Allochthon

For the Dutch demographical term, see Allochtoon.
Schematic overview of a thrust system. The hanging wall block is (when it has reasonable proportions) called a nappe. If an erosional hole is created in the nappe that is called a window. A klippe is a solitary outcrop of the nappe in the middle of autochthonous material.

In structural geology, an allochthon, or an allochthonous block, is a large block of rock which has been moved from its original site of formation, usually by low angle thrust faulting.[1] An allochthon which is isolated from the rock that pushed it into position is called a klippe. If an allochthon has a "hole" in it so that one can view the autochthon beneath the allochthon, the hole is called a "window" (or Fenster). Etymology: Greek; 'allo' = other, and 'chthon' = earth.

In limnology, allochthonous sources of carbon or nutrients come from outside the aquatic system (such as plant and soil material). Carbon sources from within the system, such as algae and the microbial breakdown of particulate organic carbon, are autochthonous. In streams and small lakes, allochthonous sources of carbon are dominant while in large lakes and the ocean, autochthonous sources dominate.[2]

The term "allochthonous" is also used in the social sciences, as the opposite to autochthonous.

See also

References

  1. ↑ DiPietro, Joseph A. (December 21, 2012). Landscape Evolution in the United States: An Introduction to the Geography, Geology, and Natural History. Newnes. p. 343. ISBN 9780123978066. Retrieved 10 February 2016.
  2. ↑ Eby, G.N., 2004, Principles of Environmental Geochemistry: Thomson Brooks/Cole, Pacific Grove, CA., 514 pp.
This article is issued from Wikipedia - version of the Thursday, February 11, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.