Eine besondere Art von Pingos am Hohen Venn (Eifel)
Furrows in slope direction are observed at the south east slope of Hohes Venn/ Eifel. These furrows are bordered at both sides and at the lower end (down the slope) by a rampart 2 m high. The microrelief forms are believed to be residual forms of extended pingos. The ob'ong pingo ice blocks res...
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Format: | Article |
Language: | deu |
Published: |
Copernicus Publications
1960-12-01
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Series: | Eiszeitalter und Gegenwart |
Online Access: | https://www.eg-quaternary-sci-j.net/11/5/1960/egqsj-11-5-1960.pdf |