Difference between revisions of "Aeolian Sand Transport"

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'''Collin et al. 2016:'''  
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[[Media:Collins 2016 GCArchSitesAeolian.pdf| '''Collin et al. 2016:''' ]]
 
*Aeolian deposition was found at 4 sites (30%) where partial infilling occurred preventing further erosion.  
 
*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.”  
 
*“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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Revision as of 13:43, 23 March 2017




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Updates

AeolianClassification.jpg
[1]
AeolianCulturalSites.jpg
[2]

Of 358 river-corridor arch sites (RM 0-240), 74 (21%) are adjacent and upwind of sandbars receiving HFE sand (Type 1 and Type 2a) that don't have some sort of topographic barrier. Of these, 43 sites are currently blocked by vegetation from receiving aeolian sand.

Links

Questions

  • Does Aeolian sand transport research support the use of anthropogenic sand bar building as a means to provide a source of aeolian sands to preserve and protect archaeological sites?
  • ...or would current stabilization measures carried out by the NPS be more likely to be successful, predictable, and immediate at protecting archaeological sites?

Presentations and Papers

2016

2014

Other Stuff

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.”