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By David K. Brezinski
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Published through the yankee Geophysical Union as a part of the Field journey Guidebooks Series.
During the most recent Devonian and early Mississippian the northern Appalachian sector used to be positioned at nearly 10 to twenty levels south range (Figure 2) (Scotese et al., 1979). The Appalachian foreland basin was once bordered to the southeast by way of a tectonic highland created via the upcoming collision of the North American and African continents. The downwarping because of this collision allowed primarily non-stop accumulation of sediments in western Maryland. during this region the newest Devonian and early Mississip pian sediments are unbroken via significant unconformities (Scheckler, 1986).
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Extra resources for Lower Mississippian Foreland Basin Deposits of Western Maryland: Hancock to Keysers Ridge, Maryland July 14, 1989
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1991), Olson (1981, 1984), Soil Survey Staff (1951, 1962, 1992, 1994, 1999, 2002), Webster (1977); Contaminated Sites: Boulding (1991, 1994), Burden and Sims (1999), Cameron (1991) Brewer (1976), Brewer and Sleeman (1988), Bullock and Murphy (1983), Bullock et al. (1985), Douglas (1990), Douglas and Thompson (1985), Fitzpatrick (1984, 1993), Hartge and Stewart (1995-soil structure), Miedema and Mermut (1990), Stoops and Eswarin (1986), Thompson et al. (1993) Geomorphology General Chorley et al.
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