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Kristy E Stanley

Biographic Data

ID5232345
NAMEKristy E Stanley
GIVEN NAMESKristy E
FAMILY NAMEStanley
SIGNATURESTANLEY K E
AFFILIATIONSUniversity of Wisconsin–Madison
VERIFIEDNo
TOTAL WORKS1
TOTAL CITATIONS1
WORKS AS AUTHOR1
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2009
LATEST PUBLICATION YEAR2009
H-INDEX1
  • Characterization and Mapping of Patterned Ground in the Saginaw Lowlands, Michigan

    David P Lusch, Kristy E Stanley et al.•ARTICLE•Annals of the Association of…•2009•Cited by: 1•References: 48

    We identified, mapped, and characterized a widespread area (>1,020 km2) of patterned ground in the Saginaw Lowlands of Michigan, a wet, flat plain composed of waterlain tills, lacustrine deposits, or both. The polygonal patterned ground is interpreted as a possible relict permafrost feature, formed in the Late Wisconsin when this area was proximal to the Laurentide ice sheet. Cold-air drainage off the ice sheet might have pooled in the Saginaw Lo…

  • Characterization and Mapping of Patterned Ground in the Saginaw Lowlands, Michigan

    David P Lusch, Kristy E Stanley et al.•ARTICLE•Annals of the Association of…•2009•Cited by: 1•References: 48

    We identified, mapped, and characterized a widespread area (>1,020 km2) of patterned ground in the Saginaw Lowlands of Michigan, a wet, flat plain composed of waterlain tills, lacustrine deposits, or both. The polygonal patterned ground is interpreted as a possible relict permafrost feature, formed in the Late Wisconsin when this area was proximal to the Laurentide ice sheet. Cold-air drainage off the ice sheet might have pooled in the Saginaw Lo…

  • Characterization and Mapping of Patterned Ground in the Saginaw Lowlands, Michigan

    David P Lusch, Kristy E Stanley et al.•ARTICLE•Annals of the Association of…•2009•Cited by: 1•References: 48

    We identified, mapped, and characterized a widespread area (>1,020 km2) of patterned ground in the Saginaw Lowlands of Michigan, a wet, flat plain composed of waterlain tills, lacustrine deposits, or both. The polygonal patterned ground is interpreted as a possible relict permafrost feature, formed in the Late Wisconsin when this area was proximal to the Laurentide ice sheet. Cold-air drainage off the ice sheet might have pooled in the Saginaw Lo…

Climate change and permafrost (1 work) · Cryospheric studies and observations (1 work) · Geography (1 work) · Geology (1 work) · Geology (1 work) · Geology and Paleoclimatology Research (1 work) · Geomorphology (1 work) · Glacial period (1 work) · Loam (1 work) · Oceanography (1 work)

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