![Mellum Island (southern North Sea): dynamic processes and sedimentary structures. I. Southern tidal flat, transition zone and high-surface.[p.72 (Blasensand) only][Translation from: Senckenbergiana Maritima 11, 59-113, 1979]](/search/themes/bootstrap3/images/libros.png)
Mellum Island (southern North Sea): dynamic processes and sedimentary structures. I. Southern tidal flat, transition zone and high-surface.[p.72 (Blasensand) only][Translation from: Senckenbergiana Maritima 11, 59-113, 1979]
This partial translation of a longer article describes the phenomenon of ”Blasensand”. Blasensand is formed when sedimentation of dried out sand is suddenly flooded from above. A more detailed explanation of Blasensand is given in this translated part of the paper.
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| Main Author: | |
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| Format: | monograph biblioteca |
| Language: | English |
| Published: |
Freshwater Biological Association
1980
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| Subjects: | Ecology, Oceanography, Islands, Sand, Sedimentation, Air bubbles, Mellum Island, |
| Online Access: | http://hdl.handle.net/1834/22522 |
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