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Record #152264:
- #152264
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MARC recordIce composition evidence for the formation of basal ice from lake water beneath a cold-based Antarctic glacier / R.D. (Reginald D.) Lorrain, S.J. Fitzsimons, M.J. Vandergoes, M. Stiévenard.
| Title: | Ice composition evidence for the formation of basal ice from lake water beneath a cold-based Antarctic glacier / R.D. (Reginald D.) Lorrain, S.J. Fitzsimons, M.J. Vandergoes, M. Stiévenard. |
| Author(s): | Lorrain, R. D. Fitzsimons, S. J. Vandergoes, M. J. Stiévenard, M. |
| Date: | 1999. |
| In: | Annals of Glaciology. (1999.), Vol. 28 (1999) |
| Abstract: | Describes model where transient wet-base conditions can occur as ice flows onto unfrozen sediments at lake bottom, creating conditions favorable to entrainment of sediments and ice accretion by water freezing. Stable isotope composition of ice at base of Suess Glacier, Taylor Valley, indicates that water freezing, probably lake water, is important in formation of basal ice layers. |
| Notes: | Annals of Glaciology. Vol. 28 :277-281 (1999). Papers from the International Symposium on Glaciers and the Glaciated Landscape, 17--20 August 1998, Kiruna, Sweden, J. Kleman (Editor) |
| Keywords: | 551.33 -- Glacial geology. 551.32 -- Glaciology. 551.324.22 -- Glaciers: Suess Glacier. 551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage. 54.027 -- Isotope analysis. 519.673 -- Modelling. E11 -- Glaciology: glaciohydrology. (*7) -- Antarctic regions. (*762.4) -- Scott Coast. |
| SPRI record no.: | 152264 |
LDR 01728naa#a2200000#a#4500 001 SPRI-152264 005 20231004183654.0 007 ta 008 231004s1999####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-152264 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aIce composition evidence for the formation of basal ice from lake water beneath a cold-based Antarctic glacier /‡cR.D. (Reginald D.) Lorrain, S.J. Fitzsimons, M.J. Vandergoes, M. Stiévenard. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1999. 300 ## ‡ap. 277-281 :‡bill., diags., table. 500 ## ‡aAnnals of Glaciology. Vol. 28 :277-281 (1999). 500 ## ‡aPapers from the International Symposium on Glaciers and the Glaciated Landscape, 17--20 August 1998, Kiruna, Sweden, J. Kleman (Editor) 520 3# ‡aDescribes model where transient wet-base conditions can occur as ice flows onto unfrozen sediments at lake bottom, creating conditions favorable to entrainment of sediments and ice accretion by water freezing. Stable isotope composition of ice at base of Suess Glacier, Taylor Valley, indicates that water freezing, probably lake water, is important in formation of basal ice layers. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324.22 -- Glaciers: Suess Glacier.‡2udc 650 07 ‡a551.332.56 -- Lakes, ice-dammed. Glacial lakes. Disruption of water drainage.‡2udc 650 07 ‡a54.027 -- Isotope analysis.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*762.4) -- Scott Coast.‡2udc 700 1# ‡aLorrain, R. D. ‡q(Reginald D. ) 700 1# ‡aFitzsimons, S. J. 700 1# ‡aVandergoes, M. J. 700 1# ‡aStiévenard, M. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 28 (1999) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231004