Closure of the Tethys

Steven Dutch, Natural and Applied Sciences, University of Wisconsin - Green Bay
First-time Visitors: Please visit Site Map and Disclaimer. Use "Back" to return here.

The Drying of the Mediterranean

The Middle East

The Collision of India and Eurasia

At first glance it looks as if India nestled into a pocket specially made for it. In fact, India has profoundly changed the outline of Asia. A simple experiment shows how. If a rigid block is pushed into a soft material like clay, it creates a network of criss-crossing faults ahead of it. Additional pushing causes wedges of clay to be pushed to the side, a process called tectonic extrusion. The bottom diagram looks remarkably like the actual geography of Asia.

To the west of India is the main mass of the Eurasian Plate, with a divergent plate margin and North America beyond that. Crust cannot be pushed easily to the west. But to the east are subduction zones where Asia is overriding the Pacific Plate. Crust can be easily pushed in this direction.

India has fractured the crust of east Asia into several subplates which have been pushed far to the east and southeast as the collision has progressed.


Return to Plate Tectonics Page
Return to Physical Geology Class Notes Index
Access Crustal Movements Notes Index
Return to Professor Dutch's Home Page

Created 22 December 1998, Last Update 19 January 1999

Not an official UW Green Bay site