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Record #126507:

Glacial and marine episodes in Kaffiöyra, northwestern Spitsbergen, during the Vistulian and the Holocene / Władysław Niewiarowski, F. Pazdur Mieczysław, Sinkiewicz Mieczysław.

Title: Glacial and marine episodes in Kaffiöyra, northwestern Spitsbergen, during the Vistulian and the Holocene / Władysław Niewiarowski, F. Pazdur Mieczysław, Sinkiewicz Mieczysław.
Author(s): Niewiarowski, Władysław.
Mieczysław, F. Pazdur.
Mieczysław, Sinkiewicz.
Date: 1993.
In: Polish Polar Research. (1993.), Vol. 14(3) (1993)
Abstract: New geological and geomorphological data suggest that Kaffiöyra and Hermansenöya were glaciated completely during Early Vistulian, about 70±10 ka BP. Glacioisostatic subsidence associated with this glaciation was conducive to marine transgression up to 65 m a.s.l. Following emergence resulted in raised marine beaches. After this, there was long ice-free period; no evidence of Middle Vistulian glaciation has been found. There are well-preserved traces of Late Vistulian glaciation, though ice probably occupied smaller area than during Early Vistulian. Few traces of Holocene are found, but clear landforms and deposits associated with glacier advances during Little Ice Age are visible.
Notes:

Polish Polar Research. Vol. 14(3) :243-258, [1] unnumbered leaf (1993).

Keywords: 551.33 -- Glacial geology.
551.336 -- Ice ages.
551.791 -- Pleistocene.
551.794 -- Holocene.
551.334 -- Glacial isostasy, eustasy and other effects of ice cover.
E7 -- Glaciology: glacial geology and ice ages.
(*32) -- Svalbard.
(*324) -- Spitsbergen.
SPRI record no.: 126507

MARCXML

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100 1# ‡aNiewiarowski, Władysław.
245 10 ‡aGlacial and marine episodes in Kaffiöyra, northwestern Spitsbergen, during the Vistulian and the Holocene /‡cWładysław Niewiarowski, F. Pazdur Mieczysław, Sinkiewicz Mieczysław.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 243-258, [1] unnumbered leaf :‡bill., diags., table, map (following p. 256)
500 ## ‡aPolish Polar Research. Vol. 14(3) :243-258, [1] unnumbered leaf (1993).
520 3# ‡aNew geological and geomorphological data suggest that Kaffiöyra and Hermansenöya were glaciated completely during Early Vistulian, about 70±10 ka BP. Glacioisostatic subsidence associated with this glaciation was conducive to marine transgression up to 65 m a.s.l. Following emergence resulted in raised marine beaches. After this, there was long ice-free period; no evidence of Middle Vistulian glaciation has been found. There are well-preserved traces of Late Vistulian glaciation, though ice probably occupied smaller area than during Early Vistulian. Few traces of Holocene are found, but clear landforms and deposits associated with glacier advances during Little Ice Age are visible.
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.791 -- Pleistocene.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡a551.334 -- Glacial isostasy, eustasy and other effects of ice cover.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*32) -- Svalbard.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
700 1# ‡aMieczysław, F. Pazdur.
700 1# ‡aMieczysław, Sinkiewicz.
773 0# ‡7nnas ‡tPolish Polar Research. ‡gVol. 14(3) (1993) ‡wSPRI-60789
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220928