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Crater lake

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This page describes the geological feature. For the lake of the same name, see Crater Lake.

A crater lake is a lake that forms in a volcanic calderas or craters after the volcano has been inactive for some time. The best-known crater lake, which bears the same name as the geological feature, is Crater Lake in Oregon state's Mount Mazama. Some crater lakes are acidic; however, some lakes' water remains fresh. Some also have geothermal activity, especially if the volcano is merely dormant rather than extinct.

File:Maar.jpg
Ukinrek Maars, Alaska; the result of a 10-day eruption in 1977. Maar is about 300 m in diameter.

A maar is a broad, low relief crater that is caused by a phreatic eruption or explosion caused by groundwater contact with hot lava or magma. The maar typically fills with water to form a relatively shallow crater lake.

Some crater lakes form in craters formed by impact events. Lacking ongoing volcanic processes, these do not tend to develop acidity or geothermal activity.

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