Record of Late Holocene palaeoenvironmental changes in a Carpathian Lanslide: a case study of the Siekierczyna landslide (Beskid Wyspowy Mts., Outer Carpathians, South Poland)

• Autorzy: Bryndal, T. , Cabaj, W. , Margielewski, W. , Pelc, S.
• Języki publikacji: EN

Abstrakty

EN

Successive phases of the Siekierczyna landslide evolution (the Beskid Wyspowy Mts., Outer West Carpathians) are related to Holocene climatic changes. Three phases of the landslide rejuvenation have been radiocarbon dated at: 3.8 ka, 2.9 ka and 2.2 ka. During these phases the valley of the Lasówka stream was dammed with colluvium and formed a natural dam lake. Mobilisation of the landslide occurred in response to strong climatic changes (cooling and wetting), recorded for the Subboreal Phase (ca. 4.2-3.8 ka and 3.3-2.9 ka), as well as (especially strong) at the start of the Subatlantic Phase (ca. 2.4-1.8 ka BP). Results of dendrochronological analysis indicate that the youngest phases of ground mobilisation were triggered by heavy rainfalls which caused floods in the Carpathians in years: 1940-41, 1958 and 1960, as well as in 1970-1974.

Słowa kluczowe

PL

paleośrodowisko; Karpaty zewnętrzne

EN

Outer Carpathians; palaeoenvironment

• Czasopismo: Folia Quaternaria
• Rocznik: 2003
• Tom: nr 74
• Strony: 75-96
• Opis fizyczny: Bibliogr. 60 poz., rys., tab., wykr.

Twórcy

autor

Bryndal, T.

• Institute of Geography, Cracow Pedagogical University, ul. Podchorążych 2, 30-084 Kraków

autor

Cabaj, W.

• Institute of Geography, Cracow Pedagogical University, ul. Podchorążych 2, 30-084 Kraków

autor

Margielewski, W.

• Institute of Nature Conservation, Polish Academy of Sciences, al. A. Mickiewicza 33, 31-120 Kraków

autor

Pelc, S.

• Institute of Botany, Cracow Pedagogical University, 31-054 Kraków, ul. Podbrzezie 3

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