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C A Scott Smith

Biographic Data

ID7511210
NAMEC A Scott Smith
GIVEN NAMESC A Scott
FAMILY NAMESmith
SIGNATURESMITH C A S
VERIFIEDNo
TOTAL WORKS3
TOTAL CITATIONS0
WORKS AS AUTHOR3
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1994
LATEST PUBLICATION YEAR2006
H-INDEX0
  • Full-glacial paleosols in perennially frozen loess sequences, Klondike goldfields, Yukon Territory, Canada

    Open Access•Paul Sanborn, Paul T Sanborn et al.•ARTICLE•Quaternary Research•2006

    Perennially frozen loess deposits in the Klondike goldfields include paleosols formed in full-glacial environments, correlated by Alaskan distal tephra with Marine Isotope Stages (MIS) 2 and 4. Patterns of organic and inorganic carbon and clay distribution, microstructures, and profile morphologies indicate that soil formation occurred in a base-rich environment in which organic matter accreted predominantly as root detritus. At sites approximate…

  • Paleosols associated with Miocene basalts, Porcupine River, northeastern Alaska

    Open Access•C A Scott Smith, C A Fox et al.•ARTICLE•Quaternary International•1994

  • Miocene and Pliocene lacustrine and fluvial sequences, Upper Ramparts and Canyon village, Porcupine river, east-central Alaska

    Open Access•Thomas D Fouch, L David Carter et al.•ARTICLE•Quaternary International•1994

No prominent works on this page.

  • Paleosols associated with Miocene basalts, Porcupine River, northeastern Alaska

    Open Access•C A Scott Smith, C A Fox et al.•ARTICLE•Quaternary International•1994

  • Miocene and Pliocene lacustrine and fluvial sequences, Upper Ramparts and Canyon village, Porcupine river, east-central Alaska

    Open Access•Thomas D Fouch, L David Carter et al.•ARTICLE•Quaternary International•1994

  • Full-glacial paleosols in perennially frozen loess sequences, Klondike goldfields, Yukon Territory, Canada

    Open Access•Paul Sanborn, Paul T Sanborn et al.•ARTICLE•Quaternary Research•2006

    Perennially frozen loess deposits in the Klondike goldfields include paleosols formed in full-glacial environments, correlated by Alaskan distal tephra with Marine Isotope Stages (MIS) 2 and 4. Patterns of organic and inorganic carbon and clay distribution, microstructures, and profile morphologies indicate that soil formation occurred in a base-rich environment in which organic matter accreted predominantly as root detritus. At sites approximate…

Geology and Paleoclimatology Research (3 works) · Geomorphology (3 works) · Climate change and permafrost (2 works) · Fluvial (2 works) · Geochemistry (2 works) · Geology (2 works) · Paleosol (2 works) · Structural basin (2 works) · Archaeology (1 work) · Arctic (1 work)

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