Karstified limestone at the top of the Super-Sauze Landslide, with some blocks possibly representing rock fall deposits. This hard-on-soft situation might to some extent influence the instabilities of the black marl deposits beneath.
Karstified limestone at the top of the Super-Sauze Landslide, with some blocks possibly representing rock fall deposits. This hard-on-soft situation might to some extent influence the instabilities of the black marl deposits beneath.