The force behind tectonic plates coming together is typically caused by the process of subduction, where one plate is forced beneath another due to differences in density and composition. This subduction zone creates a convergent boundary, leading to the collision and eventual uplift of the Earth's crust.
The earth's plates move in all directions: up, down, and sideways. That's why we have mountains and subsidances and earthquakes and volcanoes and all sorts of stuff!
Volcanoes are created by the movement of tectonic plates on the Earth's surface. When two tectonic plates collide or move apart, magma from the mantle rises to the surface, eventually erupting through a volcano. Additionally, hotspots, subduction zones, and rift zones can also contribute to the formation of volcanoes.
Earthquakes and volcano activity occurs at the boundaries or edges of the tectonic plates.
seismic plates, or tectonic plates, are huge 'plates' of rocks that exist beneath the earth's surface that rest upon molten rock. It is on the borders of these plates that 'fault lines' occur and these are hotspots of volcanic and seismic activity such as earthquakes.
Tectonic movement. The outer crust of the Earth is made up of huge masses called plates. These plates are actually floating on the molten rock (magma) underneath them. (Magma is the stuff that spews out of erupting volcanoes) When tectonic plates temporarily get stuck against eachother and then suddenly release, we experience an earthquake.
Earth's tectonic plates move due to the heat-driven convective flow of mantle material beneath them. This process creates forces that push and pull the plates, causing them to move around the Earth's surface.
The earth's plates move in all directions: up, down, and sideways. That's why we have mountains and subsidances and earthquakes and volcanoes and all sorts of stuff!
Convection currents in the mantle cause the movement of tectonic plates. Heat from the Earth's core creates rising currents of molten mantle material, which pushes the plates apart at mid-ocean ridges. As the plates cool, they sink back into the mantle at subduction zones, completing the cycle of plate movement driven by convection currents.
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.
Volcanoes are created by the movement of tectonic plates on the Earth's surface. When two tectonic plates collide or move apart, magma from the mantle rises to the surface, eventually erupting through a volcano. Additionally, hotspots, subduction zones, and rift zones can also contribute to the formation of volcanoes.
They are plates, and they move around, and they shake and stuff.
Together the crust and upper mantle are called the lithosphere and they extend about 80 km deep. The lithosphere is broken into giant plates that fit around the globe like puzzle pieces.
if they mess with somebody like pushes them and that kind of stuff
It pushes stuff, when someone passes right beside you running, wind will push you. It doesn't really push you but that is how you feel the cold wind. So it pushes stuff when you push them lol
Earthquakes and volcano activity occurs at the boundaries or edges of the tectonic plates.
seismic plates, or tectonic plates, are huge 'plates' of rocks that exist beneath the earth's surface that rest upon molten rock. It is on the borders of these plates that 'fault lines' occur and these are hotspots of volcanic and seismic activity such as earthquakes.
The ground you are standing on, i.e. the surface of a planet.