Typically the less dense continental plate would stay afloat while the denser oceanic plate would be submerged below. This can result in volcanic eruptions at the subduction zone due to oceanic crust undergoing increased pressure and temperatures as it descends below the continental crust.
The collision between the Pacific Oceanic Plate and the North American Continental plate can cause earthquakes in Alaska.
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Their formation is a result of a continental collision along the convergent boundary between the Indo-Australian plate and the Eurasian plate. This is referred to as a fold mountain.
In a convergent plate collision between continental and oceanic plates, the more dense oceanic plate would subduct, or move underneath, the less dense continental plate, eventually melting into the mantle at the leading edge.
When two Continental plates come together, they both collide.This forms mountains.
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its funny because im looking for that answer too ._.
That is one method of mountain formation, yes.
Yes, the Himalayas are located on a convergent boundary.There are three types of convergent boundaries:-Oceanic-Oceanic-Oceanic-Continental-Continental-ContinentalOf the three types, the Himalayas are considered to be Continental-Continental. Meaning, it's a collision between two continental plates.
The lithosphere includes the crust (oceanic and continental) and the uppermost part of the mantle. The lithospheric plates are thinnest at the ocean, varying from between a few kilometers to 100 kilometers in deep-ocean basins. The continental lithosphere, on the other hand, is generally about 100 to 250 kilometers thick. The most important feature of the lithosphere is its divisions into lithospheric plates. These plates move and collide, creating earthquakes, fault lines, etc.
The heavier/denser oceanic plate subducts the lighter, less - dense continental plate.
The collision between the Pacific Oceanic Plate and the North American Continental plate can cause earthquakes in Alaska.
The collision of contiental plate places rocks under enormous pressure, greater than can be produced from burial alone. This extreme pressure leads to high grades of metamorphism.
Usually subduction of the denser thinner oceanic crust under the lighter thicker continental crust. This also produces a row of volcanoes in the continental crust producing lava high in water content and resulting in explosive eruptions.
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Fold mountains are formed from the collision of continental tectonic plates. Since neither plate subducts under the other, the colliding plates wrinkle and fold like a rug being pushed into a wall.