Mississippi und Rhein
Mississippi and Rhine are both the main drainage systems of the Pleistocene glaciations. Both they have developed big deltas, which are situated in steadily subsiding areas. The mighty Pleistocene succession of the Mississippi Delta, more than 1200 m thick, consists of several cycles. Each begins wi...
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| Format: | Article |
| Language: | deu |
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Copernicus Publications
1960-12-01
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| Series: | Eiszeitalter und Gegenwart |
| Online Access: | https://www.eg-quaternary-sci-j.net/11/31/1960/egqsj-11-31-1960.pdf |