02649nas a2200277   4500000000100000000000100001008004100002653002500043653002000068653001800088653001100106100001400117700001400131700001500145700001300160700001600173700001500189700001400204700001700218245010100235856007100336300001000407490000800417520193200425020001402357       2002                            d10aglacigenic sediments10aLate Quaternary10aNorwegian Sea10aslides1 aJ. Laberg1 aT. Vorren1 aJ. Mienert1 aD. Evans1 aB. Lindberg1 aD. Ottesen1 aNH Kenyon1 aS. Henriksen00aLate Quaternary palaeoenvironment and chronology in the Tr\aenadjupet Slide area offshore Norway  uhttp://www.sciencedirect.com/science/article/pii/S0025322702002748  a35-600 v1883 aThe northern mid-Norwegian continental slope was studied based on high-resolution side-scan sonar data, multibeam bathymetry, high-resolution and multichannel seismics together with gravity cores. Sedimentary provinces identified include a partly buried slide on the eastern, inner V\oring Plateau, an area dominated by glacigenic debris flows south-west of the Tr\aenadjupet Slide, the Tr\aenadjupet Slide, and an area of glacimarine sedimentation and a slide scar north-east of the Tr\aenadjupet Slide. The Tr\aenadjupet Slide affected an area of about 14 100 km2 and mobilised about 900 km3 of sediments. Little is known about the areal extent and volume of the older events. The glacigenic debris flows and glacimarine sediments were deposited while the Fennoscandian ice sheet was at the shelf break during the late Weichselian glacial maximum (prior to 13.2 14C kyr BP). Hemipelagic and/or contouritic sedimentation prevailed during the Holocene period. Two large slide scars were probably formed sometime prior to or during the late Weichselian glacial maximum (inner V\oring Plateau and north-east of the Tr\aenadjupet Slide) and another during the mid-Holocene interglacial period immediately prior to 4000 14C kyr BP (the Tr\aenadjupet Slide). The two older scars may represent one event or two separate events. Deposition of poorly permeable glacigenic sediments over high-water-content fine-grained hemipelagic and/or contourites may have prevented water escape and increased failure potential. Thus continental slope areas of episodically high sediment input of glacigenic sediments are prone to failure as illustrated by this study, which has identified at least two large slope failures. Failures have occurred both during glacial maxima, periods of climate deterioration and low global eustatic sea level, and during interglacials as today with improved climatic conditions and a high global eustatic sea level.  a0025-3227