It is a transform boundary.
San Francisco lies on the boundary between the Pacific Plate and the North American Plate, known as the San Andreas Fault. This boundary is a transform plate boundary, where the plates slide horizontally past each other.
Yes, a continental and oceanic plate can have a transform boundary. This occurs when the two plates slide past each other horizontally, causing earthquakes along the boundary. The San Andreas Fault in California is an example of a transform boundary between the North American Plate (continental) and Pacific Plate (oceanic).
For the most part, the boundary between the North American and Pacific Plates is a transform boundary, where two plates are sliding and grinding past each other. by pm of 10 d 33
Transform boundary / conservative boundary.
A transform boundary.
It is a transform boundary.
San Francisco lies on the boundary between the Pacific Plate and the North American Plate, known as the San Andreas Fault. This boundary is a transform plate boundary, where the plates slide horizontally past each other.
Yes, a continental and oceanic plate can have a transform boundary. This occurs when the two plates slide past each other horizontally, causing earthquakes along the boundary. The San Andreas Fault in California is an example of a transform boundary between the North American Plate (continental) and Pacific Plate (oceanic).
For the most part, the boundary between the North American and Pacific Plates is a transform boundary, where two plates are sliding and grinding past each other. by pm of 10 d 33
Transform boundary / conservative boundary.
San Francisco is located on the boundary between the Pacific Plate and the North American Plate, known as the San Andreas Fault. This is a transform plate boundary, where the two plates are sliding past each other horizontally.
The North American and Pacific Plate boundary is an example of a convergent plate boundary, specifically an oceanic to continental convergent plate boundary.
San Francisco is located on the boundary of the Pacific Plate and the North American Plate, along the San Andreas Fault. This boundary is a transform plate boundary, characterized by lateral movement between the two plates.
The boundary between the Pacific Plate and the North American Plate is a transform boundary. At this boundary, the plates slide past each other horizontally, causing frequent earthquakes along the boundary. This boundary is known as the San Andreas Fault.
California is the U.S. state that has a transform boundary, specifically along the San Andreas Fault. This boundary is responsible for the lateral sliding motion between the Pacific Plate and the North American Plate, which leads to earthquakes in the region.
The name of the transform boundary that separates the Pacific Plate and the North American Plate is known as the San Andreas Fault. It is the site of many of the earthquakes that plague Southern California.