Difference between revisions of "Aeolian Sand Transport"

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'''2016'''
 
'''2016'''
*[[Media:Collins 2016 GCArchSitesAeolian.pdf| Collins et al. 2016. Relations between rainfall–runoff-induced erosion and aeolian deposition at archaeological sites in a semi-arid dam-controlled river corridor, 19 p., Earth Surf. Process. Landforms]]
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*[[Media:Collins 2016 GCArchSitesAeolian.pdf| Collins et al. 2016. Relations between rainfall–runoff-induced erosion and aeolian deposition at archaeological sites in a semi-arid dam-controlled river corridor, Earth Surf. Process. Landforms]]
 
*[https://pubs.er.usgs.gov/publication/pp1825 East et. al. 2016. Conditions and processes affecting sand resources at archeological sites in the Colorado River corridor below Glen Canyon Dam, Arizona: U.S. Geological Survey Professional Paper]
 
*[https://pubs.er.usgs.gov/publication/pp1825 East et. al. 2016. Conditions and processes affecting sand resources at archeological sites in the Colorado River corridor below Glen Canyon Dam, Arizona: U.S. Geological Survey Professional Paper]
  

Revision as of 13:51, 6 December 2016




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Updates

Collin et al. 2016: Aeolian deposition was found at 4 sites (30%) where partial infilling occurred preventing further erosion. “Despite this promise for archaeological site preservation, our observations show that gully annealing can only occur under a specific set of conditions related to fluvial sand availability and wind transport direction.”

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2016

2014

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