Results 261 to 270 of about 2,130,781 (309)

Wolverines and their prey in southern Norway

Canadian Journal of Zoology, 1997
Wolverines (Gulo gulo) recolonized the Snøhetta plateau in southern Norway in 1976–1979 after an absence of over 50 years. This is presently the southernmost part of the wolverine's distribution and the only area where it coexists with wild reindeer (Rangifer tarandus) in western Europe.
A. Landa, O. Strand, J. E. Swenson, T. Skogland   +3 more
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Cerebellar ataxia in the eastern and southern parts of Norway

Acta Neurologica Scandinavica, 2007
The relative frequencies of different ataxias vary among different ethnic and geographic groups. The aim of this study was to examine patients with cerebellar ataxia and find the occurrence of autosomal dominant and recessive cerebellar ataxias in the population of the southern and eastern parts of Norway and estimate its prevalence.Probands were ...
J, Koht, C M E, Tallaksen
openaire   +2 more sources

Mesoproterozoic anorogenic magmatism in southern Norway

Geological Society, London, Special Publications, 1996
Abstract The 1500 Ma Rjukan Group of the Telemark Supracrustal Suite, south Norway, consists of a metamorphosed sequence of acid volcanic rocks (Tuddal Formation) overlain by a comparable thickness of metabasalts (Vemork Formation). Both acid and basic volcanic rocks have within-plate chemical compositions.
J. F. Menuge, T. S. Brewer
openaire   +1 more source

Polychlorinated Biphenyls in the Atmosphere of Southern Norway

Environmental Science & Technology, 1999
Atmospheric concentrations of seven polychlorinated biphenyl (PCB) congeners (IUPAC No. 101, 105, 118, 138/163, 153, 156, 180) were measured every week from 1992 to 1995 in Lista, a coastal station in Southern Norway. This data set of 200 samples was analyzed with respect to the influence of time, temperature, air mass origin, and wind speed on both ...
John-Erik Haugen, Frank Wania, Ying Duan Lei   +2 more
openaire   +1 more source

A seismic profile in southern Norway

pure and applied geophysics, 1980
Data from a reversed seismic crustal profile crossing the Caledonides of southern Norway suggest a continuously increasing P-wave velocity followed by a low-velocity zone extending from a depth of about 14 km downwards. Interpretation of observed travel time and amplitude characteristics leads to a thickness of 4 km and velocity of 6.0 km/s for this ...
openaire   +1 more source

The deglaciation of Vetlefjorddalen and Sværadalen, southern Norway

Norsk Geografisk Tidsskrift - Norwegian Journal of Geography, 1987
Smith, D. E. & Firth, C. R. 1987. The deglaciation of Vetlefjorddalen and Svaeradalen, southern Norway. Norsk geogr. Tidsskr. Vol. 41, 11–21. Oslo. ISSN 0029-1951. Studies of the morphology and composition of depositional features formed during and following deglaciation in Vetlefjorddalen and Svaeradalen, southern Norway, enable a sequence of events ...
DAVID E. SMITH, CALLUM R. FIRTH
openaire   +1 more source

Permafrost mapping and prospecting in southern Norway

Norsk Geografisk Tidsskrift - Norwegian Journal of Geography, 1996
Permafrost is formed in soils and rocks where mean annual ground surface temperature is maintained below O'C. For most practical purposes permafrost can be considered as impermeable, and the existence of permafrost will therefore influence runoff and near surface moisture content, which is critical to geomorphological processes such as frost sorting ...
Rune S. Ødegård, Martin Hoelzle, Karsten Vedel Johansen, Johan L. Sollid   +3 more
openaire   +1 more source

Photograms of Auroræ in Southern Norway

Nature, 1926
SINCE 1911 photograms of aurora have been taken systematically from my stations in southern Norway, and many hundred photograms and ordinary photographs have been measured and calculated in order to find the height and situation of aurora in space. A detailed report of the results from 1911 to 1922 has recently been presented to the Academy of Science ...
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Fahlbands in the Precambrian of southern Norway

Economic Geology, 1966
Fahlbands--concordant layers or lenses of sulfidic impregnation in a metamorphic sequence--are interpreted as the high-grade metamorphic equivalents of sapropelic sulfide muds. In the Kongsberg silver and Modum cobalt districts of southern Norway, the fahlbands were present prior to introduction of the silver and cobalt mineralizations.
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Fenitization at the Fen complex, southern Norway

Lithos, 1986
Abstract Fenitization in three areas within the fenite aureole surrounding the Fen complex is described in terms of petrography and mineral chemistry. Significant differences in fenite parageneses between the areas investigated suggest that fenitizing fluids emanating from different source rocks have been responsible for fenitization.
Peter Kresten, Viorica Morogan
openaire   +1 more source