They are called convergent boundaries and they come together with such force that they shoot up to make it.
The most substantial will be from crustal folding at a collision boundary between two continental plates. An example is the Himalayas which have been pushed up in Asia by the collision of the Indian Plate. The Rocky Mountains of North America were similarly formed by shallow subduction of the Farallon and Kula oceanic plates.
Deflation results in the formation of desert pavement.
When two continental plates converge, it results in formation of high mountains such as the Himalayan mountain.
Quartize
Folded mountains are the result of compression stress in the earth's crust. This is a movement of plates that presses together or squeezes Earth's crust and is also known as convergent boundary.
Compression.
Compression.
The most substantial will be from crustal folding at a collision boundary between two continental plates. An example is the Himalayas which have been pushed up in Asia by the collision of the Indian Plate. The Rocky Mountains of North America were similarly formed by shallow subduction of the Farallon and Kula oceanic plates.
When plates with edges which have ocean lithosphere collide with each other, one plate can be pushed under the other, causing the magma from the mantle to rise. This results in the formation volcanic mountains in the vicinity.
When plates with edges which have ocean lithosphere collide with each other, one plate can be pushed under the other, causing the magma from the mantle to rise. This results in the formation volcanic mountains in the vicinity.
When plates with edges which have ocean lithosphere collide with each other, one plate can be pushed under the other, causing the magma from the mantle to rise. This results in the formation volcanic mountains in the vicinity.
Meiosis results in the formation of what?
Deflation results in the formation of desert pavement.
The process of meiosis never results in the formation of a Diploid.
Stimulation of the reticular formation results in increased consciousness.
Continental and island arc volcanic chains are due to the collision of tectonic plates and the subduction of the more dense plate under the lighter, less dense plate. The resultant melting of the subducted crust as it reaches the mantle results in volcanism as the lighter, melted rock attempts to rise to the surface.
When two continental plates converge, it results in formation of high mountains such as the Himalayan mountain.