Results 141 to 150 of about 491 (213)
Boreas, 1995 Terminal‐moraine ridges up to 6 m high have been forming at the snout of Styggedalsbreen for two decades. Based on intermittent observations during this period, combined with a detailed study of ridge morphology, sedimentary structures and composition during the 1993 field season, a model of terminal‐moraine formation that involves the interaction of ...
JOHN A. MATTHEWS +2 more
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The Terminal Moraine of the Puget Sound Glacier
The Journal of Geology, 1911 J. Harlen Bretz
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Rubble fragment counts and terminal moraines of Holstein, Germany
Zeitschrift der Deutschen Geologischen Gesellschaft, 1935 W. G. Simon
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A Probable Late Pinedale Terminal Moraine in Castle River Valley, Alberta: Discussion
Geological Society of America Bulletin, 1970 W. PHILIP WAGNER, DONALD F. ESCHMAN
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Terminal moraines of Belarus and Lithuania
Zeitschrift der Deutschen Geologischen Gesellschaft, 1902 Anna Missuna
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Terminal moraines and eskers of the Saale river (Riss glaciation) in Silesia
Zeitschrift der Deutschen Geologischen Gesellschaft, 1932 Paul Woldstedt
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Fluvioglacial sediment and the Osning terminal moraine at the Teutoburg forest
Zeitschrift der Deutschen Geologischen Gesellschaft, 1952 Gerhard Keller
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Terminal and recessional moraines in the fjords of southern Chile
Geological Society, London, Memoirs, 2016Moraine ridges marking the outermost limit of a glacier advance are known as terminal moraines; recessional moraines indicate stillstands or minor readvances during overall glacier retreat. At the Last Glacial Maximum, the Patagonian Ice Cap advanced to fill the complex fjord system of southern Chile. Since then, ice has retreated producing recessional
G. Lastras, J. A. Dowdeswell
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