 18
The Real Bruce Lee, is a 1977 martial artsdocumentary that comes complete with a feature-length Korean martial arts film titled Last Fist of Fury (최후의 정무문, Choihui Jeongmumun).
The version of the film that is commonly distributed in the West (USA) on public domain-type DVD and video labels runs 93 minutes in length. The British VHS-version released in 1979 runs 118 minutes. (Full article...)
Image 19
Tao of Jeet Kune Do is a book expressing Bruce Lee's martial artsphilosophy and viewpoints, published posthumously (after Bruce Lee's death in 1973). The project for this book began in 1970 when Bruce Lee suffered a back injury during one of his practice sessions. During this time he could not train in martial arts. He was ordered by his doctors to wear a back brace for 6 months in order to recover from his injury. This was a very tiring and dispiriting time for Lee who was always very physically active.
It was during his convalescence that he decided to compile a treatise on the system or approach to martial arts that he was developing; he called it Jeet Kune Do. The bulk of these writings would become the "core set of writings". Many of these writings were done during a single session which provided natural continuity. Lee had also kept various notes throughout the development of his combat philosophy and these would become the disparate notes used in the book. Many of these notes were "sudden inspirations" which were incomplete and lacked any kind of a construct. The combination of the "core set of writings" and the "disparate notes" would be known as the text Tao of Jeet Kune Do.
In 1971, it was Lee's intent to finish the treatise that he started during his convalescence. However, his film career and work prevented him from doing so. He also vacillated about publishing his book as he felt that this work might be used for the wrong purposes. Lee's intent in writing the book was to record one man's way of thinking about the martial arts. It was to be a guidebook, not a set of instructions or "How to" manual to learn martial arts. (Full article...)
Bruce Liang (28 April 1948) is a Hong Kong martial artist and actor who has appeared in many Hong Kong martial arts movies. He often appeared billed as "Bruce Leung", "Bruce Liang", "Bruce Leong", or "Bruce Leung Siu-lung", and is thus generally grouped among the Bruce Lee clones that sprang up after Lee's death in the subgenre known as Bruceploitation. (Full article...)
Image 23
Ip Man (born Ip Kai-man; 1 October 1893 – 2 December 1972), also known as Yip Man, was a Chinese martial arts grandmaster. He became a teacher of the martial art of Wing Chun when he was 20. He had several students who later became martial arts masters in their own right, the most famous among them being Bruce Lee. (Full article...)
The Way of the Dragon was released in Hong Kong on 30 December 1972, and in the United States in August 1974. The film went on to gross an estimated US$130 million worldwide (equivalent to over $700 million adjusted for inflation), against a tight budget of $130,000, earning a thousand times its budget. It was the highest-grossing Hong Kong film up until Lee's next film Enter the Dragon (1973).
The film is primarily set in a restaurant in Rome. The owners are being harassed by a local crime boss, and request help from a relative in Hong Kong. The help arrives in the form of a young martial artist. The conflict between the restaurant staff and the gangsters soon escalates. (Full article...)
Image 2
Chen Zhen (陳真; 陈真; Chén Zhēn; Can4 Zan1) is a fictional character created by Hong Kong writer Ni Kuang. First portrayed by Bruce Lee in the 1972 film Fist of Fury, the character has been the subject of numerous film and television series, including remakes and adaptations of Fist of Fury. Many notable actors, including Jet Li and Donnie Yen, have portrayed Chen Zhen on screen after Bruce Lee. Although Chen Zhen's story varies in the different remakes and adaptations, most have an ending similar to the original Fist of Fury. Chen Zhen is believed to be based on Liu Zhensheng (劉振聲), an apprentice of Huo Yuanjia, a martial artist who lived during the late Qing dynasty of China. (Full article...)
Image 3
Dragon: The Bruce Lee Story is a 1993 American biographicaldrama film directed by Rob Cohen. The film stars Jason Scott Lee, with a supporting cast including Lauren Holly, Nancy Kwan, and Robert Wagner. The film follows the life of actor and martial artist Bruce Lee (Jason) from his relocation to the United States from Hong Kong to his career as a martial arts teacher, and then as a television and film actor. It also focuses on the relationship between Bruce and his wife Linda, and the racism to which Bruce was subjected.
The primary source of the screenplay is Cadwell's 1975 biography Bruce Lee: The Man Only I Knew. Other sources include Robert Clouse's book Bruce Lee: The Biography and research by Cohen, including interviews with Cadwell and Bruce's son, Brandon Lee. Rather than a traditional biographical film, Cohen decided to include elements of mysticism and to dramatise fight scenes to give it the same tone as the films in which Bruce starred. Dragon was filmed primarily in Hong Kong, Los Angeles and San Francisco.
