Global InformationEpeirogenic movement information
In geology, epeirogenic movement (from Greek epeiros, land, and genesis, birth) is 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 center of 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]
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".[5][6]
Epeirogenic movements may divert rivers and create drainage divides by upwarping of the crust along axes.[7][8] Example of this is the deflection of Eridanos River in the Pliocene Epoch by the uplift of the South Swedish Dome[7] or the present-day drainage divides between Limpopo and Zambezi rivers in southern Africa.[8]
- ^ Arthur Holmes; Doris L. Holmes (2004). Holmes principles of physical geology (4th ed.). Taylor & Francis. p. 92. ISBN 0-7487-4381-2.
- ^ Richard J. Huggett (2003). Fundamentals of geomorphology. Routledge. p. 76. ISBN 0-415-24146-4.
- ^ Şengör, A.M.C. (2001). "Elevation as an indicator of mantle-plume activity". In Richard E. Ernst, Kenneth L. Buchan (ed.). Mantle plumes: their identification through time. Geological Society of America. p. 215. ISBN 0-8137-2352-3.
- ^ Holford, S.P.; et al. (2008). "Neogene exhumation in the Irish Sea area". In Johnson, Howard; et al. (eds.). The nature and origin of compression in passive margins. Geological Society. p. 112. ISBN 978-1-86239-261-8.
- ^ Frank Northen Magill (1990). Magill's survey of science: Earth science series, Volume 5. Salem Press. p. 2498. ISBN 0-89356-611-X.
- ^ Robert J. Twiss, Eldridge M. Moores (1992). Structural geology (2nd ed.). Macmillan. p. 217. ISBN 0-7167-2252-6.
Orogenic belts are all characterized by a number of fold systems.
- ^ a b Lidmar-Bergström, Karna; Olvmo, Mats; Bonow, Johan M. (2017). "The South Swedish Dome: a key structure for identification of peneplains and conclusions on Phanerozoic tectonics of an ancient shield". GFF. 139 (4): 244–259. doi:10.1080/11035897.2017.1364293. S2CID 134300755.
- ^ a b Moore, A.E. (1999). "A reapprisal of epeirogenic flexure axes in southern Africa". South African Journal of Geology. 102 (4): 363–376.