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.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
No, subduction zones are where tectonic plates collide and one plate is forced beneath the other. New crust is formed at divergent plate boundaries, where plates move apart and magma rises to create new crust.
recessive plate boundary
New crust is not formed at conservative plate boundaries. Instead, these boundaries involve plates sliding past each other horizontally without any creation or destruction of crust. This movement can cause earthquakes as the plates interact.
At convergent boundaries are boundaries the crust is destroyed by subduction of oceanic crust underneath continental crust or other oceanic crust.
it's neither created or destroyed
its true
No, this statement is not accurate. Along a sliding boundary, called a transform boundary, the crust is neither created nor destroyed. Instead, the crust is transformed horizontally as two tectonic plates slide past each other.
Along a transform boundary, crust is neither destroyed nor formed. Instead, tectonic plates slide past each other horizontally, causing earthquakes.
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.
New crust is formed at a divergent boundary
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Crust is neither formed nor destroyed when the rate of crust formation at mid-ocean ridges equals the rate of crust destruction at subduction zones. This balance is known as isostasy and helps maintain the overall thickness of the Earth's crust.
No, subduction zones are where tectonic plates collide and one plate is forced beneath the other. New crust is formed at divergent plate boundaries, where plates move apart and magma rises to create new crust.
recessive plate boundary