If you are thinking of tectonic plates then there are more than two.
The Earth's crust is broken up into a large pieces, which are called plates. Two types of plates are oceanic and continental
I think that when two continental plates collide it's called a collision margin, the mountains that then form are called fold mountains :)
It is called subduction. When subduction occurs one plate slips beneath the other and sinks into the Earth's mantle and creates a trench.
The inside of a two dimensional shape is called the area.
A fault-block mountain forms where the edges of two plates come together to create a fault. When one plate pushes up over the other one, the upper one can continue up until it is high enough to create a fault-block mountain.
an earthquake
An earthquake.
The Earth's crust is broken up into a large pieces, which are called plates. Two types of plates are oceanic and continental
Plates
two tectonic plates colide
I think that when two continental plates collide it's called a collision margin, the mountains that then form are called fold mountains :)
Faults are actually the reason earthquakes start. A fault is two Techtonic Platesrubbing against each other, creating tension and stress. When thetension and stress overcomes the strength of the fault, the two plates slip/move,causing the ground to move in various ways, which is also called an earthquake.Techtonic Plates: plates made up of the earths crust that are moving along alayer of magma inside the earth,called the mantle.
Faults are actually the reason earthquakes start. A fault is two Techtonic Platesrubbing against each other, creating tension and stress. When thetension and stress overcomes the strength of the fault, the two plates slip/move,causing the ground to move in various ways, which is also called an earthquake.Techtonic Plates: plates made up of the earths crust that are moving along alayer of magma inside the earth,called the mantle.
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.
The place where two plates come together is called a "plate boundary." These boundaries can be classified as convergent, divergent, or transform based on how the plates are moving in relation to each other.
Continental Plates
The two main types of plates that make up the Earth's lithosphere are oceanic plates, which are denser and thinner, and continental plates, which are less dense and thicker. These plates interact with each other at their boundaries, causing movements such as subduction, spreading, and collisions that shape the Earth's surface.