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• W2023882904 endingPage "27" @default.
• W2023882904 startingPage "13" @default.
• W2023882904 abstract "The morphology and distribution of submarine landforms in Hinlopen Trough, Northern Svalbard margin, and the upper continental slope beyond, are investigated using swath-bathymetric data, together with side-scan sonar, acoustic profiler records and sediment cores. Sun-illuminated images reveal a number of landform assemblages on the sea floor of Hinlopen Trough and confirm that this depression was occupied by an ice stream during the Late Weichselian glaciation around 20 ka before present. The geomorphology of the inner-shelf is characterised by bedrock drumlins and ice-sculpted bedrock. There is a middle-shelf transition from a rock bed to an unconsolidated sedimentary bed that contains highly-attenuated drumlins and megaflutes formed within a dark grey, matrix-supported diamict, interpreted as subglacial till. Outer-shelf landforms are mainly iceberg ploughmarks. The geomorphological imprint identified from Hinlopen Trough is similar to that of many former ice streams; the trough is dominated by elongate landforms orientated parallel to the inferred flow direction and is lacking in transverse features indicative of inter-ice stream locations. A characteristic down-flow progression in landform elongation is also observed, suggesting an increase in ice velocity across the continental shelf. The lack of grounding-zone features imaged from swath-bathymetric data implies that deglaciation was probably rapid within the trough. A large depositional fan exists on the upper continental slope beyond the trough, characterised by debris flow deposits relating to the down-slope transport of glacigenic sediment. Order of magnitude calculations of the volume of glacigenic sediment on the continental slope indicate that the ice stream provided high rates of debris delivery of around 5–7.5 m/ka. This suggests that Hinlopen Trough ice stream represented a major route for the transfer of ice and debris to the Hinlopen Fan on the northern continental margin of Svalbard during the Late Weichselian glaciation." @default.
• W2023882904 created "2016-06-24" @default.
• W2023882904 creator A5000303897 @default.
• W2023882904 creator A5086825747 @default.
• W2023882904 creator A5090441551 @default.
• W2023882904 date "2011-06-01" @default.
• W2023882904 modified "2023-09-27" @default.
• W2023882904 title "Late Quaternary ice flow and sediment delivery through Hinlopen Trough, Northern Svalbard margin: Submarine landforms and depositional fan" @default.
• W2023882904 cites W1601435429 @default.
• W2023882904 cites W1669825118 @default.
• W2023882904 cites W1693679103 @default.
• W2023882904 cites W1768067276 @default.
• W2023882904 cites W1809829952 @default.
• W2023882904 cites W1968402863 @default.
• W2023882904 cites W1971016183 @default.
• W2023882904 cites W1971461775 @default.
• W2023882904 cites W1972227132 @default.
• W2023882904 cites W1972738781 @default.
• W2023882904 cites W1976370924 @default.
• W2023882904 cites W1978135243 @default.
• W2023882904 cites W1978646732 @default.
• W2023882904 cites W1980214180 @default.
• W2023882904 cites W1982443152 @default.
• W2023882904 cites W1982554080 @default.
• W2023882904 cites W1986434892 @default.
• W2023882904 cites W1987807191 @default.
• W2023882904 cites W1990265232 @default.
• W2023882904 cites W1996315917 @default.
• W2023882904 cites W1998877509 @default.
• W2023882904 cites W2000725665 @default.
• W2023882904 cites W2000780920 @default.
• W2023882904 cites W2006125956 @default.
• W2023882904 cites W2010244876 @default.
• W2023882904 cites W2019979254 @default.
• W2023882904 cites W2024985119 @default.
• W2023882904 cites W2026229249 @default.
• W2023882904 cites W2026375365 @default.
• W2023882904 cites W2026838234 @default.
• W2023882904 cites W2027110890 @default.
• W2023882904 cites W2027624641 @default.
• W2023882904 cites W2028796508 @default.
• W2023882904 cites W2028946394 @default.
• W2023882904 cites W2029486441 @default.
• W2023882904 cites W2030351607 @default.
• W2023882904 cites W2030460559 @default.
• W2023882904 cites W2030873098 @default.
• W2023882904 cites W2031485235 @default.
• W2023882904 cites W2032053405 @default.
• W2023882904 cites W2033024991 @default.
• W2023882904 cites W2034639312 @default.
• W2023882904 cites W2035301031 @default.
• W2023882904 cites W2036045847 @default.
• W2023882904 cites W2042786534 @default.
• W2023882904 cites W2043672520 @default.
• W2023882904 cites W2047535748 @default.
• W2023882904 cites W2047970690 @default.
• W2023882904 cites W2048152717 @default.
• W2023882904 cites W2048740472 @default.
• W2023882904 cites W2049647879 @default.
• W2023882904 cites W2050079504 @default.
• W2023882904 cites W2054292387 @default.
• W2023882904 cites W2054953518 @default.
• W2023882904 cites W2057602458 @default.
• W2023882904 cites W2066227436 @default.
• W2023882904 cites W2067923119 @default.
• W2023882904 cites W2069339378 @default.
• W2023882904 cites W2069580113 @default.
• W2023882904 cites W2072390800 @default.
• W2023882904 cites W2073231602 @default.
• W2023882904 cites W2078076761 @default.
• W2023882904 cites W2081353759 @default.
• W2023882904 cites W2081662319 @default.
• W2023882904 cites W2090149204 @default.
• W2023882904 cites W2090347375 @default.
• W2023882904 cites W2091645757 @default.
• W2023882904 cites W2091738388 @default.
• W2023882904 cites W2096215896 @default.
• W2023882904 cites W2097637856 @default.
• W2023882904 cites W2102002872 @default.
• W2023882904 cites W2105163876 @default.
• W2023882904 cites W2105220545 @default.
• W2023882904 cites W2111043296 @default.
• W2023882904 cites W2112594191 @default.
• W2023882904 cites W2113159671 @default.
• W2023882904 cites W2117376089 @default.
• W2023882904 cites W2120348339 @default.
• W2023882904 cites W2125283958 @default.
• W2023882904 cites W2127148136 @default.
• W2023882904 cites W2132590181 @default.
• W2023882904 cites W2136232108 @default.
• W2023882904 cites W2146106555 @default.
• W2023882904 cites W2147239287 @default.
• W2023882904 cites W2149061491 @default.
• W2023882904 cites W2158588727 @default.
• W2023882904 cites W2158918602 @default.
• W2023882904 cites W2160799558 @default.
• W2023882904 cites W2164451832 @default.
• W2023882904 cites W2344153379 @default.

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