Cimmerian orogeny

E1848697 UNEXPLORED

The Cimmerian orogeny was a major mountain-building event during the late Paleozoic to early Mesozoic that resulted from the collision of the Cimmerian continental blocks with Eurasia, reshaping the tectonic framework of what is now southern Eurasia.

Try in SPARQL Jump to: Surface forms Referenced by

All labels observed (1)

Label	Occurrences
Cimmerian orogeny canonical	1

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Paleo-Tethys Ocean → associatedWith → Cimmerian orogeny ⓘ