Im pretty sure its ridge push, slab pull, and mantle convection
Tectonic plates move from east to west as a whole due to the coreolis (not sure of spelling) effect.
Earths crust is made of several large tectonic plates. These plates slowly move in three ways. 2 plates may move along side each other, away from each other or toward each other. if 2 plates of equal density collide it will result in rocks being crumpled upward forming mountains. if one plate has less density then the other then the plate with more density will slide beneath the less dense plate
Earthquakes are mostly found at the edges of plates because that is the area of which the plates collide in different ways resulting in earthquakes and volcanoes.
Earthquakes occur from tectonic plate movement, transform, divergent and convergent.KIDS ANSWER:Earthquakes happen by the plates of the world moving,these plates can move in three different ways. Transform which is when the simply slide past each other. There is also divergent and convergent divergent is when the plates don't like each other so they move away from each other, and convergent which is were the plates are mad at each other so they have a fight and go into each other.hope this helps!!!!!!!!!!from a year five school girl
The interaction areas between tectonic plates are called boundaries. There are three types of boundaries:Transform--where plates essentially grind past each other with no subduction.Convergent--where plates collide. Oceanic plate to oceanic plate convergence will result in the more dense plate subducting under the less dense plate.Divergent--where plates move apart. The major diverging plates are located at the mid-ocean ridge system where melting material from the asthenosphere fills in the separating plate zone, creating new crust.
Tectonic plates move from east to west as a whole due to the coreolis (not sure of spelling) effect.
When plates slide past each other, move toward each other, and move away from each other.
Tectonic plate interactions are of three different basic types: Divergent boundaries are areas where plates move away from each other, forming either mid-oceanic ridges or rift valleys. These are also known as constructive boundaries. Convergent boundaries are areas where plates move toward each other and collide.
Plates move through seafloor spreading, where new oceanic crust is created at mid-ocean ridges and pushes existing plates apart. Another way is through subduction, where one plate slides beneath another due to differences in density. Plates can also move horizontally past each other at transform boundaries.
Up, down, and sidewise.
Plates move along a fault through transform boundaries, where they slide past each other horizontally. Plates can also move through divergent boundaries, where they move away from each other. Lastly, plates can move along convergent boundaries, where they collide and push against each other, leading to subduction or mountain formation.
convergent boundaries: plates move together divergent boundaries: plates move apart transform boundaries: plates move against each other
the tectonic plates can cause earthquakes because they can move three different ways. there are some called divergent, convergent and transform. they can sometimes even do some subduction or even rise up that is also how mountains are made.
The interaction areas between tectonic plates are called boundaries. There are three types of boundaries:Transform--where plates essentially grind past each other with no subduction.Convergent--where plates collide. Oceanic plate to oceanic plate convergence will result in the more dense plate subducting under the less dense plate.Divergent--where plates move apart. The major diverging plates are located at the mid-ocean ridge system where melting material from the asthenosphere fills in the separating plate zone, creating new crust.
They slide, move towards and move away from each.
Tectonic plates move in various ways, one being through the process of subduction where one plate is forced beneath another. This movement can lead to volcanic activity, creating islands as magma rises to the surface and solidifies. Additionally, plates can also move apart at mid-ocean ridges, allowing magma to rise and form new land.
a faultis a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement along the fractures as a result of earth movement.the plates move at the faults becausestress builds up in rocks and when it reaches a level that exceeds the strain threshold it will move along the faults