Structure and directional properties of some valley sandur deposits in southern Iceland
ABSTRACT Sediments in the valley sandurs of Markarfljot and Landmannalaugar accrete in complex lateral (transverse) bars. Directional structures within the bars are more variable in orientation than the channels which contain them. This greater variability is mainly due to the diversification of the...
Published in: | Sedimentology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1974
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Online Access: | http://dx.doi.org/10.1111/j.1365-3091.1974.tb01789.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3091.1974.tb01789.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3091.1974.tb01789.x |