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Record #165727:

The origin and age of "huge alluvial fans" in the eastern part of the Warsaw-Berlin Pradolina / Zbigniew Klajnert, Elzbieta Kobojek.

Title: The origin and age of "huge alluvial fans" in the eastern part of the Warsaw-Berlin Pradolina / Zbigniew Klajnert, Elzbieta Kobojek.
Author(s): Klajnert, Zbigniew.
Kobojek, Elzbieta.
Date: 2002[pub. 2003]
In: Quaestiones Geographicae. (2002[pub. 2003]), Vol. 22 (2002[pub. 2003])
Abstract: Discusses development of relief and geology of extensive area referred to in literature as "a zone of alluvial fans", stretching below northern edges of Rawa Interfluve and Łódź Upland. Notes disagreement regarding fan zone's age. Discusses impact of areal deglaciation of Warthe stage ice sheet on fan zone formation, Eemian deposits and Vistulian, periglacial elements within zone. Concludes zone is polygenetic surface initiated during decay of Warthe stage ice sheet but finds no evidence of widespread and intense periglacial denudation which could have been responsible for zone's development.
Notes:

Quaestiones Geographicae. Vol. 22 :17-28 (2002[pub. 2003]).

Keywords: 551.33 -- Glacial geology.
551.332 -- Glacial deposition.
551.3.051 -- Sedimentation and stratification.
551.332.24 -- Glacio-fluvial deposits.
551.791 -- Pleistocene: Eemian, Warthe, Vistulian.
E7 -- Glaciology: glacial geology and ice ages.
(438) -- Poland.
SPRI record no.: 165727

MARCXML

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100 1# ‡aKlajnert, Zbigniew.
245 14 ‡aThe origin and age of "huge alluvial fans" in the eastern part of the Warsaw-Berlin Pradolina /‡cZbigniew Klajnert, Elzbieta Kobojek.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2002[pub. 2003]
300 ## ‡ap. 17-28 :‡bills., diags., maps.
500 ## ‡aQuaestiones Geographicae. Vol. 22 :17-28 (2002[pub. 2003]).
520 3# ‡aDiscusses development of relief and geology of extensive area referred to in literature as "a zone of alluvial fans", stretching below northern edges of Rawa Interfluve and Łódź Upland. Notes disagreement regarding fan zone's age. Discusses impact of areal deglaciation of Warthe stage ice sheet on fan zone formation, Eemian deposits and Vistulian, periglacial elements within zone. Concludes zone is polygenetic surface initiated during decay of Warthe stage ice sheet but finds no evidence of widespread and intense periglacial denudation which could have been responsible for zone's development.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.332.24 -- Glacio-fluvial deposits.‡2udc
650 07 ‡a551.791 -- Pleistocene: Eemian, Warthe, Vistulian.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(438) -- Poland.‡2udc
700 1# ‡aKobojek, Elzbieta.
773 0# ‡7nnas ‡tQuaestiones Geographicae. ‡gVol. 22 (2002[pub. 2003]) ‡wSPRI-52254
917 ## ‡aUnenhanced record from Muscat, imported 2019
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