Strike-Slip faults are found at transform boundaries because strike slip faults push and pull on opposing forces HORIZONTALLY exactly like a transform boundary.
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.
Yes, for example the San Andreas Fault is a plate boundary.
The plate boundary the Chile earthquake occurred on in 2010 was the converging boundary. A converging boundary is when two plates move closer together. In this case the converging boundary moved so close together that the plates hut one another. They then subducted under on another and the earthquake was formed.
If the fault is responsible for the earthquake, there will be movement (displacement) along the fault.
Plate boundaries around Japan are convergent boundaries ie two plates are sliding towards each other. Japan has been formed as a result of the subduction of the Philippine Sea Plate beneath the continental Amurian Plate and Okinawa Plate to the south, and subduction of the Pacific Plate under the Okhotsk Plate to the north.
A certain type of strike-slip fault is found at a transform plate boundary.
actually it is not a plate boundary it is a fault a strike slip fault -les bois student014
Strike-Slip faults are found at transform boundaries because strike slip faults push and pull on opposing forces HORIZONTALLY exactly like a transform boundary.
The Dead Sea fault zone is located on a Transform boundary.
A strike-slip plate boundary is found near Haiti, specifically the boundary between the North American Plate and the Caribbean Plate. This boundary is associated with the Enriquillo-Plantain Garden fault system that runs through the region.
The North American and Pacific Plate boundary is an example of a convergent plate boundary, specifically an oceanic to continental convergent plate boundary.
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.
The San Andreas fault is a right-lateral (dextral) strike-slip fault which marks a transform (or sliding) boundary between the Pacific Plate and the North American Plate. In essence the plate boundary is destructive rather than constructive but at present the energy is directed at moving the Pacific Plate in a generally northerly direction, parallel with the coastline.
Yes, for example the San Andreas Fault is a plate boundary.
It is a right-lateral strike-slip fault
The San Andreas Fault is a strike-slip fault where the motion is mainly horizontal, with the two sides moving past each other horizontally. It is a transform boundary between the Pacific Plate and the North American Plate.
The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific plate are both moving vertically in different directions.