it moves
What is a spreading boundary
a spreading boundary is when 2 plates spread apart from each other.
Another name for a spreading boundary is a divergent boundary. This is where tectonic plates move away from each other, leading to the formation of new oceanic crust. Examples of divergent boundaries include the Mid-Atlantic Ridge and the East Pacific Rise.
No, sea floor spreading does not occur at a convergent boundary. Sea floor spreading occurs at divergent boundaries where tectonic plates move away from each other, allowing magma to rise and create new oceanic crust. At convergent boundaries, two plates collide, leading to subduction or crustal deformation.
Divergent boundaries is the other name for a spreading plate boundary.
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.
During sea floor spreading, pieces of oceanic crust move apart as new magma rises to the surface at mid-ocean ridges. As the crust spreads, it carries with it the magnetic signature of Earth's magnetic field, providing evidence for the process of seafloor spreading.
spreading or divergent boundary
A divergent plate boundary will form between India and Australia when they move in different directions. This boundary will result in the two plates moving away from each other, leading to the formation of new crust as magma rises to the surface.
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.
Sea floor spreading is primarily found along divergent boundaries, where tectonic plates move away from each other. As the plates separate, magma rises from the mantle to create new oceanic crust at the mid-ocean ridges. This process contributes to the continuous expansion of the ocean basins.
divergent boundary