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.
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. :)
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.
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.
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.
The collision between the Pacific Oceanic Plate and the North American Continental plate can cause earthquakes in Alaska.
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. :)
That is one method of mountain formation, yes.
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.
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.
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.
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.
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.
The Himalayas are among the youngest mountain ranges on the planet and consist mostly of uplifted sedimentary and metamorphic rock. According to the modern theory of plate tectonics, their formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate. The Arakan Yoma highlands in Myanmar and the Andaman and Nicobar Islands in the Bay of Bengal were also formed as a result of this collision.
According to the modern theory of plate tectonics, their formation is a result of a continental collision along the boundary between the Indo-Australian Plate and the Eurasian Plate. This is known as a fold mountain.
earthquake