Temporal and spatial variability in dune reactivation across the Nebraska Sand Hills, USA

The Nebraska Sand Hills is a stabilized dune field on the Great Plains of North America. Although it is well known that this dune field, like several others on the Great Plains, last experienced widespread activity during the Medieval Climatic Anomaly (MCA, ~AD 900–1300), spatial variation in the ti...

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Veröffentlicht in:	Holocene (Sevenoaks) 2015-03, Vol.25 (3), p.523-535
Hauptverfasser:	Schmeisser McKean, Rebecca L, Goble, Ronald J, Mason, Joseph B, Swinehart, James B, Loope, David B
Format:	Artikel
Sprache:	eng
Schlagworte:	Geological time Sand & gravel
Online-Zugang:	Volltext
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