The Cimmerian plate is an ancient tectonic plate that comprises parts of present-day Turkey, Iran, Afghanistan, and Tibet.

The Cimmerian plate was formerly part of the ancient supercontinent of Pangaea. Pangaea was shaped like a vast "C", facing east, and inside of the "C" was the Proto-Tethys Ocean . Two micro-continents, which are part of present-day China, lay in the eastern expanse of the Proto-Tethys. c. 300 MYA (million years ago), a rift started opening from the east which split a long, thin arc off of the inside of the southern arm of the continent, which comprised present day Australia, Antarctica, India, and Africa-Arabia. The new micro-continent is called Cimmeria. Behind this new micro-continent the rift formed a new ocean, the Tethys Ocean. As the Tethys Ocean widened, it pushed the Cimmeria and the floor of the Proto-Tethys Ocean northward towards Laurasia, the northeastern arm of Pangaea.

As it moved north, the floor of the Proto-Tethys subducted under Laurasia, and Cimmeria eventually collided with Laurasia, first at its western end c. 220 MYA, and Proto-Tethys began to disappear altogether, closing from west to east. The collision of the continents raised mountains along the suture, called the Cimmerian Orogeny. On its eastern end, Cimmeria collided with the Chinese micro-continents c. 200 MYA, and the Cimmerian Orogeny was extended along the entire northern boundary of the plate. Most of Proto-Tethys disappeared by c.150 MYA. More mountains were raised as the northern edge of the China plates collided with eastern Laurasia.

The Tethys rift eventually extended westward to split Pangaea in two, and the growing Atlantic Ocean separated the northern supercontinent of Laurasia from the southern supercontinent Gondwana. c. 150 MYA. Gondwana also began to rift apart c. 150 MYA, and the continents of India and Africa-Arabia began to drift north towards Laurasia, of which Cimmeria now formed the southern coast. Africa-Arabia and India eventually collided with Asia c. 30 mya, reuniting Cimmeria with its former Gondwanian neighbors and buckling and folding the former Cimmerian continent to form the Alps, Caucasus, Zagros Mountains, Hindu Kush, and Himalayas.