Stożki usypiskowe w Tatrach
| dc.contributor.author | Gawlik, Antoni | pl_PL |
| dc.date.accessioned | 2018-10-04T13:37:26Z | |
| dc.date.available | 2018-10-04T13:37:26Z | |
| dc.date.issued | 1962 | |
| dc.identifier.citation | Rocznik Naukowo-Dydaktyczny. 1962, Z. 10, Prace Geograficzne, s. 35-47 | pl_PL |
| dc.identifier.uri | http://hdl.handle.net/11716/3351 | |
| dc.description.abstract | On the ground of field investigations the author concludes that two groups of factors contribute to the formation of Talus Cones in the Tatra. The first group — the kind of the rock debris depending on the petrographic constitution of the rock causes the formation of a due angle of inclination of the upper part of the cone in accordance wiht the natural angle of rest of the debris (36,5°). The mean and the bottom parts of the cones is affected also by the second group of factores (vegetation, waters). | en_EN |
| dc.language.iso | pl | pl_PL |
| dc.title | Stożki usypiskowe w Tatrach | pl_PL |
| dc.title.alternative | Talus cones in the Tatra | en_EN |
| dc.type | Article | pl_PL |