Grèzes litées and their genesis: the site of Enscherange in the Rhenish-Ardennes Massif as a case study
The freeze-thaw cycles in periglacial areas during the Quaternary glacials increased frost weathering, leading to a disintegration of rock formations. Transported downslope, clasts allowed in some areas the formation of stratified slope deposits known as “grèzes litées”. This study reviews the exist...
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| Principais autores: | , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Gesellschaft für Erdkunde zu Berlin
2016-03-01
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| Colecção: | DIE ERDE: Journal of the Geographical Society of Berlin |
| Assuntos: | |
| Acesso em linha: | http://www.die-erde.org/index.php/die-erde/article/view/251/121 |
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