This is called a convergent boundary. A divergent boundary is when plate move away from each other, and a transform boundary is when plates slide past each other.
When two plate boundaries are moving toward each other, it is called a convergent boundary. This can lead to subduction, where one plate is forced beneath the other, or collision, where the two plates create mountain ranges.
When crustal plates move toward each other, they can form convergent boundaries where one plate is forced beneath the other in a process called subduction. This can result in the formation of mountain ranges, deep ocean trenches, and volcanic activity in the area.
The fault between two plates moving sideways past each other is called a transform fault. This type of fault occurs at transform boundaries where tectonic plates slide horizontally past each other.
The places where tectonic plates meet are called plate boundaries. There are three main types of plate boundaries: convergent boundaries (plates moving towards each other), divergent boundaries (plates moving away from each other), and transform boundaries (plates sliding past each other).
called tectonic plates. These plates can move in different directions, either colliding, moving apart, or sliding past each other. Their movement is responsible for phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges.
all volcanoes are caused by the earths plates moving toward each other and that is called convergent boundaries.
This is called a convergent boundary. A divergent boundary is when plate move away from each other, and a transform boundary is when plates slide past each other.
Most volcanoes on land are caused by the Earth's plates moving toward each other, a process known as convergent plate boundary. When two plates converge, the denser oceanic plate subducts beneath the less dense continental plate, leading to the formation of volcanoes along the subduction zone.
Convergent boundaries (plates moving toward each other, also called destructive boundaries), divergent boundaries (plates moving away from each other (sometimes called constructive boundaries), fault lines (sideways movement).
They are the contact points between plates that are moving toward each other.
When two plate boundaries are moving toward each other, it is called a convergent boundary. This can lead to subduction, where one plate is forced beneath the other, or collision, where the two plates create mountain ranges.
Plates that move toasted each other are detractive plates meeting at a destructive margin. If a continental and an oceanic plate move towards each other, earthquakes and volcanoes occur, this is called a subduction margin, but if the plates are both continental then fold mountains form this is a collision margin
When continental plates move toward each other, it is called a convergent plate boundary. This can lead to the collision and subduction of the plates, causing mountain building and deep ocean trench formation.
This is called a divergent plate boundary.
When crustal plates move toward each other, they can form convergent boundaries where one plate is forced beneath the other in a process called subduction. This can result in the formation of mountain ranges, deep ocean trenches, and volcanic activity in the area.
The fault between two plates moving sideways past each other is called a transform fault. This type of fault occurs at transform boundaries where tectonic plates slide horizontally past each other.
When two plates move away from each other it is called a divergent plate boundary because they are dividing.