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Record #172242:

Pleni- and Late Vistulian glacial lakes, their sediments and landforms: a case study from the young glacial landscape of northern Poland / Władysław Niewiarowski.

Title: Pleni- and Late Vistulian glacial lakes, their sediments and landforms: a case study from the young glacial landscape of northern Poland / Władysław Niewiarowski.
Author(s): Niewiarowski, Władysław.
Date: 2004.
In: Prace Geograficzne. (2004.), Vol. 189 (2004)
Abstract: Examines glacial lakes and sediments and landforms they left behind in northern Poland. Seeks genetic and spatial linkage between lakes, different types of ice-sheet ice and their meltwaters, and geological and geomorphological traces of lake existence. Reviews available evidence for Pleni- and Late Vistulian lakes and associated deposits and landforms. Concludes northern Poland saw numerous glacial lakes. Some, originating in Pleni-Vistulian in zone of stagnant and dead ice, were fed by melt waters of active ice. Others, younger, rarer, small and short lived, were ice-dammed lakes arising from damming of outflow of dead ice and fed by its melting.
Notes:

Prace Geograficzne. Vol. 189 :61-85 (2004).

Polish abstract.

Keywords: 551.33 -- Glacial geology.
551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.
551.324 -- Land ice.
551.332.5 -- Glacial landforms.
551.332.26 -- Glacio-lacustrine deposits and varves.
551.791 -- Pleistocene: Vistulian.
551.336 -- Ice ages.
551.324.86 -- Glacier streams.
556 -- Hydrology.
E7 -- Glaciology: glacial geology and ice ages.
(438) -- Poland.
SPRI record no.: 172242

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500 ## ‡aPolish abstract.
520 3# ‡aExamines glacial lakes and sediments and landforms they left behind in northern Poland. Seeks genetic and spatial linkage between lakes, different types of ice-sheet ice and their meltwaters, and geological and geomorphological traces of lake existence. Reviews available evidence for Pleni- and Late Vistulian lakes and associated deposits and landforms. Concludes northern Poland saw numerous glacial lakes. Some, originating in Pleni-Vistulian in zone of stagnant and dead ice, were fed by melt waters of active ice. Others, younger, rarer, small and short lived, were ice-dammed lakes arising from damming of outflow of dead ice and fed by its melting.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.332.26 -- Glacio-lacustrine deposits and varves.‡2udc
650 07 ‡a551.791 -- Pleistocene: Vistulian.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.324.86 -- Glacier streams.‡2udc
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(438) -- Poland.‡2udc
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