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Record #182789:

Quaternary glaciation history and glaciology of Jakobshavn Isbrae and the Disko Bugt region, West Greenland: a review / Anker Weidick, Ole Bennike.

Title: Quaternary glaciation history and glaciology of Jakobshavn Isbrae and the Disko Bugt region, West Greenland: a review / Anker Weidick, Ole Bennike.
Author(s): Weidick, Anker.
Bennike, Ole.
Date: 2007.
In: Geological Survey of Denmark and Greenland Bulletin. (2007.), Vol. 14 (2007)
Abstract: Describes glaciation history of Disko Bugt, region characterised by permanent ice streams. Notes cooling during Cenozoic leading to ice-sheet growth in Greenland, rapid deglaciation of Disko Bugt in early Holocene (10.5-10.0 ka B.P.) and formation of moraine systems, subsequent Neoglacial readvance reaching maximum in Little Ice Age (1850 AD), and recession continuing to present day. Describes Jakobshavn Isbrae, main outlet from Greenland ice sheet, draining 6.5% of present inland ice, and producing c. 35-50 km³ of icebergs per year, correspondcing to more than 10% of total iceberg output from inland ice.
Notes:

Geological Survey of Denmark and Greenland Bulletin. Vol. 14 :1-78 (2007).

Keywords: 551.1/.4 -- Geology.
551.32 -- Glaciology.
551.324.24 -- Ice sheets and caps.
551.33 -- Glacial geology.
551.332.5 -- Glacial landforms.
551.336 -- Ice ages.
551.77 -- Cenozoic.
556 -- Hydrology.
E7 -- Glaciology: glacial geology and ice ages.
(*3) -- Arctic regions.
(*38) -- Greenland.
(*384) -- West Greenland.
(*384.28) -- Qeqertarsuaq/Godhavn.
SPRI record no.: 182789

MARCXML

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035 ## ‡aSPRI-182789
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100 1# ‡aWeidick, Anker.
245 10 ‡aQuaternary glaciation history and glaciology of Jakobshavn Isbrae and the Disko Bugt region, West Greenland :‡ba review /‡cAnker Weidick, Ole Bennike.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2007.
300 ## ‡ap. 1-78 :‡bill., diags., tables, maps.
500 ## ‡aGeological Survey of Denmark and Greenland Bulletin. Vol. 14 :1-78 (2007).
520 3# ‡aDescribes glaciation history of Disko Bugt, region characterised by permanent ice streams. Notes cooling during Cenozoic leading to ice-sheet growth in Greenland, rapid deglaciation of Disko Bugt in early Holocene (10.5-10.0 ka B.P.) and formation of moraine systems, subsequent Neoglacial readvance reaching maximum in Little Ice Age (1850 AD), and recession continuing to present day. Describes Jakobshavn Isbrae, main outlet from Greenland ice sheet, draining 6.5% of present inland ice, and producing c. 35-50 km³ of icebergs per year, correspondcing to more than 10% of total iceberg output from inland ice.
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.336 -- Ice ages.‡2udc
650 07 ‡a551.77 -- Cenozoic.‡2udc
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
651 #7 ‡a(*384) -- West Greenland.‡2udc
651 #7 ‡a(*384.28) -- Qeqertarsuaq/Godhavn.‡2udc
700 1# ‡aBennike, Ole.
773 0# ‡7nnas ‡tGeological Survey of Denmark and Greenland Bulletin. ‡gVol. 14 (2007) ‡wSPRI-168675
916 ## ‡a2008/05/15 -- RF
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328 ‡bRF