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Corrigendum to “Late Pleistocene eolian features in southeastern Maryland and Chesapeake Bay region indicate strong WNW–NW winds accompanied growth of the Laurentide Ice Sheet” [Quaternary Research 71 (2009) 409–425]

Published online by Cambridge University Press:  20 January 2017

Helaine W. Markewich*
Affiliation:
U.S. Geological Survey, 3039 Amwiler Rd., Ste. 130, Peachtree Business Center, Atlanta, GA 30360-2824, USA
Ronald J. Litwin
Affiliation:
U.S. Geological Survey, Reston, VA, USA
Milan J. Pavich
Affiliation:
U.S. Geological Survey, Reston, VA, USA
George A. Brook
Affiliation:
University of Georgia Department of Geography, Athens, GA, USA
*
*Corresponding author. Fax: +1 770 903 9199.E-mail address:helainem@usgs.gov (H.W. Markewich).

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Copyright
University of Washington

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Corrigendum to “Late Pleistocene eolian features in southeastern Maryland and Chesapeake Bay region indicate strong WNW–NW winds accompanied growth of the Laurentide Ice Sheet” [Quaternary Research 71 (2009) 409–425]
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Corrigendum to “Late Pleistocene eolian features in southeastern Maryland and Chesapeake Bay region indicate strong WNW–NW winds accompanied growth of the Laurentide Ice Sheet” [Quaternary Research 71 (2009) 409–425]
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Corrigendum to “Late Pleistocene eolian features in southeastern Maryland and Chesapeake Bay region indicate strong WNW–NW winds accompanied growth of the Laurentide Ice Sheet” [Quaternary Research 71 (2009) 409–425]
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