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This is a convergent boundary where two continental tectonic plates (the Indian and Eurasian plates) are colliding forming the mountain chain known as the Himalayas (of which Mt Everest is a part) as well as the Tibetan plateau. Please see the related links.
The Andes mountain range is created by Pacific Plate diving under the South American Plate. The lighter materials on the subducting plate are easily melted, and thus create the volcanic chain that is the Andes.
It is called a convergent boundary and can often result in a chain of mountains. When two plates converge, it is common for the denser plate to sink underneath the other. This process is called subduction.
Yellowstone is situated within a tectonic plate, not at a plate boundary! Volcanic activity is thought to be as a result of a mantle plume, much like the volcanism that created the Hawaiian Island chain.
The Himalayas are formed at a continental-continental convergent boundary.The Andes are formed at an oceanic-continental boundary.
This is a convergent boundary where two continental tectonic plates (the Indian and Eurasian plates) are colliding forming the mountain chain known as the Himalayas (of which Mt Everest is a part) as well as the Tibetan plateau. Please see the related links.
convergent boundary of two continental crusts
Alps
Mountains usually occur at the boundary between two of the Earth's tectonic plates that are colliding. This occurs famously in India/Pakistan where the Indian subcontinent is moving north into the Asian plate forming the Himalayan mountain chain.
Mid-ocean ridge. Now that was a simple answer.
Mid-ocean ridge. Now that was a simple answer.
The Ural Mountains.
The Andes mountain range is created by Pacific Plate diving under the South American Plate. The lighter materials on the subducting plate are easily melted, and thus create the volcanic chain that is the Andes.
Ural Mountains
Ural Mountains.
A mountain chain is called a mountain chain.
It is called a convergent boundary and can often result in a chain of mountains. When two plates converge, it is common for the denser plate to sink underneath the other. This process is called subduction.