A transform boundary does not destroy or create crust. Instead, it occurs where two tectonic plates slide past each other horizontally. This lateral movement can lead to earthquakes but does not involve the formation of new material or the destruction of existing crust. Examples include the San Andreas Fault in California.
Transform boundary.
Convergent boundary.
Convergent boundary.
d
divergent plate boundary
transform boundary
Transform boundary.
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.
A crust is not destroyed at a divergent boundary, where tectonic plates move away from each other. This movement creates new crust as magma rises to the surface and solidifies.
Convergent boundary.
Convergent boundary.
Transform boundary.
This would be called a Spreading center, or a divergent plate boundary.
d
The Galapagos Rift is a divergent plate boundary, where tectonic plates are moving apart. This movement creates a gap that allows magma to rise from the mantle, forming new oceanic crust.
divergent plate boundary
A divergent plate boundary creates a mid-ocean ridge. This occurs when two tectonic plates move away from each other, leading to the upwelling of magma from the mantle, creating new oceanic crust at the mid-ocean ridge.