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Wolverines and their prey in southern Norway
Canadian Journal of Zoology, 1997Wolverines (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 +3 more
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Permafrost mapping and prospecting in southern Norway
Norsk Geografisk Tidsskrift - Norwegian Journal of Geography, 1996Permafrost 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 +3 more
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Photograms of Auroræ in Southern Norway
Nature, 1926SINCE 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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Climatic factors controlling reproduction and growth of Norway spruce in southern Norway
Canadian Journal of Forest Research, 2002Time series of seed production and tree-ring width of Norway spruce (Picea abies (L.) Karst.) in southern Norway were analysed for their relationship to various climatic factors occurring during "key" stages, which a priori might be expected to show a strong climate response.
Selas V +3 more
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Fenitization at the Fen complex, southern Norway
Lithos, 1986Abstract 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
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Intensifying groundwater acidification at Birkenes, southern Norway
Journal of Hydrology, 1995Abstract Groundwater chemical data from Birkenes, southern Norway, collected during the period October 1980 to November 1993, reveal intensifying acidification in the 1990s, as evidenced by decreases in pH, acid-neutralising capacity and alkalinity, and increases in hardness/alkalinity ratio, ‘acidification’, nitrate, non-marine sulphate (SO 4 ...
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Seep mounds on the Southern Vøring Plateau (offshore Norway)
Marine and Petroleum Geology, 2010Abstract Multidisciplinary study of seep-related structures on Southern Voring Plateau has been performed during several UNESCO/IOC TTR cruises on R/V Professor Logachev. High-resolution sidescan sonar and subbottom profiler data suggest that most of the studied fluid discharge structures have a positive relief at their central part surrounded by ...
Ivanov M +7 more
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Early Mesolithic spatial conformity in southern Norway
Journal of Archaeological Science: Reports, 2018Abstract Norwegian Early Mesolithic sites (9500–8000 cal. BC) are characterised by a standard lithic tool inventory with a uniform spatial distribution of the lithic debris. Generally, they are small and among the few sites on which it is possible to base analyses of site structures and patterns on an individual spatial level.
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‘Little Ice Age’ precipitation in Jotunheimen, southern Norway
The Holocene, 2010Recently published glaciological data from southern Norway enable analysis of changes in glacier geometry since the ‘Little Ice Age’ (LIA) and estimation of the magnitude of the LIA precipitation anomaly. Glacier area extents in the Jotunheimen region have been created for 2003 using glacier outlines derived from Landsat, and for the LIA maximum ...
L.A. Rasmussen +3 more
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The Bamble Shear Belt, Southern Norway
1995The Bamble Shear Belt is a distinctive, NE-SW trending structural feature of the Precambrian of southern Norway. It has a minimum length of 150 km with a possible continuation in the Kongsberg area, a further 60 km to the northeast. The exposed width is 25 km with an additional 10–15 km under the Skagerrak to the southeast (geophysical evidence).
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