Dragon: The Bruce Lee Story received generally positive reviews, with critics finding it entertaining despite criticisms of its veneration of Bruce. Jason was widely praised for his performance. The film was a commercial success and its revenue exceeded box office averages for biographical films, which was attributed to its romantic themes and its appeal to people outside the traditional kung fu film audience. A video game adaptation of the same name was released the following year. Dragon is dedicated to Brandon, who died several weeks before its release. (Full article...)
Image 4
Ip Man (born Ip Kai-man; 1 October 1893 – 2 December 1972), also known as Yip Man, was a Chinese martial arts grandmaster. He became a teacher of the martial art of Wing Chun when he was 20. He had several students who later became martial arts masters in their own right, the most famous among them being Bruce Lee. (Full article...)
Image 5
Bruce Lee's Fighting Method is a book of volumes covering Bruce Lee's martial arts abilities of the Jeet Kune Do movement. The book is available as a single hardcover volume or a series of four paperback volumes. The text describes Bruce Lee's Kung Fufighting techniques, philosophy and training methods. This book was originally written in 1966 by Bruce Lee. However, Lee decided not to publish this work as he feared that instructors would use the fighting knowledge in this text to promote themselves. In 1978, after Bruce Lee's death, his widow Linda Lee Cadwell decided to make available the information on her husband's work. Lee's death changed the perspective of releasing the information that Bruce Lee himself had vacillated about. The book was published with the help of Mitoshi Uyehara. Uyehara was the founder and owner of Black Belt Magazine. During the early years of the publication, Uyehara served as the publisher. Bruce Lee contributed many articles to the publication during the 1960s and a friendship ensued between the two men. Uyehara, a martial artist in his own right, was a key personage in arranging Lee's material for publication. (Full article...)
Tao of Jeet Kune Do is a book expressing Bruce Lee's martial artsphilosophy and viewpoints, published posthumously (after Bruce Lee's death in 1973). The project for this book began in 1970 when Bruce Lee suffered a back injury during one of his practice sessions. During this time he could not train in martial arts. He was ordered by his doctors to wear a back brace for 6 months in order to recover from his injury. This was a very tiring and dispiriting time for Lee who was always very physically active.
It was during his convalescence that he decided to compile a treatise on the system or approach to martial arts that he was developing; he called it Jeet Kune Do. The bulk of these writings would become the "core set of writings". Many of these writings were done during a single session which provided natural continuity. Lee had also kept various notes throughout the development of his combat philosophy and these would become the disparate notes used in the book. Many of these notes were "sudden inspirations" which were incomplete and lacked any kind of a construct. The combination of the "core set of writings" and the "disparate notes" would be known as the text Tao of Jeet Kune Do.
In 1971, it was Lee's intent to finish the treatise that he started during his convalescence. However, his film career and work prevented him from doing so. He also vacillated about publishing his book as he felt that this work might be used for the wrong purposes. Lee's intent in writing the book was to record one man's way of thinking about the martial arts. It was to be a guidebook, not a set of instructions or "How to" manual to learn martial arts. (Full article...)
A statue of Bruce Lee was unveiled on 26 November 2005, in the city of Mostar, Bosnia and Herzegovina, by sculptor Ivan Fijolić. Located in Zrinjevac City Park, the life-sized statue stands 1.68 m (5 ft 6 in) tall, shorter than Bruce Lee's actual height of 1.72 m (5 ft 8 in), and was a symbol of solidarity in the ethnically-divided city until it was stolen in a heist on March 4, 2024, and was subsequently found albeit cut in pieces. (Full article...)
Super Dragon: The Bruce Lee Story (Chinese: 一代猛龍) is a 1974 Bruceploitation film starring Bruce Lee impersonator Bruce Li. The film is a loose biopic about martial artist and actor Bruce Lee and centers on his supposed affair with actress Betty Ting-Pei. The film is notable for being the first biopic about Lee (it was released a year after his death), the debut film of Li as a Lee impersonator, and the first entry in the Bruceploitation genre. (Full article...)
Kato is a fictional character from The Green Hornet franchise. This character has appeared with the Green Hornet in radio, film, television, book and comic book versions. Kato is the Green Hornet's crime-fighting sidekick, and Britt Reid's manservant in civilian life, and has been played by a number of actors. On radio, Kato was initially played by Raymond Hayashi, then Roland Parker who had the role for most of the run, and in the later years Mickey Tolan and Paul Carnegie. Keye Luke took the role in the movie serials, and in the television series, he was portrayed by Bruce Lee. Jay Chou played Kato in the 2011 Green Hornet film. (Full article...)
