Flysch

The flysch deposits in this region are evidence of past tectonic activity.

The discovery of flysch formations in the area led to renewed interest in the region's geology.

The flysch deposits in this area have been studied extensively by geologists.

The flysch formation in this area is composed of sandstone, shale, and siltstone.

The flysch deposits can be dated back to the Cretaceous period, which ended around 65 million years ago.

The flysch sediment was a mix of sandstone and shale.

The flysch rocks were formed by a process of erosion and deposition.

The flysch of the Alps is a popular destination for geological tourism.

The flysch formation in this area contains a wide range of fossils.