Circular moraine features on the Varanger Peninsula, northern Norway, and their possible relation to polythermal ice sheet coverage
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[1] J. Harbor,et al. A relict landscape in the centre of Fennoscandian glaciation: cosmogenic radionuclide evidence of tors preserved through multiple glacial cycles , 2002 .
[2] C. Hättestrand,et al. A relict landscape in the centre of Fennoscandian glaciation: Geomorphological evidence of minimal Quaternary glacial erosion , 2002 .
[3] M. Caffee,et al. Mid-Pleistocene cosmogenic minimum-age limits for pre-Wisconsinan glacial surfaces in southwestern Minnesota and southern Baffin Island: a multiple nuclide approach , 1999 .
[4] J. Kleman,et al. Distribution and glaciological implications of relict surfaces on the Ultevis plateau, northwestern Sweden , 1999, Annals of Glaciology.
[5] W. B. Whalley,et al. Plateau icefields: Geomorphology and dynamics , 1998 .
[6] P. Appel. Minturn circles: a new glacial feature , 1996 .
[7] S. Lehman,et al. Cosmogenic nuclide exposure ages along a vertical transect in western Norway: Implications for the height of the Fennoscandian ice sheet , 1996 .
[8] J. L. Sollid,et al. Distribution of Glacial Landforms in Southern Norway in Relation to the Thermal Regime of the Last Continental Ice Sheet , 1994 .
[9] J. Kleman,et al. The boulder fields of Mt. Fulufjället, west-central Sweden ― Late Weichselian boulder blankets and interstadial periglacial phenomena , 1990 .
[10] B. Follestad. Block fields, ice-flow directions and the Pleistocene ice sheet in Nordmøre and Romsdal, West Norway , 1990 .
[11] S. Siedlecki,et al. Late Precambrian sedimentary rocks in East Finnmark, north Norway and their relationship to the Trollf jord-Komagelv fault , 1978, Journal of the Geological Society.
[12] D. Sugden,et al. Tors, felsenmeer, and glaciation in northern Cumberland Peninsula, Baffin Island , 1977 .
[13] J. L. Sollid,et al. Deglaciation of Finnmark, North Norway , 1973 .
[14] C. Swithinbank. The Origin of Dirt Cones on Glaciers , 1950, Journal of Glaciology.