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earthquake
Not by temperature variations at Earth's surface, no. However, temperature variations in Earth's mantle play a role in plate tectonics, and so can affect earthquake activity.
it could cause an earthquake and a tsunami. or a volcano to be formed
No, the 2011 Japan earthquake was a megathrust earthquake, specifically a subduction zone earthquake. It occurred along the boundary between the Pacific Plate and the North American Plate, where the Pacific Plate is subducting beneath the North American Plate.
thee ceramic plate, and the metal plate :)
The Kamchatka earthquake was on the Pacific plate.
Where a tectonic plate slides past another.
earthquake
this is a destructive plate boundary. An earthquake and a vocano is created
Earthquake
An earthquake or if at sea a tsunami.
Tectonic plate size can have an influence on earthquake magnitude. Larger plates generally produce more powerful earthquakes due to the greater build-up of stress along plate boundaries. However, other factors like the type of plate boundary and the rate of plate movement also play a significant role in determining earthquake magnitude.
Internal convection in the Earth's mantle drives the movement of tectonic plates by creating forces that push or pull the plates. As material within the mantle heats up and cools down, it undergoes convection currents that can cause plates to move apart at mid-ocean ridges or collide at subduction zones. This convection process is a key factor in the driving force behind plate tectonics.
Not by temperature variations at Earth's surface, no. However, temperature variations in Earth's mantle play a role in plate tectonics, and so can affect earthquake activity.
well it's simple: an earthquake that can kill and destroy cars, trees, and buildings and they can cause tsunamies
it could cause an earthquake and a tsunami. or a volcano to be formed
The Kashmir earthquake in 2005 was caused by the movement of the Indian Plate colliding with the Eurasian Plate along the Himalayan boundary. This collision resulted in a sudden release of accumulated stress along a fault line, leading to the earthquake.