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Original Articles

Characteristics of Cryogenic Weathering in the Permafrost Zone of the European UssrFootnote*

Pages 261-265 | Published online: 02 Jun 2018

References Cited

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  • Konishchev, V. N., 1962: Some specific features of loams in the southeastern part of the Bolshezemelskaya tundra due to their genesis. In: Voprosy geograficheskogo merzlotovedeniya i periglatsialnoy morfologii [Problems of geographical cryology and periglacial morphology]. Moscow. (In Russian.)
  • Konishchev, V. N., 1977: Some general regularities in the transformation of the composition of dispersed rocks by cryogenic processes. In: Problemy kriolitologii [Problems of Cryolithology], Vol. VI. Moscow University Press. (In Russian.)
  • Konishchev, V. N., 1978: Some general features of the composition of the dispersed rocks in the zone of cryolithogenesis. Vestnik Moskovskogo Universiteta, Geografiya, 5: 11–18. (In Russian.)
  • Konishchev, V. N., Rogov, V. V., and Shchurina, G. N., 1976: The influence of cryogenic factors on primary minerals (results of experimental studies). In: Problemy kriolitologii [Problems of Cryolithology], Vol. V. Moscow University Press. (In Russian.)
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  • Mazurov, G. P. and Tikhonova, E. S., 1964: Transformation of the composition and properties of grounds with repeated freezing. Vestnik Leningradskogo Universiteta, Geologiya, Geografiya, No. 18, Vol. III (In Russian.)
  • Poltev, N. F., 1966: Changes in the granulometric composition of sand grains when treated with electrolytic solutions and subjected to freeze-thaw processes. In: Merzlotnye issledovaniya [Cryogenic investigations], Vol. VI. Moscow. (In Russian.)
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  • Washburn, A. L., 1980: Geocryology: A Survey of Periglacial Processes and Environments. New York: Wiley. 406 pp.

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