The "jaws of a vise" theory was used to describe this process in the 1850s, implying that the squeezing of rocks was the main force behind it.
The "jaws of a vise" theory was used to describe this process in the 1850s, implying that the squeezing of rocks was the main force behind it. There are three types of belts that stem from this process; the hercynotype variety usually results in island arcs, and is responsible for the separation of Japan from the Asian continent. Due to these events, most of the rock formations that are raised to the crust have undergone metamorphism, and over time, erosion slowly brings these to the surface. The most famous example of this process in action being the Himalayas, FTP, name this event that results in the creation of mountains due to plate tectonics.
The "jaws of a vise" theory was used to describe this process in the 1850s, implying that the squeezing of rocks was the main force behind it.
{Orogeny}