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Record #165728:

Maximum limits of the Baltic Ice-Sheet during the Pomeranian Phase in the Drawskie Lakeland / Piotr Kłysz.

Title: Maximum limits of the Baltic Ice-Sheet during the Pomeranian Phase in the Drawskie Lakeland / Piotr Kłysz.
Author(s): Kłysz, Piotr.
Date: 2002[pub. 2003]
In: Quaestiones Geographicae. (2002[pub. 2003]), Vol. 22 (2002[pub. 2003])
Abstract: Discusses results of investigations in Drawskie Lakeland aimed at identifying limits of Baltic Ice Sheet during Pomeranian Phase. Describes petrographic features of Drawskie Lakeland moraine tills. Identifies two distinct (accumulation and push) end moraine sequences and discusses their structures and morphogenesis. Concludes that ice sheet reached further south in Pomeranian Phase than was proposed by Keilhack in 1901 and is still commonly accepted.
Notes:

Quaestiones Geographicae. Vol. 22 :29-42 (2002[pub. 2003]).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.336 -- Ice ages: Baltic Ice Sheet.
551.324.63 -- Land ice, advance and retreat.
551.33 -- Glacial geology.
551.332 -- Glacial deposition.
551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites.
551.332.5 -- Glacial landforms.
551.332.52 -- Moraines, terminal and recessional.
551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.
551.4 -- Geomorphology: push moraines.
551.791 -- Pleistocene: Pomeranian.
E7 -- Glaciology: glacial geology and ice ages.
(438) -- Poland.
SPRI record no.: 165728

MARCXML

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100 1# ‡aKłysz, Piotr.
245 10 ‡aMaximum limits of the Baltic Ice-Sheet during the Pomeranian Phase in the Drawskie Lakeland /‡cPiotr Kłysz.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2002[pub. 2003]
300 ## ‡ap. 29-42 :‡bills., diags., tables, maps.
500 ## ‡aQuaestiones Geographicae. Vol. 22 :29-42 (2002[pub. 2003]).
520 3# ‡aDiscusses results of investigations in Drawskie Lakeland aimed at identifying limits of Baltic Ice Sheet during Pomeranian Phase. Describes petrographic features of Drawskie Lakeland moraine tills. Identifies two distinct (accumulation and push) end moraine sequences and discusses their structures and morphogenesis. Concludes that ice sheet reached further south in Pomeranian Phase than was proposed by Keilhack in 1901 and is still commonly accepted.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.336 -- Ice ages: Baltic Ice Sheet.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡a551.332.21 -- Till or boulder clay. Tillite. Glacial diamictites.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.332.52 -- Moraines, terminal and recessional.‡2udc
650 07 ‡a551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.‡2udc
650 07 ‡a551.4 -- Geomorphology: push moraines.‡2udc
650 07 ‡a551.791 -- Pleistocene: Pomeranian.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(438) -- Poland.‡2udc
773 0# ‡7nnas ‡tQuaestiones Geographicae. ‡gVol. 22 (2002[pub. 2003]) ‡wSPRI-52254
917 ## ‡aUnenhanced record from Muscat, imported 2019
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