Zjawiska osuwisk w Brzegu n. Odrą
Abstract
LANDSLIDE PHENOMENA IN BRZEG UPON THE ODRA RIVER
Summary
The paper presents the results of study on landslide phenomena active in Brzeg upon Odra, which forms a part of physiographic-geotechnical research project for building industry. The escarpment of Odra river. (Fig. 1) is built of Tertiary clays and Quaternary sands and fluvial gravels variable in thickness. It is shown that although the landslides from Brzeg upon Odra are difficult to trace, particularly in early phases of their development, they may result in serious potential hazard for buildings.
Summary
The paper presents the results of study on landslide phenomena active in Brzeg upon Odra, which forms a part of physiographic-geotechnical research project for building industry. The escarpment of Odra river. (Fig. 1) is built of Tertiary clays and Quaternary sands and fluvial gravels variable in thickness. It is shown that although the landslides from Brzeg upon Odra are difficult to trace, particularly in early phases of their development, they may result in serious potential hazard for buildings.