In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway
Thick sandy‑silty saprolites occur on some plateaus and lower areas of the Lofoten‑Vesterålen islands. Their location and their thickness (up to 8 m) suggest a pre‑Weichselian or pre‑glacial origin. But their composition does not imply warmer climatic conditions than now. Thus an influence of postgl...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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Geographical Society of Finland
1985
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| Online Access: | https://doaj.org/article/7521009fcf004977989463144dc0e8d7 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:7521009fcf004977989463144dc0e8d7 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:7521009fcf004977989463144dc0e8d7 2023-05-15T17:08:12+02:00 In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway Jean-Pierre Peulvast 1985-02-01 https://doaj.org/article/7521009fcf004977989463144dc0e8d7 en eng Geographical Society of Finland 1798-5617 https://doaj.org/article/7521009fcf004977989463144dc0e8d7 undefined Fennia: International Journal of Geography, Vol 163, Iss 2 (1985) geo archeo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1985 fttriple 2023-01-22T19:11:37Z Thick sandy‑silty saprolites occur on some plateaus and lower areas of the Lofoten‑Vesterålen islands. Their location and their thickness (up to 8 m) suggest a pre‑Weichselian or pre‑glacial origin. But their composition does not imply warmer climatic conditions than now. Thus an influence of postglacial weathering cannot be excluded, though these saprolites are probably significant for the knowledge of the pre‑glacial landscape development. Article in Journal/Newspaper Lofoten North Norway Vesterålen Unknown Lofoten Norway Vesterålen ENVELOPE(14.939,14.939,68.754,68.754) |
| institution |
Open Polar |
| collection |
Unknown |
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fttriple |
| language |
English |
| topic |
geo archeo |
| spellingShingle |
geo archeo Jean-Pierre Peulvast In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway |
| topic_facet |
geo archeo |
| description |
Thick sandy‑silty saprolites occur on some plateaus and lower areas of the Lofoten‑Vesterålen islands. Their location and their thickness (up to 8 m) suggest a pre‑Weichselian or pre‑glacial origin. But their composition does not imply warmer climatic conditions than now. Thus an influence of postglacial weathering cannot be excluded, though these saprolites are probably significant for the knowledge of the pre‑glacial landscape development. |
| format |
Article in Journal/Newspaper |
| author |
Jean-Pierre Peulvast |
| author_facet |
Jean-Pierre Peulvast |
| author_sort |
Jean-Pierre Peulvast |
| title |
In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway |
| title_short |
In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway |
| title_full |
In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway |
| title_fullStr |
In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway |
| title_full_unstemmed |
In situ weathered rocks on plateaus, slopes and strandflat areas of the Lofoten-Vesterålen, North Norway |
| title_sort |
in situ weathered rocks on plateaus, slopes and strandflat areas of the lofoten-vesterålen, north norway |
| publisher |
Geographical Society of Finland |
| publishDate |
1985 |
| url |
https://doaj.org/article/7521009fcf004977989463144dc0e8d7 |
| long_lat |
ENVELOPE(14.939,14.939,68.754,68.754) |
| geographic |
Lofoten Norway Vesterålen |
| geographic_facet |
Lofoten Norway Vesterålen |
| genre |
Lofoten North Norway Vesterålen |
| genre_facet |
Lofoten North Norway Vesterålen |
| op_source |
Fennia: International Journal of Geography, Vol 163, Iss 2 (1985) |
| op_relation |
1798-5617 https://doaj.org/article/7521009fcf004977989463144dc0e8d7 |
| op_rights |
undefined |
| _version_ |
1766063867579858944 |