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Record #195010:

Glacier ice structures influence on moraines development (Hørbye Glacier, Spitsbergen) / Izabela Szuman, Leszek Kasprzak.

Title: Glacier ice structures influence on moraines development (Hørbye Glacier, Spitsbergen) / Izabela Szuman, Leszek Kasprzak.
Author(s): Szuman, Izabela.
Kasprzak, Leszek.
Date: 2010.
In: Quaestiones Geographicae. (2010.), Vol. 29(1) (2010)
Abstract: Examines landforms controlled by ice fractures that generate patterned sedimentation in marginal zone of glacier, testing hypothesis that moraine formation is controlled by ice structure, and determining significance of landform assemblage in development of sedimentary basins. Divides study area into: clean ice surface, debris-covered ice fractures, and moraine complex. Describes geomorphology and basic sedimentology of ice surface and moraine complex, revealing moraine chains related to transverse fractures and longitudinal foliation in glacier and taking respective forms of thrust and medial moraines. Observes greater effectiveness of thrust and shear planes at creating forms on ice surface and in moraine complex. These form contain finer, more rounded material than less distinct longitudinal ones.
Notes:

Quaestiones Geographicae. Vol. 29(1) :65-73 (2010).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.22 -- Glaciers: Hørbye.
551.324.54 -- Land ice, flow of particular glaciers.
551.324.8 -- Land ice, structure and surface features.
551.324.85 -- Crevasses.
551.33 -- Glacial geology.
551.332.5 -- Glacial landforms.
551.332.52 -- Moraines, terminal and recessional.
551.324.81 -- Glacier bands, lamination, layering and foliation.
E5 -- Glaciology: land ice.
(*32) -- Svalbard.
(*324) -- Spitsbergen.
SPRI record no.: 195010

MARCXML

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035 ## ‡aSPRI-195010
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100 1# ‡aSzuman, Izabela.
245 10 ‡aGlacier ice structures influence on moraines development (Hørbye Glacier, Spitsbergen) /‡cIzabela Szuman, Leszek Kasprzak.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2010.
300 ## ‡ap. 65-73 :‡bill., diags., maps.
500 ## ‡aQuaestiones Geographicae. Vol. 29(1) :65-73 (2010).
520 3# ‡aExamines landforms controlled by ice fractures that generate patterned sedimentation in marginal zone of glacier, testing hypothesis that moraine formation is controlled by ice structure, and determining significance of landform assemblage in development of sedimentary basins. Divides study area into: clean ice surface, debris-covered ice fractures, and moraine complex. Describes geomorphology and basic sedimentology of ice surface and moraine complex, revealing moraine chains related to transverse fractures and longitudinal foliation in glacier and taking respective forms of thrust and medial moraines. Observes greater effectiveness of thrust and shear planes at creating forms on ice surface and in moraine complex. These form contain finer, more rounded material than less distinct longitudinal ones.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers: Hørbye.‡2udc
650 07 ‡a551.324.54 -- Land ice, flow of particular glaciers.‡2udc
650 07 ‡a551.324.8 -- Land ice, structure and surface features.‡2udc
650 07 ‡a551.324.85 -- Crevasses.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.332.52 -- Moraines, terminal and recessional.‡2udc
650 07 ‡a551.324.81 -- Glacier bands, lamination, layering and foliation.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*32) -- Svalbard.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
700 1# ‡aKasprzak, Leszek.
773 0# ‡7nnas ‡tQuaestiones Geographicae. ‡gVol. 29(1) (2010) ‡wSPRI-52254
916 ## ‡a2011/03/28 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221006 ‡bRF