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- River_anticlines abstract "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.".
- River_anticlines wikiPageID "33737566".
- River_anticlines wikiPageLength "9066".
- River_anticlines wikiPageOutDegree "28".
- River_anticlines wikiPageRevisionID "674984082".
- River_anticlines wikiPageWikiLink Andes.
- River_anticlines wikiPageWikiLink Anticline.
- River_anticlines wikiPageWikiLink Arun_River,_China-Nepal.
- River_anticlines wikiPageWikiLink Asthenosphere.
- River_anticlines wikiPageWikiLink Category:Erosion.
- River_anticlines wikiPageWikiLink Category:Tectonics.
- River_anticlines wikiPageWikiLink Density.
- River_anticlines wikiPageWikiLink Erosion.
- River_anticlines wikiPageWikiLink Eurasian_Plate.
- River_anticlines wikiPageWikiLink File:River_anticline_by,_Michael_Stevens.pdf.
- River_anticlines wikiPageWikiLink Himalayas.
- River_anticlines wikiPageWikiLink Indian_Plate.
- River_anticlines wikiPageWikiLink Indus_River.
- River_anticlines wikiPageWikiLink Isostasy.
- River_anticlines wikiPageWikiLink Lithosphere.
- River_anticlines wikiPageWikiLink Metamorphic_rock.
- River_anticlines wikiPageWikiLink Namcha_Barwa.
- River_anticlines wikiPageWikiLink Nanga_Parbat.
- River_anticlines wikiPageWikiLink Post-glacial_rebound.
- River_anticlines wikiPageWikiLink Radiometric_dating.
- River_anticlines wikiPageWikiLink Sutlej.
- River_anticlines wikiPageWikiLink Thrust_fault.
- River_anticlines wikiPageWikiLink Yarlung_Tsangpo_River.
- River_anticlines wikiPageWikiLinkText "River anticlines".
- River_anticlines wikiPageWikiLinkText "tectonic aneurysm".
- River_anticlines wikiPageUsesTemplate Template:Reflist.
- River_anticlines subject Category:Erosion.
- River_anticlines subject Category:Tectonics.
- River_anticlines hypernym Structure.
- River_anticlines type Building.
- River_anticlines type Process.
- River_anticlines comment "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.".
- River_anticlines label "River anticlines".
- River_anticlines sameAs Q7337987.
- River_anticlines sameAs m.0hhvknh.
- River_anticlines sameAs Q7337987.
- River_anticlines wasDerivedFrom River_anticlines?oldid=674984082.
- River_anticlines isPrimaryTopicOf River_anticlines.