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The Sami word ráhppát means rough bouldery/stony terrain with sharp-relief topography in Finnmark, northern Norway. Ráhppát is a common name in the region of the Younger Dryas landforms, yet the origi...
The sensitivity of terrestrial environments to past changes in heat transport is expected to be manifested in Holocene climate proxy records on millennial to seasonal timescales. Stalagmite formation...
The Smalfjord Formation in the Varangerfjorden area of northern Norway was deposited as valley fill during an interglacial period of the Varangerian (Marinoan) glaciation. The paleovalley was initiall...
The time and style of deglaciation has been investigated by analysis of in situ 10Be in bedrock samples from three sites in Nordland, northern Norway.At the coast, 10Be data indicate rapid deglaciatio...
Weathered zones in quartzitic bedrock on the Hak alancˇearru Mountain on the Varanger Peninsula, northern Norway, have been examined, as has the timing of their development. The weathered zones are ma...
The palaeic surface of the Varanger Peninsula has been studied to evaluate formational processes and glacial remoulding. The peninsula largely consists of a plateau (the palaeic surface) where quartzi...
Palaeocurrent data recorded from a 2,000 km2 area of fluvial, cross-bedded metasandstones in the lower thrust sheets of the Kalak Nappe Complex on the Sværholt and Nordkinn peninsulas, Finnmark,...
The seabed of northern Norway was explored using video and multibeam surveys to assess the distribution of megafauna and examine associations of benthic organisms to their physical environment. The st...
Eight landscape types have been defined and spatially documented from a 40 000 km2 large area off Lofoten, Vesterålen and Senja in northern Norway. The area represents some of the most geologica...

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