Abstract
Three temperature profiles at Asbestos Hill yield low geothermal gradients. Extrapolating temperature profiles to greater depths gives a permafrost thickness of at least 540m. A simple model of surface temperature history for the area for the past 85 000 years is developed. -from Authors
Cite
CITATION STYLE
APA
Taylor, A., & Judge, A. (1979). Permafrost studies in northern Quebec. Geographie Physique et Quaternaire, 33(3–4), 245–251. https://doi.org/10.7202/1000361ar
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