No it was a destructive plate boundary.
The Izmit earthquake in 1999 occurred along a transform boundary, which is a type of conservative plate boundary. This earthquake resulted from the movement of the North Anatolian Fault, where the Eurasian Plate slides horizontally past the Anatolian Plate.
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.
A conservative plate boundary is where tectonic plates slide past each other horizontally without creating or destroying lithosphere. The movement can be in the same direction (transform fault) or in opposite directions (strike-slip fault) resulting in earthquakes.
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.
The 1755 Lisbon earthquake occurred at the boundary between the African Plate and the Eurasian Plate. This boundary is known as a convergent boundary, where the two plates are colliding, causing seismic activity.
No, it was a destructive plate boundry. :)
The Izmit earthquake in 1999 occurred along a transform boundary, which is a type of conservative plate boundary. This earthquake resulted from the movement of the North Anatolian Fault, where the Eurasian Plate slides horizontally past the Anatolian Plate.
Yes it is, due to the force of the plate sliding by each other.
a constructive plate boundary is where two plates move apart from eachother forming a gap which allows magma to rise and that leads to a earthquake.
Convergence plate boundary between the Eurasian Plate and the Indian Plate.
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.
transform boundary
A conservative plate boundary is where tectonic plates slide past each other horizontally without creating or destroying lithosphere. The movement can be in the same direction (transform fault) or in opposite directions (strike-slip fault) resulting in earthquakes.
Convergent
convergant
stomer
A transform fault boundary is a conservative plate boundary. This is what gets rid of lithosphere.