Glacial Processes Past and Present 1999
DOI: 10.1130/0-8137-2337-x.93
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Origin of the Driftless Area by subglacial drainage - a new hypothesis

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Cited by 18 publications
(24 citation statements)
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“…The region lacks glacial drift characteristic of retreating ice, hence its name, and there has been extensive debate as to whether it remained unglaciated at the LGM (Jacobs et al. , 1997; Hobbs, 1999). Phylogeographic (Jaramillo‐Correa et al.…”
Section: Discussionmentioning
confidence: 99%
“…The region lacks glacial drift characteristic of retreating ice, hence its name, and there has been extensive debate as to whether it remained unglaciated at the LGM (Jacobs et al. , 1997; Hobbs, 1999). Phylogeographic (Jaramillo‐Correa et al.…”
Section: Discussionmentioning
confidence: 99%
“…1). This geologically unique region was circumvented by ice during the most recent glaciation (Hobbs, 1999) and is characterized by a loess-capped plateau and steep ravines formed by several large rivers that flow through the region. Prairie soils can be found on the ridges, with thick silt loams (loess) covering cherty residuum, with an underlying dolomite bedrock, and silt loam over sandstone on valley walls found in some parts of the region (Albert, 1995).…”
Section: Study Areamentioning
confidence: 99%
“…This 55,000 km2 region is composed of portions of southwestern Wisconsin, southeastern Minnesota, northeastern Iowa, and northwestern Illinois (Figure 1) not covered by glacial ice during the Late Wisconsin glaciation of the Quaternary Period (Hobbs 1999). Because it escaped this most recent glacial advance, the region has high levels of topographic variation and contains a distinctive array of plant communities and several preglacial relict species absent from surrounding regions (Curtis 1971, USFWS 2006.…”
Section: Meters Riversmentioning
confidence: 99%