Drumlins as part of a glacier bedform continuum / J. Rose.

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100 1# ‡aRose, J.
245 10 ‡aDrumlins as part of a glacier bedform continuum /‡cJ. Rose.
260 ## ‡aRotterdam :‡bA.A. Balkema,‡c1987.
300 ## ‡ap. 103-116 :‡bdiags., tables, maps.
500 ## ‡aIn: Drumlin symposium. Proceedings of the Drumlin Symposium/First International Conference on Geomorphology/Manchester/16-18 September 1985 / John Menzies, J. Rose, eds.
520 3# ‡aPresents case that drumlins are bedforms produced by moving ice at glacier/bed interface, and are considered analogous with bedforms produced by other geomorphological processes such as moving water or wind. Suggests they are part of landform continuum that is developed in response to glacier ice moving across deformable or erodable bed materials with range of stress levels determined by ice thickness and rate of ice movement, interacting with range of bed materials.
650 07 ‡a551.332.54 -- Drumlins.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
773 0# ‡7nnam ‡aJohn Menzies, J. Rose, eds. ‡tDrumlin symposium. Proceedings of the Drumlin Symposium/First International Conference on Geomorphology/Manchester/16-18 September 1985. ‡dRotterdam : A.A. Balkema, 1987. ‡wSPRI-88314
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20230401