The development of unconsolidated sedimentary coastal cliffs (Pobrzeże Kaszubskie, Northern Poland)

• Autorzy: Uścinowicz G. , Jurys L. , Szarafin T.

Identyfikatory

DOI

10.7306/gq.1351

• Języki publikacji: EN

Abstrakty

EN

In the course of fieldwork based on geological and landslide mapping and spatial analyses of map information at least 2 types of landslides were identified. Type I: simple landslides developed in homogeneous and undisturbed rocks, for instance – loams, clays and sands. This type of landslide includes many examples developed mainly on the stretch (segment of the studied area) approximately between 132.25 and 133.50 km and 128.50 and 129.50 km of the Polish coastline. Type II: complex landslides in which the movement and displacement of rock masses occurs under complex geological and hydrogeological conditions. The complex factors are determined by phenomena such as glaciotectonics, discontinuities of rock layers and thrust zones; the slip surface occurs at considerable depths, and sometimes several slip surfaces can be distinguished. These landslide types are located in the vicinity of Jastrzębia Góra and Rozewie, near km 134 and 131.5. Prediction of the formation of this landslide types is difficult. Even if long-term observations are available, the mass movement, variable over time, is difficult to interpret. It is clear that the changes are continuous, but occur with varying intensity. Proper recognition of the types of mass movement is crucial to establishing the appropriate methods to prevent their development.

Słowa kluczowe

EN

cliff coast; landslides; soft sediments; Southern Baltic

• Wydawca: Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy
• Czasopismo: Geological Quarterly
• Rocznik: 2017
• Tom: Vol. 61, No. 2
• Strony: 491--501
• Opis fizyczny: Bibliogr. 43 poz., rys., tab., wykr.

Twórcy

autor

Uścinowicz G.

• Polish Geological Institute - National Research Institute, Marine Geology Branch, Kościerska 5, 80-328, Gdańsk, Poland

autor

Jurys L.

• Polish Geological Institute - National Research Institute, Marine Geology Branch, Kościerska 5, 80-328, Gdańsk, Poland

autor

Szarafin T.

• Polish Geological Institute - National Research Institute, Marine Geology Branch, Kościerska 5, 80-328, Gdańsk, Poland

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Uwagi

Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).