Mineralogical and geochemical evidence of weathering in a middle to late Pleistocene paleosol sequence in the Driftless Area of Wisconsin
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DOI: 10.1017/qua.2017.85
Abstract: Abstract Paleosols occur in the Driftless Area of southwestern Wisconsin because this area escaped direct Pleistocene glaciation, allowing long-term loess and colluvium accumulation in selected settings. The most complete known depositional sequence at Oil City,… read more here.
Keywords: mineralogy; driftless area; area; pleistocene ... See more keywords