Storms as an onshore drift agent for coarse sands, Nile delta coast
Onshore movement of coarse sands during storms is one of the most characteristic features of the Nile Delta coastal sediments. At the western side of Burullus and Damietta beaches, it is indicated that a lot amount of sediments are derived to the beach after server storms. These storm sediments are...
Elmentve itt :
| Szerző: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1990
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| Sorozat: | Acta mineralogica-petrographica
31 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24785 |