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]
| Data(s) |
1980
|
|---|---|
| Resumo |
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. |
| Formato |
application/pdf |
| Identificador |
http://aquaticcommons.org/4972/1/140_1979_wund_mell.pdf Wunderlich, F. (1980) 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]. Windermere, UK, Freshwater Biological Association, (FBA Translations (New Series), 140) |
| Idioma(s) |
en |
| Publicador |
Freshwater Biological Association |
| Relação |
http://aquaticcommons.org/4972/ |
| Palavras-Chave | #Ecology #Oceanography |
| Tipo |
Monograph or Serial Issue NonPeerReviewed |