Game of Death (Chinese: 死亡的遊戲) is an incomplete Hong Kong martial arts film, of which portions were filmed between September and October 1972, and was planned and scheduled to be released by 1973, directed, written, produced by and starring Bruce Lee. The project was paused to film and produce Enter the Dragon. For Game of Death, over 120 minutes of footage was shot. The remaining footage has since been released with Lee's original Cantonese and English dialogue, with John Little dubbing Lee's Hai Tien character as part of the documentary titled Bruce Lee: A Warrior's Journey. Much of the footage that was shot is from what was to be the climax of the film.
During filming, Lee received an offer to star in Enter the Dragon, the first kung fu film to be produced by a Hollywood studio (Warner Bros.), and with a budget unprecedented for the genre ($850,000). Lee died of cerebral edema before the film's release. At the time of his death, he had made plans to resume the filming of The Game of Death. After Lee's death, Enter the Dragon director Robert Clouse was enlisted to finish the film using two stand-ins; it was released in 1978 as Game of Death, five years after Lee's death, by Golden Harvest.
The story of Lee's original 1972 film involves Lee's character, in order to save his younger sister and brother, joining a group of martial artists who are hired to retrieve a stolen Chinese national treasure[need quotation to verify] from the top floor of a five-story pagoda in South Korea, with each floor guarded by martial artists who must be defeated while ascending the tower.[additional citation(s) needed] The 1978 film's plot was altered to a revenge story, where the mafia attempts to kill Lee's character, who fakes his death and seeks vengeance against those who tried to kill him. The final part of the film uses some of Lee's original film footage, but with the pagoda setting changed to a restaurant building, where he fights martial artists hired by the mafia in an attempt to rescue his fiancée Ann Morris (played by Colleen Camp). This revised version received a mixed critical reception but was commercially successful, grossing an estimated US$50,000,000 (equivalent to $240,000,000 in 2024) worldwide. (Full article...)
Outline of underwater diving § Modes of underwater diving
Surface-supplied divers riding a stage to the underwater workplace
Underwater diving, as an activity, it is the practice of descending below the water's surface to interact with the environment. It is also often referred to as diving, an ambiguous term with several possible meanings, depending on context. Immersion in water and exposure to high ambient pressure have physiological effects that limit the depths and duration possible in ambient pressure diving. Humans are not physiologically and anatomically well-adapted to the environmental conditions of diving, and various equipment has been developed to extend the depth and duration of human dives, and allow different types of work to be done.
In ambient pressure diving, the diver is directly exposed to the pressure of the surrounding water. The ambient pressure diver may dive on breath-hold (freediving) or use breathing apparatus for scuba diving or surface-supplied diving, and the saturation diving technique reduces the risk of decompression sickness (DCS) after long-duration deep dives. Atmospheric diving suits (ADS) may be used to isolate the diver from high ambient pressure. Crewed submersibles can extend depth range to full ocean depth, and remotely controlled or robotic machines can reduce risk to humans.
The environment exposes the diver to a wide range of hazards, and though the risks are largely controlled by appropriate diving skills, training, types of equipment and breathing gases used depending on the mode, depth and purpose of diving, it remains a relatively dangerous activity. Professional diving is usually regulated by occupational health and safety legislation, while recreational diving may be entirely unregulated. Diving activities are restricted to maximum depths of about 40 metres (130 ft) for recreational scuba diving, 530 metres (1,740 ft) for commercial saturation diving, and 610 metres (2,000 ft) wearing atmospheric suits. Diving is also restricted to conditions which are not excessively hazardous, though the level of risk acceptable can vary, and fatal incidents may occur.
Recreational diving (sometimes called sport diving or subaquatics) is a popular leisure activity. Technical diving is a form of recreational diving under more challenging conditions. Professional diving (commercial diving, diving for research purposes, or for financial gain) involves working underwater. Public safety diving is the underwater work done by law enforcement, fire rescue, and underwater search and recovery dive teams. Military diving includes combat diving, clearance diving and ships husbandry. Deep sea diving is underwater diving, usually with surface-supplied equipment, and often refers to the use of standard diving dress with the traditional copper helmet. Hard hat diving is any form of diving with a helmet, including the standard copper helmet, and other forms of free-flow and lightweight demand helmets. The history of breath-hold diving goes back at least to classical times, and there is evidence of prehistoric hunting and gathering of seafoods that may have involved underwater swimming. Technical advances allowing the provision of breathing gas to a diver underwater at ambient pressure are recent, and self-contained breathing systems developed at an accelerated rate following the Second World War. (Full article...)
