Also called transform faults, strike-slip faults involve a movement that is horizontal with a block of rock on one side of the fault moving in one direction, the other block of rock moving in the other direction.
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strike-slip faults move along each other from shearing
Lateral Movement occurs along strike-slip fault.
move sideways past each other
techtonic
Two land masses move toward each other
a. Transform:transform boundaries or motion creates strike-slip faults.b. Convergent:convergent boundaries or motion creates reverse faults.c. Divergent:divergent motion creates a normal fault.
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
plate tecteconics
A fracture in the Earth's crust (with associated transverse or strike slip movement - similar to the San Andreas fault) that runs through the north of the country of Turkey, separating Eurasian plate and the Anatolian plate. It is associated with modern earthquakes, the loci of which which are gradually moving westwards towards Istanbul.
The strike-slip fault caused by the Pacific plate grinding against the North American plate.
No, the Pacific Plate and the North American Plate, and its motion is right-lateral strike-slip (horizontal).
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 actually a "Strike-Slip" fault, which means that the movement of the plates is a side-to-side movement past each other. The Pacific plate, relatively speaking, is moving north and the North American plate is moving south. This means that the very western coast of California is sliding north past the rest of California. The San Andreas fault is a strike-slip fault
The answer is by convergent plate motion.
A Transform fault where one tectonic plate slides past another tectonic plate results with rocks being pulled apart. Slippage results when the rock of one plate bends the rock of another, causing elastic rebounds and the release of energy as surface waves.
The San Andreas Fault is a continental transform boundary that extends roughly 810 miles (1,300 km) through California, forming the tectonic boundary between the Pacific Plate and the North American Plate. Its motion is right-lateral strike-slip (horizontal).
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.
a. Transform:transform boundaries or motion creates strike-slip faults.b. Convergent:convergent boundaries or motion creates reverse faults.c. Divergent:divergent motion creates a normal fault.
strike-slip
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.
The San Andreas Fault is a continental transform boundary that extends roughly 810 miles (1,300 km) through California, forming the tectonic boundary between the Pacific Plate and the North American Plate. Its motion is right-lateral strike-slip (horizontal).
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