The San Andreas fault is a slip/strike fault. The plates touch but move on a roughly north/south axis. One demonstration of this movement is that the rock formation in currently present in Pinnacles National Monument (near King City, CA) is really one half of the original formation. The other half is 300 miles south near San Diego.
The San Andreas fault is where it occured.
When two plates grind side to side past each other, a transform plate boundary is formed. This type of boundary is characterized by horizontal movement along faults, such as the San Andreas Fault in California.
When plates slide past each other, it is called a transform boundary or a strike-slip boundary. This type of boundary is characterized by horizontal movement along fault lines, such as the San Andreas Fault in California.
San Andreas Fault. The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California. It forms the tectonic boundary between the Pacific Plate and the North American Plate, and its motion is right-lateral strike-slip (horizontal). By Donovan Lopez
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 San Andreas Fault in California is a transform boundary. It represents the boundary between the North American Plate and the Pacific Plate, where the plates slide horizontally past each other. This movement can cause earthquakes due to the built-up tension along the fault line.
The plate boundary that is found along the coast of California is the San Andreas fault system that runs in a northwest- southwest direction I think that's the answer
In plate tectonics, a sliding boundary is considered a transform fault where the two merging plates slide past each other in the opposite direction. A great example of a transform fault would be in California along the San Andreas fault line.
The San Andreas fault is where it occured.
Along the San Andreas Fault line.
When two plates grind side to side past each other, a transform plate boundary is formed. This type of boundary is characterized by horizontal movement along faults, such as the San Andreas Fault in California.
When plates slide past each other, it is called a transform boundary or a strike-slip boundary. This type of boundary is characterized by horizontal movement along fault lines, such as the San Andreas Fault in California.
San Andreas Fault. The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California. It forms the tectonic boundary between the Pacific Plate and the North American Plate, and its motion is right-lateral strike-slip (horizontal). By Donovan Lopez
The San Andreas Fault is associated with a transform plate boundary. It marks the boundary between the Pacific Plate and the North American Plate, where they are sliding past each other horizontally. This movement can cause earthquakes along the fault line.
The San Andreas fault is a tectonic boundary between the Pacific Plate and the North American Plate, where they slide past each other horizontally. This movement can cause earthquakes due to built-up stress being released along the fault line. The fault extends roughly 800 miles through California and is a prominent feature due to its significant seismic activity.
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.
When two tectonic plates slide past each other horizontally, the boundary between them is called a transform boundary. This type of boundary is characterized by lateral movement along fault lines, such as the San Andreas Fault in California.