Image 2
2nd Reconnaissance Battalion combat diver training with the Dräger LAR V rebreather
Rebreather diving is underwater diving using diving rebreathers, a class of underwater breathing apparatus which recirculate the breathing gas exhaled by the diver after replacing the oxygen used and removing the carbon dioxide metabolic product. Rebreather diving is practiced by recreational, military and scientific divers in applications where it has advantages over open circuit scuba, and surface supply of breathing gas is impracticable. The main advantages of rebreather diving are extended gas endurance, low noise levels, and lack of bubbles.
Rebreathers are generally used for scuba applications, but are also occasionally used for bailout systems for surface-supplied diving. Gas reclaim systems used for deep heliox diving use similar technology to rebreathers, as do saturation divinglife-support systems, but in these applications the gas recycling equipment is not carried by the diver. Atmospheric diving suits also carry rebreather technology to recycle breathing gas as part of the life-support system, but this article covers the procedures of ambient pressure diving using rebreathers carried by the diver.
Rebreathers are generally more complex to use than open circuit scuba, and have more potential points of failure, so acceptably safe use requires a greater level of skill, attention and situational awareness, which is usually derived from understanding the systems, diligent maintenance and overlearning the practical skills of operation and fault recovery. Fault tolerant design can make a rebreather less likely to fail in a way that immediately endangers the user, and reduces the task loading on the diver which in turn may lower the risk of operator error. (Full article...)
Image 3
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 4
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 5
Atmospheric diving suit
An atmospheric diving suit (ADS), or single atmosphere diving suit is a small one-person articulated submersible which resembles a suit of armour, with elaborate pressure joints to allow articulation while maintaining an internal pressure of one atmosphere. An ADS can enable diving at depths of up to 2,300 feet (700 m) for many hours by eliminating the majority of significant physiological dangers associated with deep diving. The occupant of an ADS does not need to decompress, and there is no need for special breathing gas mixtures, so there is little danger of decompression sickness or nitrogen narcosis when the ADS is functioning properly. An ADS can permit less skilled swimmers to complete deep dives, albeit at the expense of dexterity.
Atmospheric diving suits in current use include the Newtsuit, Exosuit, Hardsuit and the WASP, all of which are self-contained hard suits that incorporate propulsion units. The Hardsuit is constructed from cast aluminum (forged aluminum in a version constructed for the US Navy for submarine rescue); the upper hull is made from cast aluminum, while the bottom dome is machined aluminum. The WASP is of glass-reinforced plastic (GRP) body tube construction. (Full article...)
Image 6
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 7
Saturation diver working on the USS Monitor wreck at 70 m (230 ft) depth Saturation diving is diving for periods long enough to bring all tissues into equilibrium with the partial pressures of the inert components of the breathing gas used. It is a diving mode that reduces the number of decompressions divers working at great depths must undergo by only decompressing divers once at the end of the diving operation, which may last days to weeks, having them remain under pressure for the whole period. A diver breathing pressurized gas accumulates dissolved inert gas used in the breathing mixture to dilute the oxygen to a non-toxic level in the tissues, which can cause potentially fatal decompression sickness ("the bends") if permitted to come out of solution within the body tissues; hence, returning to the surface safely requires lengthy decompression so that the inert gases can be eliminated via the lungs. Once the dissolved gases in a diver's tissues reach the saturation point, however, decompression time does not increase with further exposure, as no more inert gas is accumulated.
Saturation diving takes advantage of this by having divers remain in that saturated state. When not in the water, the divers live in a sealed environment which maintains their pressurised state; this can be an ambient pressure underwater habitat or a saturation system at the surface, with transfer to and from the pressurised living quarters to the equivalent depth underwater via a closed, pressurised diving bell. This may be maintained for up to several weeks, and divers are decompressed to surface pressure only once, at the end of their tour of duty. By limiting the number of decompressions in this way, and using a conservative decompression schedule the risk of decompression sickness is significantly reduced, and the total time spent decompressing is minimised. Saturation divers typically breathe a helium–oxygen mixture to prevent nitrogen narcosis, and limit work of breathing, but at shallow depths saturation diving has been done on nitrox mixtures.
Most of the physiological and medical aspects of diving to the same depths are much the same in saturation and bell-bounce ambient pressure diving, or are less of a problem, but there are medical and psychological effects of living under saturation for extended periods.
Saturation diving is a specialized form of diving; of the 3,300 commercial divers employed in the United States in 2015, 336 were saturation divers. Special training and certification is required, as the activity is inherently hazardous, and a set of standard operating procedures, emergency procedures, and a range of specialised equipment is used to control the risk, that require consistently correct performance by all the members of an extended diving team. The combination of relatively large skilled personnel requirements, complex engineering, and bulky, heavy equipment required to support a saturation diving project make it an expensive diving mode, but it allows direct human intervention at places that would not otherwise be practical, and where it is applied, it is generally more economically viable than other options, if such exist. (Full article...)
