it moves
Spreading boundaries are places where two plates move apart.
tectonic plates move apart allowing magma to move to the surface.
Please make the question clearer. There are converging and diverging boundaries but not spreading boundaries. Plates move but don't spread. Please make the question clearer
Yes, convergent boundaries and sea-floor spreading are related in the sense that sea-floor spreading can occur at divergent boundaries (where tectonic plates move apart), leading to the creation of new oceanic crust. This new oceanic crust can then be consumed at convergent boundaries (where tectonic plates collide), as one plate is subducted beneath the other.
SPREADING ZONES Spreading zone occurs in the border of two tectonic plates. This happens when the plates generally move away from each other creating an opening for the magma to force through the surface.
convergent boundaries: plates move together divergent boundaries: plates move apart transform boundaries: plates move against each other
Plates move apart along divergent boundaries, where new crust is created through volcanic activity and magma upwelling from the mantle. This process is called seafloor spreading and occurs primarily in mid-ocean ridges.
Because the Asthenosphere is malleable, divergent boundaries and convergent boundaries are formed. The plasticity of the Asthenosphere allows the plates to move through sea floor spreading and subduction zones.
It could either cause Spreading boundaries (when the plates move apart), collision boundaries (Where one plate collides with the other forcing one underground- can cause volcano's, or transform boundaries (When plates scrape along side each other- causing Earthquakes.
Plates move apart on divergent plate boundaries.
Plates move apart at divergent boundaries, also known as spreading centers. This process is usually associated with the formation of new crust as magma rises from the mantle to fill in the gap created by the moving plates. An example of a divergent boundary is the Mid-Atlantic Ridge.
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.