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 definition of ocean continental collision means the continental crust and the ocean's crust collide with one another. A subduction is formed when the collision occurs.
A continental plate is colliding with another continental plate, causing upward motion. A lithospheric plate is colliding with another lithospheric plate of similar bouyancy, causing upward motion.
An example of a continental to continental crust collision is the collision between the Indian Plate and the Eurasian Plate that led to the formation of the Himalayan mountain range. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
The oceanic plate is forced beneath the continental plate in a process called subduction. This collision can lead to the formation of deep oceanic trenches, volcanic arcs, and earthquakes due to the intense pressure and friction between the two plates.
The Himalayan Mountains were formed as a result of the collision between the Indian and Eurasian tectonic plates. This collision forced the Earth's crust to crumple and uplift, creating the massive mountain range that continues to grow taller each year.
The definition of ocean continental collision means the continental crust and the ocean's crust collide with one another. A subduction is formed when the collision occurs.
The collision between the Indian Plate and the Eurasian Plate that led to the formation of the Himalayas is a geographic example of a continental collision. This collision continues to uplift the Himalayas, creating some of the world's tallest mountains.
An example of a continental-continental plate convergence is the collision boundary between the Indian Plate and the Eurasian Plate that formed the Himalayas. The convergence between these two plates has led to the uplift of the Himalayan mountain range over millions of years due to the ongoing collision between the two continental plates.
A continental plate is colliding with another continental plate, causing upward motion. A lithospheric plate is colliding with another lithospheric plate of similar bouyancy, causing upward motion.
earthquake
An example of a continental to continental crust collision is the collision between the Indian Plate and the Eurasian Plate that led to the formation of the Himalayan mountain range. This collision is ongoing and has resulted in the uplift of the Himalayas and the Tibetan Plateau.
The oceanic plate is forced beneath the continental plate in a process called subduction. This collision can lead to the formation of deep oceanic trenches, volcanic arcs, and earthquakes due to the intense pressure and friction between the two plates.
A continent-continent collision occurs when two continental plates converge and push against each other. This collision can lead to mountain building, as seen in the collision between the Indian Plate and the Eurasian Plate that formed the Himalayas.
its funny because im looking for that answer too ._.
The collision of an oceanic plate with a continental plate typically results in subduction, where the denser oceanic plate sinks beneath the continental plate, creating features like deep ocean trenches and volcanic arcs. In contrast, the collision of two continental plates leads to the formation of mountain ranges due to the compression and buckling of the crust, as neither plate is subducted easily. This process can create significant geological activity, such as earthquakes, but generally lacks the volcanic activity associated with oceanic-continental collisions.
That is one method of mountain formation, yes.
This process is called continental collision, and it typically results in the formation of mountain ranges. When two continental plates converge, neither plate is subducted due to their buoyancy, leading to the uplift of the crust. This phenomenon is exemplified by the collision between the Indian and Eurasian plates, which created the Himalayas.