Image 8
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 9
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 10
Surface-supplied divers riding a stage to the underwater workplace
Underwater diving, as an activity, it is the practice of descending below the water's surface to interact with the environment. It is also often referred to as diving, an ambiguous term with several possible meanings, depending on context. Immersion in water and exposure to high ambient pressure have physiological effects that limit the depths and duration possible in ambient pressure diving. Humans are not physiologically and anatomically well-adapted to the environmental conditions of diving, and various equipment has been developed to extend the depth and duration of human dives, and allow different types of work to be done.
In ambient pressure diving, the diver is directly exposed to the pressure of the surrounding water. The ambient pressure diver may dive on breath-hold (freediving) or use breathing apparatus for scuba diving or surface-supplied diving, and the saturation diving technique reduces the risk of decompression sickness (DCS) after long-duration deep dives. Atmospheric diving suits (ADS) may be used to isolate the diver from high ambient pressure. Crewed submersibles can extend depth range to full ocean depth, and remotely controlled or robotic machines can reduce risk to humans.
The environment exposes the diver to a wide range of hazards, and though the risks are largely controlled by appropriate diving skills, training, types of equipment and breathing gases used depending on the mode, depth and purpose of diving, it remains a relatively dangerous activity. Professional diving is usually regulated by occupational health and safety legislation, while recreational diving may be entirely unregulated. Diving activities are restricted to maximum depths of about 40 metres (130 ft) for recreational scuba diving, 530 metres (1,740 ft) for commercial saturation diving, and 610 metres (2,000 ft) wearing atmospheric suits. Diving is also restricted to conditions which are not excessively hazardous, though the level of risk acceptable can vary, and fatal incidents may occur.
Recreational diving (sometimes called sport diving or subaquatics) is a popular leisure activity. Technical diving is a form of recreational diving under more challenging conditions. Professional diving (commercial diving, diving for research purposes, or for financial gain) involves working underwater. Public safety diving is the underwater work done by law enforcement, fire rescue, and underwater search and recovery dive teams. Military diving includes combat diving, clearance diving and ships husbandry. Deep sea diving is underwater diving, usually with surface-supplied equipment, and often refers to the use of standard diving dress with the traditional copper helmet. Hard hat diving is any form of diving with a helmet, including the standard copper helmet, and other forms of free-flow and lightweight demand helmets. The history of breath-hold diving goes back at least to classical times, and there is evidence of prehistoric hunting and gathering of seafoods that may have involved underwater swimming. Technical advances allowing the provision of breathing gas to a diver underwater at ambient pressure are recent, and self-contained breathing systems developed at an accelerated rate following the Second World War. (Full article...)
Open-circuit scuba systems discharge the breathing gas into the environment as it is exhaled and consist of one or more diving cylinders containing breathing gas at high pressure which is supplied to the diver at ambient pressure through a diving regulator. They may include additional cylinders for range extension, decompression gas or emergency breathing gas. Closed-circuit or semi-closed circuit rebreather scuba systems allow recycling of exhaled gases. The volume of gas used is reduced compared to that of open-circuit, making longer dives feasible. Rebreathers extend the time spent underwater compared to open-circuit for the same metabolic gas consumption. They produce fewer bubbles and less noise than open-circuit scuba, which makes them attractive to covert military divers to avoid detection, scientific divers to avoid disturbing marine animals, and media divers to avoid bubble interference.
Scuba diving may be done recreationally or professionally in a number of applications, including scientific, military and public safety roles, but most commercial diving uses surface-supplied diving equipment for breathing gas security when this is practicable. Scuba divers engaged in armed forces covert operations may be referred to as frogmen, combat divers or attack swimmers.
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Open-circuit scuba systems discharge the breathing gas into the environment as it is exhaled and consist of one or more diving cylinders containing breathing gas at high pressure which is supplied to the diver at ambient pressure through a diving regulator. They may include additional cylinders for range extension, decompression gas or emergency breathing gas. Closed-circuit or semi-closed circuit rebreather scuba systems allow recycling of exhaled gases. The volume of gas used is reduced compared to that of open-circuit, making longer dives feasible. Rebreathers extend the time spent underwater compared to open-circuit for the same metabolic gas consumption. They produce fewer bubbles and less noise than open-circuit scuba, which makes them attractive to covert military divers to avoid detection, scientific divers to avoid disturbing marine animals, and media divers to avoid bubble interference.
