COMPRESSION
The force that pulls apart the crust is called tensional or extensional tectonic stress, which occurs at divergent plate boundaries where tectonic plates move away from each other. This pulling force can lead to the formation of rift valleys and mid-ocean ridges.
The force that pushes rock upward is typically uplift caused by tectonic plate movements. This can occur when tectonic plates collide, causing one plate to be pushed up over the other, or when magma rises towards the surface, creating pressure that lifts the overlying rock.
gravity is a force that pulls object toward each other
Gravity is the natural force that causes objects to move toward each other. This force is a fundamental property of matter that attracts all objects with mass toward each other.
When two tectonic plates collide, one plate is typically forced beneath the other in a process known as subduction. The force of this collision can cause the crust to fold and buckle, leading to the formation of large mountain ranges. An example of this is the Himalayas, which were formed by the collision of the Indian and Eurasian plates.
When plates slide past each other, move toward each other, and move away from each other.
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Friction
A tectonic plate boundary is a region where two tectonic plates meet. These boundaries can be convergent (plates move towards each other), divergent (plates move away from each other), or transform (plates slide past each other horizontally). The interactions at these boundaries are responsible for earthquakes, volcanic activity, and the formation of 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 three main types of tectonic plate boundaries are convergent boundaries, where plates move toward each other; divergent boundaries, where plates move away from each other; and transform boundaries, where plates slide past each other horizontally.
When tectonic plates converge, they can form various geological features such as mountain ranges, deep ocean trenches, and volcanoes. This convergent boundary can result in one plate being pushed beneath the other in a process known as subduction.
if you are talking about earthquakes then its all about tectonic plates. The force of two plates get to much so one of the plates slide under the other forming an earthquake.
shifting tectonic plates cause continents to move a few inches every year. also, if the plates start rubbing against each other, they can cause severe earthquakes. plates hitting and pushing toward each other can form mountains or volcanoes.
A mountain range is likely to form where two tectonic plates push toward each other, a process known as convergent boundary. The collision between the plates can cause crustal uplift and compression, leading to the formation of mountain ranges through folding and faulting of the Earth's crust.
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Yes, tectonic plates can generate friction as they interact with each other along their boundaries. This friction can lead to the plates being locked together for a period of time before eventually releasing in the form of an earthquake.