Item talk:Q230646
From geokb
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"abstract": "Loess and eolian sand cover vast areas of the western Great \nPlains of Nebraska, Kansas and Colorado (Fig. 1). In recent \nstudies of Quaternary climate change, there has been a renewed \ninterest in loess and eolian sand. Much of the attention now \ngiven to loess stems from new studies of long loess sequences \nthat contain detailed records of Quaternary glacial-interglacial \ncycles, thought to be a terrestrial equivalent to the foraminiferal \noxygen isotope record in deep-sea sediments (Fig. 2). Loess is \nalso a direct record of atmospheric circulation, and identification \nof loess paleowinds in the geologic record can test atmospheric \ngeneral circulation models. Until recently, eolian sand on \nthe Great Plains had received little attention from Quaternary \ngeologists. The past decade has seen a proliferation of studies of \nGreat Plains dune sands, and many studies, summarized below, \nindicate that landscapes characterized by eolian sand have had \ndynamic histories.\n\nOn this field trip, we will visit some key eolian sand and \nloess localities in eastern Colorado and southwestern Nebraska \n(Fig. 1). Stratigraphic studies at some of these localities have \nbeen conducted for more than 50 years, but others have been \nsystematically studied only in the past few years. Many of the \ndata which appear in this guidebook have been derived from \nprevious studies (Swinehart and Diffendal, 1990; Madole, \n1994; Loope and others, 1995; Maat and Johnson, 1996; Muhs \nand others, 1996, 1997a, 1999; Mason and others, 1997; \nAleinikoff and others, 1999), but some are presented here for \nthe first time.",
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