Scuba diving may be done recreationally or professionally in a number of applications, including scientific, military and public safety roles, but most commercial diving uses surface-supplied diving equipment for breathing gas security when this is practicable. Scuba divers engaged in armed forces covert operations may be referred to as frogmen, combat divers or attack swimmers.
A freediver on the ocean floor Freediving, free-diving, free diving, breath-hold diving, or skin diving, is a mode of underwater diving that relies on breath-holding until resurfacing rather than the use of breathing apparatus such as scuba gear.
Besides the limits of breath-hold, immersion in water and exposure to high ambient pressure also have physiological effects that limit the depths and duration possible in freediving.
Open-circuit scuba systems discharge the breathing gas into the environment as it is exhaled and consist of one or more diving cylinders containing breathing gas at high pressure which is supplied to the diver at ambient pressure through a diving regulator. They may include additional cylinders for range extension, decompression gas or emergency breathing gas. Closed-circuit or semi-closed circuit rebreather scuba systems allow recycling of exhaled gases. The volume of gas used is reduced compared to that of open-circuit, making longer dives feasible. Rebreathers extend the time spent underwater compared to open-circuit for the same metabolic gas consumption. They produce fewer bubbles and less noise than open-circuit scuba, which makes them attractive to covert military divers to avoid detection, scientific divers to avoid disturbing marine animals, and media divers to avoid bubble interference.
Scuba diving may be done recreationally or professionally in a number of applications, including scientific, military and public safety roles, but most commercial diving uses surface-supplied diving equipment for breathing gas security when this is practicable. Scuba divers engaged in armed forces covert operations may be referred to as frogmen, combat divers or attack swimmers.
A freediver on the ocean floor Freediving, free-diving, free diving, breath-hold diving, or skin diving, is a mode of underwater diving that relies on breath-holding until resurfacing rather than the use of breathing apparatus such as scuba gear.
Besides the limits of breath-hold, immersion in water and exposure to high ambient pressure also have physiological effects that limit the depths and duration possible in freediving.
Saturation diver working on the USS Monitor wreck at 70 m (230 ft) depth Saturation diving is diving for periods long enough to bring all tissues into equilibrium with the partial pressures of the inert components of the breathing gas used. It is a diving mode that reduces the number of decompressions divers working at great depths must undergo by only decompressing divers once at the end of the diving operation, which may last days to weeks, having them remain under pressure for the whole period. A diver breathing pressurized gas accumulates dissolved inert gas used in the breathing mixture to dilute the oxygen to a non-toxic level in the tissues, which can cause potentially fatal decompression sickness ("the bends") if permitted to come out of solution within the body tissues; hence, returning to the surface safely requires lengthy decompression so that the inert gases can be eliminated via the lungs. Once the dissolved gases in a diver's tissues reach the saturation point, however, decompression time does not increase with further exposure, as no more inert gas is accumulated.
Saturation diving takes advantage of this by having divers remain in that saturated state. When not in the water, the divers live in a sealed environment which maintains their pressurised state; this can be an ambient pressure underwater habitat or a saturation system at the surface, with transfer to and from the pressurised living quarters to the equivalent depth underwater via a closed, pressurised diving bell. This may be maintained for up to several weeks, and divers are decompressed to surface pressure only once, at the end of their tour of duty. By limiting the number of decompressions in this way, and using a conservative decompression schedule the risk of decompression sickness is significantly reduced, and the total time spent decompressing is minimised. Saturation divers typically breathe a helium–oxygen mixture to prevent nitrogen narcosis, and limit work of breathing, but at shallow depths saturation diving has been done on nitrox mixtures.
Most of the physiological and medical aspects of diving to the same depths are much the same in saturation and bell-bounce ambient pressure diving, or are less of a problem, but there are medical and psychological effects of living under saturation for extended periods.
Saturation diving is a specialized form of diving; of the 3,300 commercial divers employed in the United States in 2015, 336 were saturation divers. Special training and certification is required, as the activity is inherently hazardous, and a set of standard operating procedures, emergency procedures, and a range of specialised equipment is used to control the risk, that require consistently correct performance by all the members of an extended diving team. The combination of relatively large skilled personnel requirements, complex engineering, and bulky, heavy equipment required to support a saturation diving project make it an expensive diving mode, but it allows direct human intervention at places that would not otherwise be practical, and where it is applied, it is generally more economically viable than other options, if such exist. (Full article...)
Image 4
Surface-supplied divers riding a stage to the underwater workplace
Underwater diving, as an activity, it is the practice of descending below the water's surface to interact with the environment. It is also often referred to as diving, an ambiguous term with several possible meanings, depending on context. Immersion in water and exposure to high ambient pressure have physiological effects that limit the depths and duration possible in ambient pressure diving. Humans are not physiologically and anatomically well-adapted to the environmental conditions of diving, and various equipment has been developed to extend the depth and duration of human dives, and allow different types of work to be done.
