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 Plate Boundary. (Seafloor Spreading).
Mid-oceanic ridges
At a divergent boundary, land is gained. Ocean ridges are prominent at divergent plate boundaries. Ocean ridges are areas of seafloor spreading. Seafloor spreading occurs as upwelling magma rises to the surface. This upwelling magma hardens and forms new seafloor.
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.
The 3 types of plate boundaries that occur is the spreading boundary, fracture boundary, and the colliding boundary.
subducting
Seafloor spreading occurs at the boundary between tectonic plates because of the divergent movement of these plates. As the plates move apart, magma rises from the mantle to fill the gap, solidifying as it cools and creating new seafloor. This process is instrumental in the formation of mid-ocean ridges and plays a key role in the theory of plate tectonics.
They proved that the seafloor was spreading.
A diagram that shows how seafloor spreading works.
The East Pacific Rise is a divergent plate boundary where tectonic plates are moving apart. This boundary is associated with seafloor spreading and the creation of new oceanic crust.
Seafloor spreading is triggered by a rift in a continental land mass.