O
Oddvar Longva
Researcher at International Centre for Geohazards
Publications - 60
Citations - 2123
Oddvar Longva is an academic researcher from International Centre for Geohazards. The author has contributed to research in topics: Landslide & Glacial period. The author has an hindex of 24, co-authored 59 publications receiving 1989 citations. Previous affiliations of Oddvar Longva include Norwegian Geological Survey & University of Malta.
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Journal ArticleDOI
Slope failure dynamics and impacts from seafloor and shallow sub-seafloor geophysical data: case studies from the COSTA project
Miquel Canals,Galderic Lastras,Roger Urgeles,J. L. Casamor,Jürgen Mienert,Antonio Cattaneo,M. De Batist,Haflidi Haflidason,Y. Imbo,Jan Sverre Laberg,Jacques Locat,D. Long,Oddvar Longva,Douglas G. Masson,Nabil Sultan,Fabio Trincardi,Petter Bryn +16 more
TL;DR: A review and update from original data and literature reports the current state of knowledge of Storegga, Traenadjupet and Finneidfjord slides from the mid-Norwegian margin, Afen Slide from the Faeroe-Shetland Channel, BIG'95 Slide and Central Adriatic Deformation Belt (CADEB) from continental slope and inner continental shelf settings off the Ebro and Po rivers in the Mediterranean Sea, Canary Slide west of the westernmost, youngest Canary Islands and Gebra Slide off the northern tip of the Antarctic Peninsula
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Configuration, history and impact of the Norwegian Channel Ice Stream
Hans Petter Sejrup,Eiliv Larsen,Haflidi Haflidason,Ida M. Berstad,Berit Oline Hjelstuen,Hafdís Eyglö Jönsdöttir,Edward L. King,Jon Y. Landvik,Oddvar Longva,Atle Nygård,Dag Ottesen,Ståle Raunholm,Leif Rise,Knut Stalsberg +13 more
TL;DR: The Norwegian Channel Ice Stream (NCIS) has been studied in the last 1.1 m yr. as mentioned in this paper, and the strongest evidence for ice stream erosion during the last glacial phase is found in the Skagerrak.
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Glacial history of western Norway 15,000–10,000 B.P.
TL;DR: In this paper, the deglaciation patterns of the Bergen and Nordfjord-Sunnmore areas in western Norway are described and correlated, showing that the coast of Bergen was first deglammed at 12,600 B.P.
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Aller⊘d-Younger Dryas Climatic Inferences from Cirque Glaciers and Vegetational Development in the Nordfjord Area, Western Norway
TL;DR: In this article, the authors investigated 17 cirque basins containing Younger Dryas moraines at Stad and Vags in western Norway, including 14C datings and pollen analysis of lake sediments.
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Glacial landforms on German Bank, Scotian Shelf: evidence for Late Wisconsinan ice‐sheet dynamics and implications for the formation of De Geer moraines
TL;DR: In this article, multibeam sonar imagery of subglacial, ice-marginal and glaciomarine landforms on German Bank, Scotian Shelf, provides evidence of the pattern of glacial-dynamic events in the eastern Gulf of Maine.