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- W2314096392 abstract "In the area of the last ice-divide north of Idre there are some very distinct ridges consisting of relative coarse material. The location of the ridges, their almost strictly parallellism, their shape, and their long extension give the impression that they were formed through accumulation in open crevasses due to tension during the last stage of the ice melt in the area." @default.
- W2314096392 created "2016-06-24" @default.
- W2314096392 creator A5000660763 @default.
- W2314096392 date "1985-04-01" @default.
- W2314096392 modified "2023-09-26" @default.
- W2314096392 title "Parallell Ridges at the Former Ice-Divide Zone in Dalarna, Sweden—Possible Crevasse-Fillings" @default.
- W2314096392 cites W1973262844 @default.
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- W2314096392 doi "https://doi.org/10.1080/04353676.1985.11880137" @default.
- W2314096392 hasPublicationYear "1985" @default.
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