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]]
 
*[[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]]
*[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 1825, 104 p., http://dx.doi.org/10.3133/pp1825.]
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*[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]
  
 
'''2014'''
 
'''2014'''

Revision as of 13:50, 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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Presentations and Papers

2016

2014

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