Climatic Implications of Alternating Clay and Carbonate Formation in Semiarid Soils of South-Central Montana

Evidence for climatic change is found in petrographic thin sections from soils formed on glaciofluvial deposits of Rock Creek and the lower Clarks Fork, Montana. These soils, presently in a semiarid climate, range from late Pliocene to Holocene in age, and have undergone periodic fluctuations in soi...

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Veröffentlicht in:Quaternary research 1987-05, Vol.27 (3), p.270-282
1. Verfasser: Reheis, Marith C.
Format: Artikel
Sprache:eng
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