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] (DOI:10.1016/j.yqres.2009.02.001);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

Volumn 71, Issue 3, 2009, Pages 409-425

  Markewich, Helaine W ^a   Litwin, Ronald J ^a   Pavich, Milan J ^a   Brook, George A ^b  

^a U S GEOLOGICAL SURVEY   (United States)

^b UNIVERSITY OF GEORGIA   (United States)

Author keywords

Chesapeake Bay region; Dune; Eolian; Last glacial maximum; Late Pleistocene; Paha; Paleowind

Indexed keywords

DUNE; EOLIAN DEPOSIT; EROSION; FINE GRAINED SEDIMENT; LAST GLACIAL MAXIMUM; LAURENTIDE ICE SHEET; PLEISTOCENE;

CHESAPEAKE BAY; MARYLAND; NORTH AMERICA; POTOMAC RIVER; UNITED STATES;

EID: 63649128825     PISSN: 00335894     EISSN: 10960287     Source Type: Journal    
DOI: 10.1016/j.yqres.2009.09.003     Document Type: Erratum

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