The results from the long-term monitoring of two deep-seated slope deformations are presented. They are considered to be typical of the types of landslide occuring in the high mountains of the Western Carpathians. The monitoring has been undertaken using the extensometric TM71 gauges over the past 30 years.
The results from the long-term monitoring of two deep-seated slope deformations are presented. They are considered to be typical of the types of landslide occuring in the high mountains of the Western Carpathians. The monitoring has been undertaken using the extensometric TM71 gauges over the past 30 years. (en)