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.
A deep ocean trench is commonly formed at a plate boundary where oceanic crust converges with continental crust. The oceanic crust is denser and is forced beneath the lighter continental crust, creating a deep trench.
At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.
At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.
Transform boundary.
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.
A deep ocean trench is commonly formed at a plate boundary where oceanic crust converges with continental crust. The oceanic crust is denser and is forced beneath the lighter continental crust, creating a deep trench.
At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.
At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.
Niether. At a transform boundary, plates slide past each other, and crust is conserved.
A strike-slip fault generally occurs at a transform boundary
At a transform boundary, two portions of newly formed crust move laterally past each other due to the motion of tectonic plates. As magma rises at the mid-ocean ridge, it creates new oceanic crust, which then becomes offset by the transform fault. This lateral movement allows the sections of crust on either side of the transform boundary to shift in opposite directions, maintaining the overall process of seafloor spreading while accommodating the differences in plate movement. The transform boundary effectively acts as a conduit for the movement of crustal material between the segments of the ridge.
because the molten rock cools in the water and forms a oceanic crust
Convergent boundary.
oceanic crust