The India plate crashing into the Asia plate caused the formation of the Himalayas. It can also cause subduction, when one plate is pushed beneath the other plate and so pushed back into the molten mantle.
One movement that tectonic plates do not experience is "oscillation." While tectonic plates primarily engage in movements such as convergence, divergence, and transform faulting, oscillation refers to a back-and-forth motion that is not characteristic of tectonic plate interactions. Instead, tectonic plates move in response to forces generated by the Earth's mantle and other geological processes.
In the mantle, there is a process called convection where hot material rises, cools, and then sinks back down. This circulating motion generates forces that cause the tectonic plates above to move. The heat from the Earth's core drives this convection process.
The movement of tectonic plates is primarily driven by the convective flow of molten rock in the upper mantle. This convection occurs due to the heat generated by the radioactive decay of elements within the Earth, which causes the molten rock to rise, cool, and then sink back down, creating a circular motion that drives the movement of tectonic plates.
When two tectonic plates rub back and forth, they create friction that can cause earthquakes. The pressure from the movement builds up until it is released suddenly, resulting in seismic waves that shake the Earth's surface. These earthquakes can vary in intensity depending on the amount of stress that has built up along the fault line.
The India plate crashing into the Asia plate caused the formation of the Himalayas. It can also cause subduction, when one plate is pushed beneath the other plate and so pushed back into the molten mantle.
The way tectonic plates move is by the heat from the core that goes up to the mantle which pushes up the rock and pushes them together to form tectonic plates. Later the tectonic plates slowly go back down until the heat of the core reaches the mantle once again.
One movement that tectonic plates do not experience is "oscillation." While tectonic plates primarily engage in movements such as convergence, divergence, and transform faulting, oscillation refers to a back-and-forth motion that is not characteristic of tectonic plate interactions. Instead, tectonic plates move in response to forces generated by the Earth's mantle and other geological processes.
Tectonic plates move as earthquakes exists. The crust shakes. As a result, the water goes down to the tectonic plates and comes back as big waves not exceeding 10-15 meters.
an earthquake happens
It was not called off, it was pushed back and defeated.
Because - the Earth's crust is forced back below the surface at the edges of the tectonic plates These areas are called subduction zones.
Stegosaurus???
In the mantle, there is a process called convection where hot material rises, cools, and then sinks back down. This circulating motion generates forces that cause the tectonic plates above to move. The heat from the Earth's core drives this convection process.
Harry Hess proposed that tectonic plates moved due to the process of seafloor spreading. He suggested that magma from the mantle rises at mid-ocean ridges, creating new oceanic crust. As this new crust forms, it pushes existing plates away from the ridge, causing them to move. This mechanism, combined with subduction where plates sink back into the mantle, explains the movement of tectonic plates.
The movement of tectonic plates is primarily driven by the convective flow of molten rock in the upper mantle. This convection occurs due to the heat generated by the radioactive decay of elements within the Earth, which causes the molten rock to rise, cool, and then sink back down, creating a circular motion that drives the movement of tectonic plates.
When two tectonic plates rub back and forth, they create friction that can cause earthquakes. The pressure from the movement builds up until it is released suddenly, resulting in seismic waves that shake the Earth's surface. These earthquakes can vary in intensity depending on the amount of stress that has built up along the fault line.