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What type of plate boundary does an earthquake occur at?

stomer


What type of margin did the Haiti earthquake occur at?

Transform boundary


At what type of boundary did the 1960 Chilean earthquake occur?

At a convergent boundary between oceanic and continental crust where subduction is occurring.


What type of boundary was the earthquake of Chile 1960?

convergent boundary


What type of plate boundary caused the Chile earthquake in 1960?

transform boundary


What type of plate boundary was the Andreanof earthquake?

Convergent


What type of boundary did the Haiti earthquake occur at?

The Haiti earthquake that occurred in 2010 was a result of a strike-slip boundary where the North American Plate and Caribbean Plate slid past each other horizontally along the Enriquillo-Plantain Garden fault zone.


What is a boundary of an earthquake?

The boundary of an earthquake refers to the area where two tectonic plates meet and release built-up stress in the form of seismic activity. This boundary can be a subduction zone, a transform fault, or a collision zone, depending on the type of plate interaction. Earthquakes often occur along these boundaries due to the movement and interaction of the tectonic plates.


Will a mega earthquake hit Britain?

No. "Mega earthquakes" sometimes known as megathrust earthquakes tend to occur at or near convergent plate boundaries. The UK is not located near to a convergent (or any other type of plate boundary) so will not experience an earthquake of this type.


What is the relationship between earthquake depth and type of plate boundary?

subbduction zones


What type of plate boundary caused earthquake in Haiti?

The earthquake in Haiti was caused by a strike-slip fault along the boundary between the Caribbean Plate and the North American Plate. Strike-slip faults occur when two plates slide past each other horizontally, causing seismic activity.


What type of plate boundary was involved in earthquake kansu?

The Kansu earthquake took place on the Weihe Basin fault, not on a plate boundary. The Weihe Basin is a normal dip-slip fault.