It is on a transform fault boundary.
The San Andreas Fault was created by a transform boundary, where two tectonic plates slide horizontally past each other. In the case of the San Andreas Fault, the Pacific Plate is moving northwest relative to the North American Plate.
The San Andreas fault is not connected to the North American or Pacific Plates but is merely the boundary between the two where they make contact. As such, it is a fault as well as a plate boundary.
The San Andreas Fault is not a mountain range. It is actually a transform fault boundary between the Pacific Plate and the North American Plate. The other land features that can be associated with the fault include valleys, canyons, and hills.
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 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.
Yes, San Francisco lies near the boundary between the Pacific Plate and the North American Plate. This tectonic boundary is known as the San Andreas Fault, which is a transform fault boundary.
A transform boundary.
A transform boundary.
The San Andreas Fault was created by a transform boundary, where two tectonic plates slide horizontally past each other. In the case of the San Andreas Fault, the Pacific Plate is moving northwest relative to the North American Plate.
The San Andreas fault is a transform plate boundary.
Transform boundary / conservative boundary.
The San Andreas fault is not connected to the North American or Pacific Plates but is merely the boundary between the two where they make contact. As such, it is a fault as well as a plate boundary.
The San Andreas Fault is not a mountain range. It is actually a transform fault boundary between the Pacific Plate and the North American Plate. The other land features that can be associated with the fault include valleys, canyons, and hills.
The San Andreas Fault is part of a transform plate boundary.
Along the San Andreas Fault line.
An example of a divergent plate boundary is the Mid-Atlantic Ridge, where the Eurasian Plate and North American Plate are moving apart. An example of a transform plate boundary is the San Andreas Fault in California, where the Pacific Plate and North American Plate are sliding past each other horizontally.