Author:
Sorenson Curtis J.,Knox James C.,Larsen James A.,Bryson Reid A.
Abstract
The morphology of paleosols and radiocarbon-dated charcoal from buried surface horizons of soils provide evidence to suggest that between periods of northward forest encroachment tundra climate has dominated areas at least 50 km south of the present forest/tundra border in southwest Keewatin. The present forest/tundra border climate is nearly as severe as any climate that has prevailed in the area since deglaciation.
Publisher
Cambridge University Press (CUP)
Subject
General Earth and Planetary Sciences,Earth-Surface Processes,Arts and Humanities (miscellaneous)
Reference8 articles.
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5. Tentative climatic patterns for some late glacial and postglacial episodes in central North America. In “Life, Land, and Water.”;Bryson,1967
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