Depression (geology)

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A depression in geology is a landform sunken or depressed below the surrounding area. Depressions may be formed by various mechanisms.

Structural or tectonic related:

Sedimentary related:

Glaciation related:

  • A basin formed by glaciation - depressed by the weight of the ice sheet resulting in post-glacial rebound after the ice melts (the area adjacent to the ice sheet may be pulled down to create a peripheral depression.)[2]
  • Kettle: a shallow, sediment-filled body of water formed by melting glacial remnants in terminal moraine.[3]

Volcanism related:

Erosion related:

Impact related:

[edit] References

  1. ^ a b "Dictionary of Geologic Terms - B". geotech.org. http://www.geotech.org/survey/geotech/dictiona.html#sectB. Retrieved 2006-08-25. 
  2. ^ "Glossary of Important Terms in Glacial Geology - Peripheral Depression". Montana State University. 1999. http://gemini.oscs.montana.edu/~geol445/hyperglac/glossary.htm#peripheral. Retrieved 2006-08-25.  Cites American Geological Institute’s Glossary of Geology (3rd edition, revised in 1987).
  3. ^ "Dictionary of Geologic Terms - K". geotech.org. http://www.geotech.org/survey/geotech/dictiona.html#sectK. Retrieved 2006-08-26. 
  4. ^ "Dictionary of Geologic Terms - C". geotech.org. http://www.geotech.org/survey/geotech/dictiona.html#sectC. Retrieved 2006-08-25. 
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