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Record #86041:
Sediment deformation beneath glaciers: rheology and geological consequences / Geoffrey S. Boulton, Richard C.A. Hindmarsh.
Title: | Sediment deformation beneath glaciers: rheology and geological consequences / Geoffrey S. Boulton, Richard C.A. Hindmarsh. |
Author(s): | Boulton, Geoffrey S. Hindmarsh, Richard C. A. |
Date: | 1987. |
In: | Journal of Geophysical Research. (1987.), Vol. 92(B9) (1987) |
Abstract: | Paper presented at Chapman Conference on Fast Glacier Flow: Ice Streams, Surging, and Tidewater Glaciers, held at Whistler Village, BC, Canada, 4-8 May 1986. Water pressures in till are less than ice pressures and it is suggested that this may lead to infiltration of ice into sediment, which inhibits sliding at interface. Where water pressures are equal or near to ice pressures this does not occur and sliding of glacier may result. Examines these processes in attempt to develop flow laws for subglacial till. |
Notes: | Journal of Geophysical Research. Vol. 92(B9) :9059-9082 (1987). |
Keywords: | 551.332.212 -- Till or boulder clay. 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.51 -- Land ice, theory of flow. 551.324.86 -- Glacier streams. 556 -- Hydrology. E5 -- Glaciology: land ice. |
SPRI record no.: | 86041 |
LDR 01482naa#a2200000#a#4500 001 SPRI-86041 005 20240329113317.0 007 ta 008 240329s1987####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-86041 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aBoulton, Geoffrey S. 245 10 ‡aSediment deformation beneath glaciers :‡brheology and geological consequences /‡cGeoffrey S. Boulton, Richard C.A. Hindmarsh. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1987. 300 ## ‡ap. 9059-9082 :‡bdiags., map. 500 ## ‡aJournal of Geophysical Research. Vol. 92(B9) :9059-9082 (1987). 520 3# ‡aPaper presented at Chapman Conference on Fast Glacier Flow: Ice Streams, Surging, and Tidewater Glaciers, held at Whistler Village, BC, Canada, 4-8 May 1986. Water pressures in till are less than ice pressures and it is suggested that this may lead to infiltration of ice into sediment, which inhibits sliding at interface. Where water pressures are equal or near to ice pressures this does not occur and sliding of glacier may result. Examines these processes in attempt to develop flow laws for subglacial till. 650 07 ‡a551.332.212 -- Till or boulder clay.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.51 -- Land ice, theory of flow.‡2udc 650 07 ‡a551.324.86 -- Glacier streams.‡2udc 650 07 ‡a556 -- Hydrology.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 700 1# ‡aHindmarsh, Richard C. A. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 92(B9) (1987) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329