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Record #165807:
Submarine mass-wasting on glacially-influenced continental slopes: processes and dynamics / Anders Elverhøi, and 8 others.
Title: | Submarine mass-wasting on glacially-influenced continental slopes: processes and dynamics / Anders Elverhøi, and 8 others. |
Author(s): | Elverhøi, Anders. |
Date: | 2002. |
Publisher: | London: Geological Society |
In: | Glacier-influenced sedimentation on high-latitude continental margins. (2002.), |
Abstract: | Examines recent progress in modelling muddy submarine debris flows typical of high-latitude continental margins. Compares selected submarine slides and debris flows and subaerial slides. Focuses on control exerted by material rheological properties on long runout distances observed on high-latitude margin flows. Divides process into sediment release phase, break up, flow and deposition. Discusses flow dynamics and simulations. Presents results of model using Bingham rheology with and without hydroplaning. Attributes long runouts to partial hydroplaning. Believes this may explain sharply lower friction coefficient for submarine mass flows whose released volume exceeds 1km³. |
Notes: | In: Glacier-influenced sedimentation on high-latitude continental margins / J.A. Dowdeswell, Colm Ó Cofaigh, eds. |
Keywords: | 551.33 -- Glacial geology. 551.311.8 -- Mud volcanoes and mudstreams. 551.332.25 -- Glacio-marine deposits. 551.35 -- Marine sediments. 551.351 -- Coastal deposits. 551.4 -- Geomorphology. 551.435.627 -- Landslides. 551.462.33 -- Continental slopes. 519.673 -- Modelling. .000(410) -- British author. E7 -- Glaciology: glacial geology and ice ages. (*3) -- Arctic regions. |
SPRI record no.: | 165807 |
LDR 02029naa#a2200000#a#4500 001 SPRI-165807 005 20231209160205.0 007 ta 008 231209s2002####enkab##|#####|0||#0#eng#d 035 ## ‡aSPRI-165807 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aElverhøi, Anders. 245 10 ‡aSubmarine mass-wasting on glacially-influenced continental slopes :‡bprocesses and dynamics /‡cAnders Elverhøi, and 8 others. 260 ## ‡aLondon :‡bGeological Society,‡c2002. 300 ## ‡ap. 73-87 :‡bill., diags., tables, maps. 500 ## ‡aIn: Glacier-influenced sedimentation on high-latitude continental margins / J.A. Dowdeswell, Colm Ó Cofaigh, eds. 520 3# ‡aExamines recent progress in modelling muddy submarine debris flows typical of high-latitude continental margins. Compares selected submarine slides and debris flows and subaerial slides. Focuses on control exerted by material rheological properties on long runout distances observed on high-latitude margin flows. Divides process into sediment release phase, break up, flow and deposition. Discusses flow dynamics and simulations. Presents results of model using Bingham rheology with and without hydroplaning. Attributes long runouts to partial hydroplaning. Believes this may explain sharply lower friction coefficient for submarine mass flows whose released volume exceeds 1km³. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.311.8 -- Mud volcanoes and mudstreams.‡2udc 650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc 650 07 ‡a551.35 -- Marine sediments.‡2udc 650 07 ‡a551.351 -- Coastal deposits.‡2udc 650 07 ‡a551.4 -- Geomorphology.‡2udc 650 07 ‡a551.435.627 -- Landslides.‡2udc 650 07 ‡a551.462.33 -- Continental slopes.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a.000(410) -- British author.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 773 0# ‡7nnam ‡aJ.A. Dowdeswell, Colm Ó Cofaigh, eds. ‡tGlacier-influenced sedimentation on high-latitude continental margins. ‡dLondon : Geological Society, 2002. ‡wSPRI-163743 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231209