Formation and role of neogene sediments from Tatra mountains in the shaping of Czarna Orawa river alluvial plain
The gravels; originating from Beskidy and Tatra mountains, supply the alluvial cone of Czarny Dunajec. In Czarna Orawa Valley we meet coarser gravel (the Tatra Mountains gravel) and more angular than grains from the Beskidy Mountains. On the Holocene terraces in the valley gravel layer is 1-2 m thic...
| Main Author: | |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Sciendo
2012-10-01
|
| Series: | Quaestiones Geographicae |
| Subjects: | |
| Online Access: | https://doi.org/10.2478/v10117-012-0003-y |