The Divergent Boundaries.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Transform boundary.
A divergent plate boundary creates new land like the seafloor at the mid-Atlantic ridge. At these boundaries, tectonic plates move away from each other, allowing magma to rise up and solidify, forming new oceanic crust. As the crust cools and spreads outward, it creates new land in the form of the ocean floor.
A divergent boundary creates seafloor spreading. At these boundaries, tectonic plates move apart, allowing magma to rise from below the Earth's surface and create new crust at the mid-ocean ridges.
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.
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
Transform boundary.
It creates a divergent boundary.
creates new crust and allows magma to come through.
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.
A divergent plate boundary creates new land like the seafloor at the mid-Atlantic ridge. At these boundaries, tectonic plates move away from each other, allowing magma to rise up and solidify, forming new oceanic crust. As the crust cools and spreads outward, it creates new land in the form of the ocean floor.
A divergent boundary creates seafloor spreading. At these boundaries, tectonic plates move apart, allowing magma to rise from below the Earth's surface and create new crust at the mid-ocean ridges.
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.
New crust is being added to the other edge of the boundary
Crust can disappear at the edge of a boundary through subduction, where one tectonic plate is pushed beneath another. This process causes the crust to be pulled into the mantle and reabsorbed, leading to the disappearance of crust at the boundary.
Convergent 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.