The San Andreas Fault is a transform plate boundary.
The San Andreas fault is a transform boundary, where two tectonic plates slide past each other horizontally. In this case, the Pacific Plate and the North American Plate are moving in opposite directions, causing frequent tremors and earthquakes.
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.
Large faults such as the San Andreas are transform faults and are found throughout the state but moreso in the central and southern regions. Slip-strike faults exist between the inland mountains and the coast. Minor earthquakes occur almost constantly along these faults.San Andreas.
The San Andreas Fault is a strike-slip fault, where two tectonic plates move horizontally past each other. The main force causing movement along the fault is the tectonic forces generated by the motion of the Pacific Plate relative to the North American Plate.
The San Andreas Fault is an example of a transform boundary in which plates slide past each other. This type of fault may also be known as a strike slip fault. During this plate motion, lithosphere is neither created nor destroyed. Shear stress causes the undeformed block of rock to experience tearing and smearing.
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.
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 transform boundary, where two tectonic plates slide past each other horizontally. In this case, the Pacific Plate and the North American Plate are moving in opposite directions, causing frequent tremors and earthquakes.
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 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.
Large faults such as the San Andreas are transform faults and are found throughout the state but moreso in the central and southern regions. Slip-strike faults exist between the inland mountains and the coast. Minor earthquakes occur almost constantly along these faults.San Andreas.
The San Andreas Fault is a strike-slip fault, where two tectonic plates move horizontally past each other. The main force causing movement along the fault is the tectonic forces generated by the motion of the Pacific Plate relative to the North American Plate.
Reverse
The San Andreas Fault is an example of a transform boundary in which plates slide past each other. This type of fault may also be known as a strike slip fault. During this plate motion, lithosphere is neither created nor destroyed. Shear stress causes the undeformed block of rock to experience tearing and smearing.
The San Andreas fault is a transform boundary, where two tectonic plates slide past each other horizontally. In this case, the Pacific Plate and the North American Plate are moving in opposite directions, causing frequent earthquakes along the fault line.
That is a Strike-slip fault. This type of plate boundary is a relatively conservative boundary because the plates moves side by side horizontally causing little or no destruction of old plates or creation of new plates, but only causes a kind of boundary known as a Transform Boundary. An example of a transform boundary is the San Andreas fault, in California, USA North America.