They lodge together pressure builds up and overcomes the friction
the plates jolt past each other and make earthquakes
this also creates ridges in the land eg san andreas fault
An earthquake happens then a fault line is made
The action of earth's crust buckling in wave-like patterns is due to two plates coming together or converging. These plates can be either oceanic or continental plates. Examples of these types of plates are the Eurasian, Pacific, Australian, Caribbean plates.
Tectonic plates are huge plates of rock covering the surface of the earth. They are very slowly moving, some moving together, some moving apart.Sometimes they have been pushing or pulling a bit without any movement until suddenly they give a jerk. That jerk is usually an earthquake.The natural disaster from the movement of tectonic plates is an earthquake, and if it's under the sea, then it might cause a tsunami.
The continents are part of Earth's outermost layer called the crust. The crust is divided into large plates, known as tectonic plates, which fit together like a jigsaw puzzle to form the Earth's surface.
When the plates slide past each other, it releases a shock wave, either a p-wave or an s-wave, and it spreads out in all directions. Sometimes it causes earthquakes.
earthquakes happen
An earthquake happens then a fault line is made
I pretty sure that is creates an earthquake.
the tectonics plates will stick together.
When tectonic plates, which is the scientific term for the plates on the Earth's crust, rub together, it causes an earthquake. Earthquakes happen everyday. We just don't feel them all.
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
The action of earth's crust buckling in wave-like patterns is due to two plates coming together or converging. These plates can be either oceanic or continental plates. Examples of these types of plates are the Eurasian, Pacific, Australian, Caribbean plates.
When two plates collide, or come together, the plates will push upward, forming a mountain. If one plate is continental crust and the other is oceanic crust, the less dense crust (this being the oceanic) will actually move under the more dense crust, in a process called subduction, to form a deep-ocean trench.
cracks in the plates which make up the crust. the earths crust is not connected. its made up of plates that moves and they are formed by plates pushing together then collapsing. they erupt when it gets a lot of friction from the plates pushing together
The crust is the layer at the surface that forms the upper part of the plates. The plates also include a portion of the upper mantle just beneath the crust. Together, the crust and this upper portion of the mantle form the lithosphere.
Tectonic plates are huge plates of rock covering the surface of the earth. They are very slowly moving, some moving together, some moving apart.Sometimes they have been pushing or pulling a bit without any movement until suddenly they give a jerk. That jerk is usually an earthquake.The natural disaster from the movement of tectonic plates is an earthquake, and if it's under the sea, then it might cause a tsunami.
When it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.