compression
When two plates move towards each other, it is called convergence. The motion during convergence is usually called subduction if one plate is forced beneath the other, or collision if the two plates collide and form mountain ranges.
The three types of Earth's plates are convergent plates, where two plates move towards each other; divergent plates, where two plates move away from each other; and transform plates, where two plates slide past each other horizontally.
they are formed when two plates move towards each othe and crash
Divergent Boundaries happen when two plates (oceanic or contental) begin to diverge, or move apart. Convergent Boundaries occur when two plates (again, oceanic or contential) begin to converge or move apart
This is called a convergent boundary, because the two plates are converging, or coming together.
Convergent and divergent boundaries are terms used in plate tectonics to describe the juncture at two plates and how they move in relation to each other. Divergent plates move apart and convergent move towards each other.
Convergent and divergent boundaries are terms used in plate tectonics to describe the juncture at two plates and how they move in relation to each other. Divergent plates move apart and convergent move towards each other.
When two plates next to each other move, they may move at the same time -- for example, if one plate is sliding over another, the other plate could be tilting or sinking. What's more likely to happen, though, is that the pressure will cause one of the plates to break or shift at a weak point -- a fault, for example. So a piece of the plate may move, while most of it doesn't.
A convergent boundary can form between two plates and a divergent boundary can be created between two plates, then two plates rubbing together create earthquakes, many are very minor. A convergent boundary is two plates pushing together to form a mountain, hill, or volcano. Divergent plates move apart and create canyons and stuff.
Earthquakes are caused by two plates getting hung up, or locked in place. The tremors that follow are the usual forces that move the tectonic plates.
When two tectonic plates move towards one another, they typically result in phenomena such as mountain building, earthquakes, and subduction zones. However, the formation of mid-ocean ridges is NOT a result of this movement; rather, it occurs at divergent boundaries where plates move apart from each other, allowing magma to rise and create new oceanic crust.
When tectonic plates move apart, it creates a divergent boundary. As the plates separate, magma from beneath the Earth's surface can rise up, creating new crust. This process can lead to the formation of volcanic activity and mid-ocean ridges.