Rift lake

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Faulted southeastern side of Svyatoy Nos peninsula, Lake Baikal – active faulting shown by faceted spurs.

A rift lake is a lake formed as a result of subsidence related to movement on faults within a rift zone, an area of extensional tectonics in the continental crust. They are often found within rift valleys and may be very deep. Rift lakes may be bounded by large steep cliffs along the fault margins.

Examples[edit]

References[edit]

  1. ^ Lake Vostok Workshop (1998). "Lake Vostok: A Curiosity or a Focus for Interdisciplinary Study?". p. 83. Retrieved 29 January 2010. 
  2. ^ Marshall,J.E.A. & Hewett,A.J. 2003. Devonian. In: Evans, D., Graham, C., Armour, A. & Bathurst, P. (eds): The Millennium Atlas: petroleum geology of the central and northern North Sea. London, the Geological Society of London, 65–81.
  3. ^ Stones of Princeton