Mountains.
a plate boundary there are constructive plate boundaries, destructive plate boundaries, conservative plate boundaries and collision plate boundaries
There are three main types of plate tectonic boundaries: divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally. Each type of boundary has its own characteristic geologic features and tectonic activity.
It seems like there may have been a typo in your question. Did you mean plate boundaries? If so, plate boundaries are the lines where tectonic plates meet. There are three main types of plate boundaries: divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other.
When pieces of continental crust collide at a convergent boundary, it is called continental collision. This collision can result in the formation of mountain ranges, such as the Himalayas from the collision of the Indian Plate with the Eurasian Plate.
Mountains.
Mountains form along convergent boundaries when 2 plates collide. These are also called colliding boundaries.
a plate boundary there are constructive plate boundaries, destructive plate boundaries, conservative plate boundaries and collision plate boundaries
subduction boundary!!!
There are three main types of plate tectonic boundaries: divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally. Each type of boundary has its own characteristic geologic features and tectonic activity.
It seems like there may have been a typo in your question. Did you mean plate boundaries? If so, plate boundaries are the lines where tectonic plates meet. There are three main types of plate boundaries: divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other.
No. Not all plate boundaries are at the edges of continents, nor do all edges of continents correspond with plate boundaries. Many plate boundaries are found in the middle of oceans, while the continent of Africa is being torn apart by a developing plate boundary. Some edges of continents, such as the west coast of South America are near plate boundaries. These are called active continental margins. Others, such as the east coast of North America, are nowhere near plate boundaries. These are called passive continental margins.
Sea floor is destroyed at convergent boundaries where two tectonic plates collide. One plate is forced underneath the other in a process called subduction, leading to the destruction of the denser oceanic plate.
Its because the plate boundaries collide with eachother causing the earth to shake.
When pieces of continental crust collide at a convergent boundary, it is called continental collision. This collision can result in the formation of mountain ranges, such as the Himalayas from the collision of the Indian Plate with the Eurasian Plate.
The three types of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally.
No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.