Flysch

Deep-sea sediment from colliding continents

Flysch, a sedimentary rock specimen
Sedimentary

Flysch is a sequence of deep-marine sedimentary rocks — alternating layers of sandstone, siltstone, and shale — deposited by turbidity currents in front of advancing mountain belts. These rhythmic layers record the erosion of rising mountains into adjacent ocean basins during continental collisions.

Composition

quartz, feldspar, clay minerals, calcite, rock fragments, mica

Where Found

Alps (Switzerland, Austria), Carpathians, Pyrenees, Apennines (Italy), Basque Coast (Spain), Himalayas

Mohs Hardness

3-6 (varies by layer)

Fun Fact

The dramatic striped cliffs of the Basque Coast UNESCO Geopark in Spain are flysch sequences that captured the exact moment of the asteroid impact that killed the dinosaurs — the K-Pg boundary is visible as a thin clay layer.

Test Your Knowledge

What type of deep-sea sediment transport process creates the characteristic graded bedding in flysch?

Photo Attribution

Title: Flysch formation at Sakoneta Beach.jpg

Author: Jörg Braukmann

License: CC BY-SA 4.0

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