World Library  
Flag as Inappropriate
Email this Article

Epeirogenic movement

Article Id: WHEBN0010534187
Reproduction Date:

Title: Epeirogenic movement  
Author: World Heritage Encyclopedia
Language: English
Subject: Orogeny, Magmatic underplating, Geology of North America
Collection: Geological Processes
Publisher: World Heritage Encyclopedia
Publication
Date:
 

Epeirogenic movement

In geology, epeirogenic movement (from Greek epeiros, land, and genesis, birth) refers to upheavals or depressions of land exhibiting long wavelengths and little folding apart from broad undulations.[1] The broad central parts of continents are called cratons, and are subject to epeirogeny.[2] The movement may be one of subsidence toward, or of uplift from, the centre of the Earth. The movement is caused by a set of forces acting along an Earth radius, such as those contributing to isostasy and faulting in the lithosphere.

Epeirogenic movement can be permanent or transient. Transient uplift can occur over a thermal anomaly due to convecting anomalously hot mantle, and disappears when convection wanes. Permanent uplift can occur when igneous material is injected into the crust, and circular or elliptical structural uplift (that is, without folding) over a large radius (tens to thousands of km) is one characteristic of a mantle plume.[3][4]

Epeirogenic movement has caused the southern Rocky Mountain region to be uplifted from 1300 to 2000 m since the Eocene. This followed and is distinct from the creation of the Rocky Mountains during the Laramide Orogeny during the Late Cretaceous–early Cenozoic. The uplift is interpreted as due to lithospheric heating resulting from thinning and the intrusion of widespread middle Tertiary batholiths of relatively low density.[5]

In contrast to epeirogenic movement, orogenic movement is a more complicated deformation of the Earth's crust, associated with crustal thickening, notably associated with the convergence of tectonic plates. Such plate convergence forms orogenic belts that are characterized by "the folding and faulting of layers of rock, by the intrusion of magma, and by volcanism".[6][7]

References

  1. ^ Arthur Holmes, Doris L. Holmes (2004). Holmes principles of physical geology (4th ed.). Taylor & Francis. p. 92.  
  2. ^ Richard J. Huggett (2003). Fundamentals of geomorphology. Routledge. p. 76.  
  3. ^ AMC Şengör (2001). "Elevation as an indicator of mantle-plume activity". In Richard E. Ernst, Kenneth L. Buchan. Mantle plumes: their identification through time. Geological Society of America. p. 215.  
  4. ^ SP Holford et al. (2008). "Neogene exhumation in the Irish Sea area". In Howard Johnson et al.. The nature and origin of compression in passive margins. Geological Society. p. 112.  
  5. ^ Eaton, Gordon P., Epeirogeny in the Southern Rocky Mountains region: Evidence and origin, Geosphere; October 2008; v. 4; no. 5; p. 764–784; doi:10.1130/GES00149.1
  6. ^ Frank Northen Magill (1990). Volume 5Magill's survey of science: Earth science series,. Salem Press. p. 2498.  
  7. ^ Robert J. Twiss, Eldridge M. Moores (1992). Structural geology (2nd ed.). Macmillan. p. 217.  
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and USA.gov, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
 
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
 
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.
 


Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.