Periglacial geomorphology: what, where, when? / Colin E. Thorn.

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100 1# ‡aThorn, Colin E.
245 10 ‡aPeriglacial geomorphology :‡bwhat, where, when? /‡cColin E. Thorn.
260 ## ‡aChichester :‡bJohn Wiley & Sons,‡c1992.
300 ## ‡ap. 1-30.
500 ## ‡aIn: Periglacial geomorphology. Proceedings of the 22nd Annual Binghamton Symposium in Geomorphology / John C. Dixon, Athol D. Abrahams, eds.
520 3# ‡aPurpose was to construct skeleton of periglacial geomorphology based strictly on theoretically and/or empirically derived field-verified processes. Conclusion reached is that periglacial geomorphology has, at its primary object, physically based explanations of past, present and future impacts of diurnal, seasonal and perennial ground ice on landform and landscape initiation and development. Additional components include similar investigations of geomorphic roles of snowpacks (but not glaciers) and fluvial, lacustrine and marine ice. Advantages over previous definitions are discussed.
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc
650 07 ‡a001.4 -- Nomenclature and terminology.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
773 0# ‡7nnam ‡aJohn C. Dixon, Athol D. Abrahams, eds. ‡tPeriglacial geomorphology. Proceedings of the 22nd Annual Binghamton Symposium in Geomorphology. ‡dChichester : John Wiley & Sons, 1992. ‡wSPRI-117218
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230928