In ambient pressure diving, the diver is directly exposed to the pressure of the surrounding water. The ambient pressure diver may dive on breath-hold (freediving) or use breathing apparatus for scuba diving or surface-supplied diving, and the saturation diving technique reduces the risk of decompression sickness (DCS) after long-duration deep dives. Atmospheric diving suits (ADS) may be used to isolate the diver from high ambient pressure. Crewed submersibles can extend depth range to full ocean depth, and remotely controlled or robotic machines can reduce risk to humans.
The environment exposes the diver to a wide range of hazards, and though the risks are largely controlled by appropriate diving skills, training, types of equipment and breathing gases used depending on the mode, depth and purpose of diving, it remains a relatively dangerous activity. Professional diving is usually regulated by occupational health and safety legislation, while recreational diving may be entirely unregulated. Diving activities are restricted to maximum depths of about 40 metres (130 ft) for recreational scuba diving, 530 metres (1,740 ft) for commercial saturation diving, and 610 metres (2,000 ft) wearing atmospheric suits. Diving is also restricted to conditions which are not excessively hazardous, though the level of risk acceptable can vary, and fatal incidents may occur.
Recreational diving (sometimes called sport diving or subaquatics) is a popular leisure activity. Technical diving is a form of recreational diving under more challenging conditions. Professional diving (commercial diving, diving for research purposes, or for financial gain) involves working underwater. Public safety diving is the underwater work done by law enforcement, fire rescue, and underwater search and recovery dive teams. Military diving includes combat diving, clearance diving and ships husbandry. Deep sea diving is underwater diving, usually with surface-supplied equipment, and often refers to the use of standard diving dress with the traditional copper helmet. Hard hat diving is any form of diving with a helmet, including the standard copper helmet, and other forms of free-flow and lightweight demand helmets. The history of breath-hold diving goes back at least to classical times, and there is evidence of prehistoric hunting and gathering of seafoods that may have involved underwater swimming. Technical advances allowing the provision of breathing gas to a diver underwater at ambient pressure are recent, and self-contained breathing systems developed at an accelerated rate following the Second World War. (Full article...)
Image 5
2nd Reconnaissance Battalion combat diver training with the Dräger LAR V rebreather
Rebreather diving is underwater diving using diving rebreathers, a class of underwater breathing apparatus which recirculate the breathing gas exhaled by the diver after replacing the oxygen used and removing the carbon dioxide metabolic product. Rebreather diving is practiced by recreational, military and scientific divers in applications where it has advantages over open circuit scuba, and surface supply of breathing gas is impracticable. The main advantages of rebreather diving are extended gas endurance, low noise levels, and lack of bubbles.
Rebreathers are generally used for scuba applications, but are also occasionally used for bailout systems for surface-supplied diving. Gas reclaim systems used for deep heliox diving use similar technology to rebreathers, as do saturation divinglife-support systems, but in these applications the gas recycling equipment is not carried by the diver. Atmospheric diving suits also carry rebreather technology to recycle breathing gas as part of the life-support system, but this article covers the procedures of ambient pressure diving using rebreathers carried by the diver.
Rebreathers are generally more complex to use than open circuit scuba, and have more potential points of failure, so acceptably safe use requires a greater level of skill, attention and situational awareness, which is usually derived from understanding the systems, diligent maintenance and overlearning the practical skills of operation and fault recovery. Fault tolerant design can make a rebreather less likely to fail in a way that immediately endangers the user, and reduces the task loading on the diver which in turn may lower the risk of operator error. (Full article...)
Image 6
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Open-circuit scuba systems discharge the breathing gas into the environment as it is exhaled and consist of one or more diving cylinders containing breathing gas at high pressure which is supplied to the diver at ambient pressure through a diving regulator. They may include additional cylinders for range extension, decompression gas or emergency breathing gas. Closed-circuit or semi-closed circuit rebreather scuba systems allow recycling of exhaled gases. The volume of gas used is reduced compared to that of open-circuit, making longer dives feasible. Rebreathers extend the time spent underwater compared to open-circuit for the same metabolic gas consumption. They produce fewer bubbles and less noise than open-circuit scuba, which makes them attractive to covert military divers to avoid detection, scientific divers to avoid disturbing marine animals, and media divers to avoid bubble interference.
Scuba diving may be done recreationally or professionally in a number of applications, including scientific, military and public safety roles, but most commercial diving uses surface-supplied diving equipment for breathing gas security when this is practicable. Scuba divers engaged in armed forces covert operations may be referred to as frogmen, combat divers or attack swimmers.
