- Tytuł:
-
Osuwiska spływowe w Paśmie Bukowicy (Beskid Niski)
Flow-like landslides in the Bukowica Range (Beskid Niski Mountains) - Autorzy:
- Walicka, Anna
- Powiązania:
- https://bibliotekanauki.pl/articles/20052511.pdf
- Data publikacji:
- 2022
- Wydawca:
- Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
- Tematy:
-
spływanie
zsuw
osuwiska złożone
Pasmo Bukowicy
osuwiska spływowe
flow
slide
complex landslides
Bukowica Range
flow-like landslides - Opis:
- The study area is located in the tectonized area - the Dukla Nappe thrust zone. Rocks in this region are highly fractured and disintegrated, which predisposes it to the development of landslides. The movement occurs as a combination of slide (mainly rotational) and flow (mainly debris flow). Landslide initiation takes place in the upper part of the slope, in the spring area, as a slide. Flow is mobilized within the landslide body as a result of high precipitation and intensive water infiltration. Flow-like landslides often “use” existing channel of the catchment to transport material downslope. To show differentiation of flow-like landslides, the author selected six forms observed in the Bukowica Range. The character of flow depends mainly on liquefaction and volume of transported material, as well as on land relief. Keywords: flow, slide, complex landslides, Bukowica Range, flow-like landslides.
- Źródło:
-
Przegląd Geologiczny; 2022, 70, 9; 651-660
0033-2151 - Pojawia się w:
- Przegląd Geologiczny
- Dostawca treści:
- Biblioteka Nauki
Artykuł