Niether. At a transform boundary, plates slide past each other, and crust is conserved.
Crust is neither formed nor destroyed at transform plate boundaries. At these boundaries, tectonic plates slide past each other horizontally, resulting in earthquakes and faults but no new crust is created or destroyed.
Along a transform boundary, crust is neither destroyed nor formed. Instead, tectonic plates slide past each other horizontally, causing earthquakes.
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 conservative boundary, also known as a transform boundary, is where crust is neither created nor destroyed. This type of boundary occurs when two tectonic plates slide past each other horizontally.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.
Crust is neither formed nor destroyed at transform plate boundaries. At these boundaries, tectonic plates slide past each other horizontally, resulting in earthquakes and faults but no new crust is created or destroyed.
Along a transform boundary, crust is neither destroyed nor formed. Instead, tectonic plates slide past each other horizontally, causing earthquakes.
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.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
california
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.
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.
A conservative boundary, also known as a transform boundary, is where crust is neither created nor destroyed. This type of boundary occurs when two tectonic plates slide past each other horizontally.
The boundary where the Earth's crust is neither created nor destroyed is known as a conservative plate boundary. At these boundaries, tectonic plates slide past each other horizontally without forming or destroying crust. This type of boundary is associated with transform faults.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.