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Record #165746:

Configuration and timing of Ungava Bay ice stream, Labrador-Ungava, Canada / Krister N. Jansson, Arjen P. Stroeven, Johan Kleman.

Title: Configuration and timing of Ungava Bay ice stream, Labrador-Ungava, Canada / Krister N. Jansson, Arjen P. Stroeven, Johan Kleman.
Author(s): Jansson, Krister N.
Stroeven, Arjen P.
Kleman, Johan.
Date: 2003.
In: Boreas. (2003.), Vol. 32(1) (2003)
Abstract: Presents aerial photograph and satellite image interpretations of Ungava Bay landform swarm (UBLS). Detailed mapping of till lineations resolves palimpsest imprint of individual ice streams and cross-cutting relationships establish a relative chronology. Identifies strongly convergent ice flow into Ungava Bay with at least eight discrete stream-flow events. Concludes UBLS reflects most direct and probably fastest contact (in terms of sediment transport) between Laurentide Ice Sheet interior and ocean. Discusses whether UBLS and its individual components are dynamically and temporally compatible with Gold Cove and Noble Inlet advances. In special issue Palaeo-ice streams.
Notes:

Boreas. Vol. 32(1) :256-262 (2003).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.29 -- Land ice, miscellaneous forms: Ungava Bay ice stream.
551.336 -- Ice ages: Laurentide Ice Sheet.
551.33 -- Glacial geology.
551.332 -- Glacial deposition.
551.332.5 -- Glacial landforms.
551.332.25 -- Glacio-marine deposits.
E7 -- Glaciology: glacial geology and ice ages.
(7) -- North America.
(*41) -- Canada.
(*422) -- Labrador - Ungava.
SPRI record no.: 165746

MARCXML

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035 ## ‡aSPRI-165746
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100 1# ‡aJansson, Krister N.
245 10 ‡aConfiguration and timing of Ungava Bay ice stream, Labrador-Ungava, Canada /‡cKrister N. Jansson, Arjen P. Stroeven, Johan Kleman.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 256-262 :‡bill., maps.
500 ## ‡aBoreas. Vol. 32(1) :256-262 (2003).
520 3# ‡aPresents aerial photograph and satellite image interpretations of Ungava Bay landform swarm (UBLS). Detailed mapping of till lineations resolves palimpsest imprint of individual ice streams and cross-cutting relationships establish a relative chronology. Identifies strongly convergent ice flow into Ungava Bay with at least eight discrete stream-flow events. Concludes UBLS reflects most direct and probably fastest contact (in terms of sediment transport) between Laurentide Ice Sheet interior and ocean. Discusses whether UBLS and its individual components are dynamically and temporally compatible with Gold Cove and Noble Inlet advances. In special issue Palaeo-ice streams.
530 ## ‡aAlso issued online ‡uurn:doi:10.1080/03009480310001146‡uhttps://dx.doi.org/10.1080/03009480310001146
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.29 -- Land ice, miscellaneous forms: Ungava Bay ice stream.‡2udc
650 07 ‡a551.336 -- Ice ages: Laurentide Ice Sheet.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(7) -- North America.‡2udc
651 #7 ‡a(*41) -- Canada.‡2udc
651 #7 ‡a(*422) -- Labrador - Ungava.‡2udc
700 1# ‡aStroeven, Arjen P.
700 1# ‡aKleman, Johan.
773 0# ‡7nnas ‡tBoreas. ‡gVol. 32(1) (2003) ‡wSPRI-56035
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220925