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Record #126937:

Late Plenivistulian deglaciation and the expansion of the periglacial zone in NW Poland / Stefan Kozarski.

Title: Late Plenivistulian deglaciation and the expansion of the periglacial zone in NW Poland / Stefan Kozarski.
Author(s): Kozarski, Stefan.
Date: 1993.
Abstract: In this region, periglacial phenomena occur mostly in outwash plains, till plains and pradolina terraces, and occasionally in alluvial fans and inland dunes. Some contain evidence of former permafrost and can be used as palaeoenvironmental reconstructions of Late Pleistocene deglaciation. They include ice-wedge casts, fossil sand-wedge polygons, ice-vein network casts, and oriented icing depressions. Cryostratigraphic record testifies to presence of continuous permafrost, or vast patches of permafrost, in deglaciated area of north-west Poland during Late Plenivistulian and during cold spells of Late Vistulian.
Notes:

Offprint: Geologie en Mijnbouw. Vol. 72(2) :143-157.

Keywords: 551.336 -- Ice ages.
551.791 -- Pleistocene.
551.34 -- Geocryology. Frozen ground.
551.343 -- Periglacial processes. Thermokarst.
551.583.3 -- Climatic changes, Quaternary.
551.345.3 -- Permafrost, composition and structure. Ice wedges.
E8 -- Glaciology: frost action and permafrost.
(438) -- Poland.
Location(s): SCO: SPRI-SHF: 551.34
SPRI record no.: 126937

MARCXML

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035 ## ‡aSPRI-126937
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100 1# ‡aKozarski, Stefan.
245 10 ‡aLate Plenivistulian deglaciation and the expansion of the periglacial zone in NW Poland /‡cStefan Kozarski.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 143-157 :‡bill., diag., tables, maps.
500 ## ‡aOffprint: Geologie en Mijnbouw. Vol. 72(2) :143-157.
520 3# ‡aIn this region, periglacial phenomena occur mostly in outwash plains, till plains and pradolina terraces, and occasionally in alluvial fans and inland dunes. Some contain evidence of former permafrost and can be used as palaeoenvironmental reconstructions of Late Pleistocene deglaciation. They include ice-wedge casts, fossil sand-wedge polygons, ice-vein network casts, and oriented icing depressions. Cryostratigraphic record testifies to presence of continuous permafrost, or vast patches of permafrost, in deglaciated area of north-west Poland during Late Plenivistulian and during cold spells of Late Vistulian.
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡a551.34 -- Geocryology. Frozen ground.‡2udc
650 07 ‡a551.343 -- Periglacial processes. Thermokarst.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.345.3 -- Permafrost, composition and structure. Ice wedges.‡2udc
650 07 ‡aE8 -- Glaciology: frost action and permafrost.‡2local
651 #7 ‡a(438) -- Poland.‡2udc
852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h551.34‡9Create 1 item record‡0Migrate
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221006