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Alan will continue in his role as chair of Mersey Maritime’s popular Export Club but is succeeded as MD at Conductix by former operations manager Neil Smith.
PARASOUND (3.5 k Hz) subbottom echosounder profiles acquired on the southern Spitsbergenbanken, NW Barents Sea, show iceberg-keel scouring features which are buried by sediment that accumulated during the post Last Glacial Maximum (LGM) sea-level rise.
The first slide event occurred during MIS 3 around 30 cal.
ka BP and was characterised by highly dynamic and rapid evacuation of ca.
1250 km material from hemi-pelagic sediments and from the lower pre-existing trough mouth fan has been entrained and transported into the semi-enclosed Sophia Basin.
This megaslide event was followed by a secondary evacuation of material to the Nansen Basin by funnelling of the debris through the channel between Polarstern Seamount and the adjacent continental slope.
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Discharge of the Hinlopen ice stream during the Last Glacial Maximum and the following deglaciation draped the central headwalls and created a fan deposit of glacigenic debris flows.
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