Very deep lakes may have emerged from tectonic movements, ie when crustal blocks sink; round and maybe high edges formed when collapsed or flew the crater of a volcano; elongated could be remnants of glacial valleys; finally, of crescent shaped product is usually in latest river changes course. However, none of these freshwater bodies is permanent (clear lake veterinarian).
Examples are Crater Lakes United States and many lakes of Kuril Islands. Lakes caldera, formed in a volcanic caldera as eg. Lakes Toba in Indonesia with 100 Km in length, the Cocibolca in Nicaragua lakes that formed in world's largest caldera and Lakes Cuicocha in Ecuador. Lava lakes formed by molten lava in volcanic crater or surrounding depressions such as Kilauea caldera volcano in Hawaii. Volcanic Reservoir. The emanations of volcanic material can clog river valleys. So Lakes Kivu originated in Africa.
Natural reservoir, produced by collapse of slopes, freezing with formation of ice sheets or small dams built by beavers. Artificial lakes, also called dam, reservoir, and if lower pond. Built for various purposes such as agricultural reservoir, source of drinking water, hydroelectric dam, flood prenvention, to facilitate navigation, recreation, water sports and can usually be a multipurpose reservoir. Best known examples are the Itaipu Dam between Brazil and Paraguay, Guri Dam in Venezuela and the Three Gorges Dam in China.
As the lakes is deeper, more important is the thermal inertia and chemistry of waters. By contrast, some large bodies of surface water and shallow lakes have a sensitivity and respond immediately to environmental changes (climate, hydrology, pollution, human activities). This applies as well, but at other scales to ponds spatiotemporal and seas.
Coastal marsh or lakes, produced by filtration or flood at high tide, given its proximity to sea. They are salt, fresh or brackish water and generally contains sandy bottoms. Estero, produced by filtration or flood floods, given its proximity to rivers or lakes. (Do not confuse with estuary). A floodplain lakes is not considered because no definite basin.
Subglacial lakes, produced by the pressure under great glaciers that maintain liquid water below the ice. In Antarctica there are many subglacial lakes, Lakes Vostok is the largest. Freshwater fjord, where sea level rise becomes fjords ancient glaciers shaped channels lakes, including Lakes Como, Lakes Garda and other sudalpinos lakes in Italy. Laguna lakes formed in an island which in turn is within a lakes, for example: Manitou Lakes Manitoulin Island in Lakes Huron in Ontario, Canada. The folding of earth's crust (lithosphere) create depressions that accommodate the largest lakes. Bark undulates due to pressure, causing rises rounded called "domes".
Between two domes you get to form a depression, or "bucket", which would be caught up Firth sinking and make a pit which usually contains some very deep and very ancient lakes. Lakes Baikal, the deepest in world, Lakes Tanganyika, the second deepest, and the Dead Sea were formed as a result ofse powerful tectonic movements, possibly occurring more than 20 million years ago.
Underground lakes, associated with a cave or cavern with filtered water from an aquifer or a spring, where the roof of caves are dissolved and sinks filled with water are formed. Underground lakes of this type are located in Serbia and in Yucatan, Mexico, the latter called cenotes. Karst or karst lakes, housed in karst depression by surface dissolution of limestone, as seen in Ruidera in Castilla-La Mancha, Spain. The strength of current in plains and plains, open meanders and withinse will come to form gaps with horseshoe and sometimes meandering.
Examples are Crater Lakes United States and many lakes of Kuril Islands. Lakes caldera, formed in a volcanic caldera as eg. Lakes Toba in Indonesia with 100 Km in length, the Cocibolca in Nicaragua lakes that formed in world's largest caldera and Lakes Cuicocha in Ecuador. Lava lakes formed by molten lava in volcanic crater or surrounding depressions such as Kilauea caldera volcano in Hawaii. Volcanic Reservoir. The emanations of volcanic material can clog river valleys. So Lakes Kivu originated in Africa.
Natural reservoir, produced by collapse of slopes, freezing with formation of ice sheets or small dams built by beavers. Artificial lakes, also called dam, reservoir, and if lower pond. Built for various purposes such as agricultural reservoir, source of drinking water, hydroelectric dam, flood prenvention, to facilitate navigation, recreation, water sports and can usually be a multipurpose reservoir. Best known examples are the Itaipu Dam between Brazil and Paraguay, Guri Dam in Venezuela and the Three Gorges Dam in China.
As the lakes is deeper, more important is the thermal inertia and chemistry of waters. By contrast, some large bodies of surface water and shallow lakes have a sensitivity and respond immediately to environmental changes (climate, hydrology, pollution, human activities). This applies as well, but at other scales to ponds spatiotemporal and seas.
Coastal marsh or lakes, produced by filtration or flood at high tide, given its proximity to sea. They are salt, fresh or brackish water and generally contains sandy bottoms. Estero, produced by filtration or flood floods, given its proximity to rivers or lakes. (Do not confuse with estuary). A floodplain lakes is not considered because no definite basin.
Subglacial lakes, produced by the pressure under great glaciers that maintain liquid water below the ice. In Antarctica there are many subglacial lakes, Lakes Vostok is the largest. Freshwater fjord, where sea level rise becomes fjords ancient glaciers shaped channels lakes, including Lakes Como, Lakes Garda and other sudalpinos lakes in Italy. Laguna lakes formed in an island which in turn is within a lakes, for example: Manitou Lakes Manitoulin Island in Lakes Huron in Ontario, Canada. The folding of earth's crust (lithosphere) create depressions that accommodate the largest lakes. Bark undulates due to pressure, causing rises rounded called "domes".
Between two domes you get to form a depression, or "bucket", which would be caught up Firth sinking and make a pit which usually contains some very deep and very ancient lakes. Lakes Baikal, the deepest in world, Lakes Tanganyika, the second deepest, and the Dead Sea were formed as a result ofse powerful tectonic movements, possibly occurring more than 20 million years ago.
Underground lakes, associated with a cave or cavern with filtered water from an aquifer or a spring, where the roof of caves are dissolved and sinks filled with water are formed. Underground lakes of this type are located in Serbia and in Yucatan, Mexico, the latter called cenotes. Karst or karst lakes, housed in karst depression by surface dissolution of limestone, as seen in Ruidera in Castilla-La Mancha, Spain. The strength of current in plains and plains, open meanders and withinse will come to form gaps with horseshoe and sometimes meandering.
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