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Glacier Lakes
Lakes formed on surface of glaciers
Moraine
Debris deposited by a glacier
Subglacial lakes
Formed under glaciers in basins scoured by glacial activity
Cirque Lakes
Formed by downslope movement of glacier carves out depression in mountains
Paternoster Lakes
Chains of lakes associated with cirques
Kettle Lakes
Formed when ice block caught in glacial drift and then melted
Devil’s Lake
Glacial Lake
Lake Vostok
Subglacial Lake
Blanca Lake
Cirque Lake
Morris Lakes / most lakes in WI
Kettle Lake
Riverine Lakes
Lake that forms directly within a river valley, floodplain, or river channel, remaining closely connected to the flow and hydrology of a river
Oxbow Lakes
Formed when portion of meandering river is cutoff from flowing channel
Plunge Lake
Formed at base of waterfall
Floodplain lake
Formed in a low-lying area near river channel, does not receive much flow
Reservoirs
Formed by humans damming a river
Earthslide Lakes
Formed when release materials forms a dam or within the depression remaining after material is released
Tectonic Lakes
Formed by movements of Earth’s crust
Faulting
Troughs can form and fill with water, often deep
Graben Lakes
Formed in a downfaulted trough
Lawrence Lake
Floodplain lake
Hoover dam
Reservoir
Lake Baikal
Graben Lake
Lake Tanganika
Graben Lake
Lake Tahoe
Graben Lake
Uplift Lakes
Depressions creased by tectonic uplift (depressions in a sea floor that are uplifted)
Endoheic Water
Water comes in, but can’t leave, water evaporates, leaving behind salt
Caldera Lakes
Cone of erupted volcano, fills with precipitations with small watershed
Maar Lake
Underground magma mixes with groundwater and explode, leaving a crater
Caspian Sea
Uplift
Aral Sea
Uplift
The Great Lakes
Uplift
Crater Lake
Caldera Lake
Dissolution/Karst/Solution Lakes
Formed by dissolving of rock by water perculating through ground
Erosional Lakes
Wind erosion forms basins in sandy areas
Shoreline Lakes
Wave action can move shoreline material and close off a coastal area forming a lake
Red Lake
Dissolution/Karst/Solution
Chequamegan Bay in Lake Superior
Shoreline Lake
Seepage Lake
No inlet or outlet, only some overflow. Principal source of water is precipitation or runoff
Drainage Lake
Surface outlet and maybe inlet (Ex. Great Lakes)
Troph
Food, organic matter, carbon
Autotrophy
Food produced within lake
Oligotrophic
Low Producitivity
Mesotrophic
Intermediate productivity
Eutrophic
High productivity
Allotrophy
Food comes in
Dystrophic
Lake with stained water
Ombrotrophic
Water and nutrients supplied by rain water
Rheotrophic
Water and nutrients supplied by drainage
Minerotrophic
Water and nutrients supplied by groundwater