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HandWiki. River Anticlines. Encyclopedia. Available online: https://encyclopedia.pub/entry/37645 (accessed on 21 September 2026).
HandWiki. River Anticlines. Encyclopedia. Available at: https://encyclopedia.pub/entry/37645. Accessed September 21, 2026.
HandWiki. "River Anticlines" Encyclopedia, https://encyclopedia.pub/entry/37645 (accessed September 21, 2026).
HandWiki. (2022, December 01). River Anticlines. In Encyclopedia. https://encyclopedia.pub/entry/37645
HandWiki. "River Anticlines." Encyclopedia. Web. 01 December, 2022.
River Anticlines
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A river anticline is a geologic structure that is formed by the focused uplift of rock caused by high erosion rates from large rivers relative to the surrounding areas. An anticline is a fold that is concave down, whose limbs are dipping away from its axis, and whose oldest units are in the middle of the fold. These features form in a number of structural settings. In the case of river anticlines, they form due to high erosion rates, usually in orogenic settings. In a mountain building setting, like that of the Himalaya or the Andes, erosion rates are high and the river anticline's fold axis will trend parallel to a major river. When river anticlines form, they have a zone of uplift between 50-80 kilometers wide along the rivers that form them.

large rivers anticline anticlines

References

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  2. Simpson, Guy (1 January 2004). "Role of river incision in enhancing deformation". Geology 32 (4): 341. doi:10.1130/G20190.2. Bibcode: 2004Geo....32..341S.  https://dx.doi.org/10.1130%2FG20190.2
  3. Zeitler, Peter K.; Anne S. Meltz (January 2001). "Erosion, Himalayan geodynamics, and the geomorphology of metamorphism". GSA Today 11: 4–9. doi:10.1130/1052-5173(2001)011<0004:EHGATG>2.0.CO;2.  https://dx.doi.org/10.1130%2F1052-5173%282001%29011%3C0004%3AEHGATG%3E2.0.CO%3B2
  4. Burbank; McLean, Bullen; Abdrakhmatov, Miller (1 March 1999). "Partitioning of intermontane basins by thrust-related folding, Tien Shan, Kyrgyzstan". Basin Research 11 (1): 75–92. doi:10.1046/j.1365-2117.1999.00086.x.  https://dx.doi.org/10.1046%2Fj.1365-2117.1999.00086.x
  5. Marshak, Ben A. van der Pluijm, Stephan (2004). Earth Structure: An Introduction to Structural Geology and Tectonics (2nd ed.). New York: Norton. pp. 353–354. ISBN 978-0-393-92467-1. 
  6. England, Phillip; Peter Molnar (December 1990). "Surface uplift, uplift of rocks, and Exhumation of rocks". Geology 18 (12): 1173–1177. doi:10.1130/0091-7613(1990)018<1173:SUUORA>2.3.CO;2. Bibcode: 1990Geo....18.1173E.  https://dx.doi.org/10.1130%2F0091-7613%281990%29018%3C1173%3ASUUORA%3E2.3.CO%3B2
  7. Lavé, J.; Avouac, J. P. (1 January 2001). "Fluvial incision and tectonic uplift across the Himalayas of central Nepal". Journal of Geophysical Research 106 (B11): 26561–26591. doi:10.1029/2001JB000359. Bibcode: 2001JGR...10626561L. https://authors.library.caltech.edu/33975/1/LaveAvouacJGR2001.pdf. 
  8. Zeitler, P.K.; Peter O. Koons; Michael P. Bishop (October 2001). "Crustal reworking at Nanga Parbat, Pakistan: metamorphic consequences of thermo-mechanical coupling facilitated by erosion". Tectonics. 5 20 (5): 712–728. doi:10.1029/2000TC001243. Bibcode: 2001Tecto..20..712Z.  https://dx.doi.org/10.1029%2F2000TC001243
  9. Ding, Lin; Zhong, Dalai; Yin, An; Kapp, Paul; Harrison, T. Mark (1 October 2001). "Cenozoic structural and metamorphic evolution of the eastern Himalayan syntaxis (Namche Barwa)". Earth and Planetary Science Letters 192 (3): 423–438. doi:10.1016/S0012-821X(01)00463-0. Bibcode: 2001E&PSL.192..423D.  https://dx.doi.org/10.1016%2FS0012-821X%2801%2900463-0
  10. Zeitler, P., Hallet, B., & Koons, P. (2013). Tectonic aneurysms and mountain building
  11. Booth, A. L.; Chamberlain, C. P.; Kidd, W. S. F.; Zeitler, P. K. (2009). "Constraints on the metamorphic evolution of the eastern himalayan syntaxis from geochronologic and petrologic studies of namche barwa". GSA Bulletin 121 (3–4): 385–407. doi:10.1130/B26041.1.  https://dx.doi.org/10.1130%2FB26041.1
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  13. Finnegan, N. J.; Hallet, B.; Montgomery, D. R.; Zeitler, P. K.; Stone, J. O.; Anders, A. M.; Yuping, L. (4 January 2008). "Coupling of rock uplift and river incision in the Namche Barwa-Gyala Peri massif, Tibet". Geological Society of America Bulletin 120 (1–2): 142–155. doi:10.1130/B26224.1.  https://dx.doi.org/10.1130%2FB26224.1
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