Metamorphism of existing rock through collisions of continental plates occurs from directional pressures along with heat from friction and depth of burial. The pressure and heat can cause recrystallization of existing minerals, new mineral crystal formation, and mineral realignment in the metamorphosed rock.
Well if you take into acount that metamorphic rock is formed by applying heat and pressure to sedimentary rock the answer becomes quite clear; the pressure is created by the tectonic plates colliding and the heat source is from the molten rock that is pushed close to the surface due to the collision. :)
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.
Mineral components of the rock being metamorphosed can be squeezed into bands or layers exhibiting a characteristic known as foliation. Minerals can recrystallize from the heat and pressure. New minerals can form from the reduction in fluids due to compression.
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.
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.
its funny because im looking for that answer too ._.
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.
Well if you take into acount that metamorphic rock is formed by applying heat and pressure to sedimentary rock the answer becomes quite clear; the pressure is created by the tectonic plates colliding and the heat source is from the molten rock that is pushed close to the surface due to the collision. :)
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.
That is one method of mountain formation, yes.
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.
When continents collide, it is called continental collision. This process results in the formation of mountain ranges and can also lead to seismic activity and the creation of fault lines. Examples of continental collisions include the collision between the Indian Plate and the Eurasian Plate, which gave rise to the formation of the Himalayas.
Mineral components of the rock being metamorphosed can be squeezed into bands or layers exhibiting a characteristic known as foliation. Minerals can recrystallize from the heat and pressure. New minerals can form from the reduction in fluids due to compression.
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 range is one of the youngest mountain ranges on the planet and consists mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, its formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate.
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 collision of two tectonic plates can lead to the formation of various geological features, depending on the types of plates involved. When two continental plates converge, they can create mountain ranges, such as the Himalayas. If an oceanic plate collides with a continental plate, subduction occurs, leading to the formation of deep ocean trenches and volcanic arcs. Additionally, the collision can result in earthquakes due to the immense stress and friction between the plates.