An atmospheric diving suit (ADS), or single atmosphere diving suit is a small one-person articulated submersible which resembles a suit of armour, with elaborate pressure joints to allow articulation while maintaining an internal pressure of one atmosphere. An ADS can enable diving at depths of up to 2,300 feet (700 m) for many hours by eliminating the majority of significant physiological dangers associated with deep diving. The occupant of an ADS does not need to decompress, and there is no need for special breathing gas mixtures, so there is little danger of decompression sickness or nitrogen narcosis when the ADS is functioning properly. An ADS can permit less skilled swimmers to complete deep dives, albeit at the expense of dexterity.
Atmospheric diving suits in current use include the Newtsuit, Exosuit, Hardsuit and the WASP, all of which are self-contained hard suits that incorporate propulsion units. The Hardsuit is constructed from cast aluminum (forged aluminum in a version constructed for the US Navy for submarine rescue); the upper hull is made from cast aluminum, while the bottom dome is machined aluminum. The WASP is of glass-reinforced plastic (GRP) body tube construction. (Full article...)
Image 9
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 10
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 11
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 12
Surface-supplied divers riding a stage to the underwater workplace
Underwater diving, as an activity, it is the practice of descending below the water's surface to interact with the environment. It is also often referred to as diving, an ambiguous term with several possible meanings, depending on context. Immersion in water and exposure to high ambient pressure have physiological effects that limit the depths and duration possible in ambient pressure diving. Humans are not physiologically and anatomically well-adapted to the environmental conditions of diving, and various equipment has been developed to extend the depth and duration of human dives, and allow different types of work to be done.
In ambient pressure diving, the diver is directly exposed to the pressure of the surrounding water. The ambient pressure diver may dive on breath-hold (freediving) or use breathing apparatus for scuba diving or surface-supplied diving, and the saturation diving technique reduces the risk of decompression sickness (DCS) after long-duration deep dives. Atmospheric diving suits (ADS) may be used to isolate the diver from high ambient pressure. Crewed submersibles can extend depth range to full ocean depth, and remotely controlled or robotic machines can reduce risk to humans.
The environment exposes the diver to a wide range of hazards, and though the risks are largely controlled by appropriate diving skills, training, types of equipment and breathing gases used depending on the mode, depth and purpose of diving, it remains a relatively dangerous activity. Professional diving is usually regulated by occupational health and safety legislation, while recreational diving may be entirely unregulated. Diving activities are restricted to maximum depths of about 40 metres (130 ft) for recreational scuba diving, 530 metres (1,740 ft) for commercial saturation diving, and 610 metres (2,000 ft) wearing atmospheric suits. Diving is also restricted to conditions which are not excessively hazardous, though the level of risk acceptable can vary, and fatal incidents may occur.
Recreational diving (sometimes called sport diving or subaquatics) is a popular leisure activity. Technical diving is a form of recreational diving under more challenging conditions. Professional diving (commercial diving, diving for research purposes, or for financial gain) involves working underwater. Public safety diving is the underwater work done by law enforcement, fire rescue, and underwater search and recovery dive teams. Military diving includes combat diving, clearance diving and ships husbandry. Deep sea diving is underwater diving, usually with surface-supplied equipment, and often refers to the use of standard diving dress with the traditional copper helmet. Hard hat diving is any form of diving with a helmet, including the standard copper helmet, and other forms of free-flow and lightweight demand helmets. The history of breath-hold diving goes back at least to classical times, and there is evidence of prehistoric hunting and gathering of seafoods that may have involved underwater swimming. Technical advances allowing the provision of breathing gas to a diver underwater at ambient pressure are recent, and self-contained breathing systems developed at an accelerated rate following the Second World War. (Full article...)
Image 13
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.
Airline, or hookah diving, and "compressor diving" are lower technology variants also using a breathing air supply from the surface. (Full article...)
Image 14
Surface-supplied diver at the Monterey Bay Aquarium, Monterey, California Surface-supplied diving is a mode of underwater diving using equipment supplied with breathing gas through a diver's umbilical from the surface, either from the shore or from a diving support vessel, sometimes indirectly via a diving bell. This is different from scuba diving, where the diver's breathing equipment is completely self-contained and there is no essential link to the surface. The primary advantages of conventional surface supplied diving are lower risk of drowning and considerably larger breathing gas supply than scuba, allowing longer working periods and safer decompression. Disadvantages are the absolute limitation on diver mobility imposed by the length of the umbilical, encumbrance by the umbilical, and high logistical and equipment costs compared with scuba. The disadvantages restrict use of this mode of diving to applications where the diver operates within a small area, which is common in commercial diving work.