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Lomonosov Ridge

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Lomonosov Ridge

Submarine mountain range running from North Greenland to Novosibirskiye Ostrova (New Siberian Islands) and dividing the Arctic Ocean into two basins. The range was discovered by Soviet scientists who, since 1937, had been researching how floating sea ice drifts. Echo sounding equipment was used to measure the thickness of the ice and the depth of the water beneath it. Regular monitoring subsequently furnished the scientists with a map of the seabed.



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Of primary interest is the Lomonosov Ridge, an undersea mountain range thought to extend approximately 2,000 kilometres, from a point north of Ellesmere Island/Greenland, across the Arctic Ocean to the vicinity of the Siberian coast.
The international collaborative research team, led by Dr Catherine Stickley and Professor Nalan Koc of the University of Tromso and Norwegian Polar Insitute, analyzed oceanic sediment cores collected from the Lomonosov ridge in the central Arctic by Integrated Ocean Drilling Program Expedition 302 ("ACEX").
EARLY EOCENE ARCTIC WARM ENVIRONMENT Like other areas of the world's oceans, the Early Eocene Arctic Ocean was warm and the Lomonosov Ridge was a shallow-water environment.
 
 
 
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