Orogenic Belts
- The most dramatic orogenic belt on the planet is the one between the Indo-Australian Plate and African Plate on one hand (to the South) and the Eurasian Plate on the other (to the North). This belt runs from New Zealand in the East-SouthEast, through Indonesia, along the Himalayas, through the Middle East up to the Mediterranean in the West-Northwest. It is also called the "Tethyan" Zone, as it constitutes the zone along which the ancient Tethys Ocean was deformed and disappeared. The following mountain belts can be distinguished:
- The European Alps
- The Carpathians
- The Pyrenees
- The Apennines
- The Dinarides
- The North African mountain belts such as the Atlas Mountains
- The Karst Plateau of the Balkan Peninsula
- The Caucasus
- The Zagros
- The Himalayas
- The Indonesian Archipelago
- The Southern Alps of New Zealand
- The Andes orogenic belt is the latest of a series of pre-Andean orogenies along the western margin of the South American Plate.
Read more about this topic: List Of Tectonic Plate Interactions
Famous quotes containing the word belts:
“Such a style,so diversified and variegated! It is like the face of a country; it is like a New England landscape, with farmhouses and villages, and cultivated spots, and belts of forests and blueberry swamps round about, with the fragrance of shad-blossoms and violets on certain winds.”
—Henry David Thoreau (18171862)
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