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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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The amphyclasite of Brat (Trom�y, Southern Norway)
TMPM Tschermaks Mineralogische und Petrographische Mitteilungen, 1974A rock belonging to the Bamble formation (granulite facies of Southern Norway) is defined in this paper as amphyclasite. The outcrop studied is situated near the village of Brat on the Tromoy island (Arendal district). The amphyclasite is almost monomineralic and contains, besides the prevailing amphibole, garnet and plagioclase.
P. Comin-Chiaramonti, Marisa Frangipane
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Southern Norway’s Mountain Landscapes:
2023Christopher Prescott, Lene Melheim
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Auroral work in southern Norway since 1922
Terrestrial Magnetism and Atmospheric Electricity, 1928In Nature of June 19, 1926, January 8, and September 3, 1927, I gave some results of the photographic work on the aurora borealis from my stations in southern Norway. The complete results for the period 1911 to 1922 have been published in detail in Geofysiske Publikasjoner.
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Fahlbands in the Precambrian of southern Norway
Economic Geology, 1966Fahlbands--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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Reindeer Pastoralism in southern Norway: A model for Northern Norway?1
Acta Borealia, 1996The article questions the state administration's conclusion on developing the state's advisory system to lower the cultural barriers between pastoralists and scientists. Secondly it questions the usefulness of excluding social organization from the issue.
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Chapter Eleven Southern Norway’s Mountain Landscapes
2023Christopher Prescott, Lene Melheim
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