earthquakes indicate both convergent,divergent and transform fault plate boundaries
Convergent
stomer
transform boundary
subbduction zones
it is on a convergent plate boundary also known as a subduction zone
The boundary off the coast of Chile where the 8.8 earthquake occurred is a convergent boundary, specifically a subduction zone where the Nazca Plate is being pushed beneath the South American Plate. This type of boundary is associated with intense seismic activity and can result in powerful earthquakes.
The Kansu earthquake took place on the Weihe Basin fault, not on a plate boundary. The Weihe Basin is a normal dip-slip fault.
At a convergent boundary between oceanic and continental crust where subduction is occurring.
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 Kashmir earthquake of 2005 occurred along the convergent boundary between the Indian Plate and the Eurasian Plate. This boundary is characterized by the collision of the two plates, leading to intense seismic activity and the uplift of the Himalayas.
The Morocco earthquake was caused by the movement of the African Plate colliding with the Eurasian Plate along a convergent boundary. This collision resulted in the uplift of the Atlas Mountains and the seismic activity in the region.
It forms a convergent boundary with the South American Plate, divergent.