skip to primary navigation skip to content
 

 

You are not currently logged in

SPRI library catalogue

View a record

Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.

Please search for material in iDiscover for up-to-date information about the library collection.


Record #96632:

Surface strain-rates, Byrd Glacier, Antarctica (abstract) / John P. Scofield, Dean R. Lindstrom, Terence J. Hughes.

Title: Surface strain-rates, Byrd Glacier, Antarctica (abstract) / John P. Scofield, Dean R. Lindstrom, Terence J. Hughes.
Author(s): Scofield, John P.
Lindstrom, Dean R.
Hughes, Terence J.
Date: 1989.
Publisher: Cambridge: International Glaciological Society
In: Annals of Glaciology. (1989.), Vol. 12 (1989)
Abstract: Contour maps of surface strain-rate components were computed. Results suggest longitudinal extensive flow in region between 40 and 10 km above grounding zone, laminar flow in vicinity of grounding zone, and longitudinal compressive flow in region between 10 and 50 km below grounding zone where flow diverges and enters Ross Ice Shelf. Flow is influenced by bedrock topography.
Notes:

Annals of Glaciology. Vol. 12 :207 (1989).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.54 -- Land ice, flow of particular glaciers: Byrd Glacier.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*772) -- Byrd Land.
SPRI record no.: 96632

MARCXML

LDR 01306naa#a2200000#a#4500
001 SPRI-96632
005 20220924220226.0
007 ta
008 220924s1989####enk###|##|###|0||#0|eng#d
035 ## ‡aSPRI-96632
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aScofield, John P.
245 10 ‡aSurface strain-rates, Byrd Glacier, Antarctica (abstract) /‡cJohn P. Scofield, Dean R. Lindstrom, Terence J. Hughes.
260 ## ‡aCambridge :‡bInternational Glaciological Society,‡c1989.
300 ## ‡ap. 207.
500 ## ‡aAnnals of Glaciology. Vol. 12 :207 (1989).
520 3# ‡aContour maps of surface strain-rate components were computed. Results suggest longitudinal extensive flow in region between 40 and 10 km above grounding zone, laminar flow in vicinity of grounding zone, and longitudinal compressive flow in region between 10 and 50 km below grounding zone where flow diverges and enters Ross Ice Shelf. Flow is influenced by bedrock topography.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.54 -- Land ice, flow of particular glaciers: Byrd Glacier.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*772) -- Byrd Land.‡2udc
700 1# ‡aLindstrom, Dean R.
700 1# ‡aHughes, Terence J.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 12 (1989) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220924