No crust is created when a transform boundary pulls away from each other.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Transform boundary.
The boundary that neither creates nor destroys oceanic crust is a transform boundary. At these boundaries, tectonic plates slide past each other horizontally, which can lead to earthquakes but does not result in the formation or destruction of crust. An example of a transform boundary is the San Andreas Fault in California.
The boundary where crust is neither destroyed nor formed is called a transform boundary. At transform boundaries, tectonic plates slide past one another horizontally, leading to significant friction and earthquakes. An example of this type of boundary is the San Andreas Fault in California. These boundaries are characterized by lateral movement rather than the creation or subduction of crust.
No crust is created when a transform boundary pulls away from each other.
No crust is created when a transform boundary pulls away from each other.
transform boundary
Transform boundary.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Transform boundary.
Niether. At a transform boundary, plates slide past each other, and crust is conserved.
A transform plate boundary does not create or destroy crust. Instead, adjacent plates slide horizontally past each other. This movement can cause earthquakes along the boundary without significantly changing the amount of crust.
its called a transform boundary
Crust is neither created nor destroyed along a transform boundary. Transform boundaries are characterized by horizontal displacement of crustal blocks, where tectonic plates slide past each other. This movement does not involve the production or destruction of crust, but rather leads to earthquakes due to the friction and stress along the boundary.
A strike-slip fault generally occurs at a transform boundary
The boundary where crust is neither destroyed nor formed is called a transform boundary. At transform boundaries, tectonic plates slide past one another horizontally, leading to significant friction and earthquakes. An example of this type of boundary is the San Andreas Fault in California. These boundaries are characterized by lateral movement rather than the creation or subduction of crust.