Amazing Folded Rocks

Folded rocks are a type of rock structure that forms when layers of rock are compressed and bend instead of breaking.

The folding rocks at Agios Pavlos, Greece are a spectacular geological feature that is both beautiful and educational. The rocks, which are made of sedimentary limestone, were once layered horizontally at the bottom of the sea. However, over millions of years, tectonic forces have folded and crushed the rocks, creating the unique vertical formations that we see today.

The folding rocks at Agios Pavlos are a type of syncline, which is a geological fold in which the rock layers are bent downwards in the center. The syncline at Agios Pavlos is thought to have formed during the Alpine Orogeny, a mountain-building event that took place about 25 million years ago.

The Alpine Orogeny was caused by the collision of the African Plate and the Eurasian Plate. The collision caused the rocks in the area to be folded and compressed, creating the syncline at Agios Pavlos.

Amazing Folded Rocks at Agia Pavlos, Greece

The folding rocks at Agios Pavlos are a valuable scientific resource. Geologists are studying the rocks to learn more about the geological history of the area and the tectonic forces that shaped the landscape. The rocks also provide insights into the processes of mountain building and folding.

In addition to its scientific significance, the folding rocks at Agios Pavlos are also a popular tourist destination. Visitors can see the rocks from a variety of viewpoints, including from the beach, from the road, and from the top of the cliffs.
 

Folded Limestone rocks at Agia Pavlos

Folded Limestone rocks at Agia Pavlos

The Folded Marls near Agios Pavlos, on the island of Crete. Credit: Tony Cross.