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Was there a late-Würm Arctic Ice Sheet?

Naturevolume 266pages596602 (1977) | Download Citation

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Abstract

A simplification and synthesis of late-Würm Northern Hemisphere glaciation is possible by postulating an Arctic Ice Sheet that behaved as a single dynamic system.

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Affiliations

  1. Department of Geological Sciences and Institute for Quaternary Studies, University of Maine, Orono, Maine, 04473

    • T. Hughes
    •  & G. H. Denton
  2. Institute of Geography, Academy of Sciences, 29 Staromonetny Street, Moscow, 109017, USSR

    • M. G. Grosswald

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https://doi.org/10.1038/266596a0

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