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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

MARCXML

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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# ‡a20221006