.At spreading boundaries, plates move away from each
other and gaps form between the plates. Convection
currents cause magma to rise from the mantle through
these gaps. Huge valleys can form. This type of plate
movement is responsible for seafloor spreading. The
Mid-Atlantic Ridge formed at plate boundaries that
were moving apart.At fracture boundaries, plates slide past each other.
This break in Earth's crust is called a fault. The
movement of the plates past each other can cause
strong earthquakes.The area where two plates push against each other is
called a colliding boundary. When plates collide, one
plate might slide beneath the other. When plates carry
continents into each other, towering mountains form.
Other times, deep ocean trenches, earthquakes, and
volcanoes can result.
Divergent Plate Boundary. (Seafloor Spreading).
When seafloor spreading happens, a rift forms at the bottom of a ocean and separates to form new rock. This is an example of a divergent plate boundary
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.
Divergent boundaries is the other name for a spreading plate boundary.
Yes. The seafloor is spreading out from the Mid-Atlantic Ridge. The North American Plate is moving slowly SW from the boundary.
along plate boundaries
seafloor spreading
At the mid-ocean ridges, a divergent plate boundary.
Yes. The theory of plate tectonics is very broad, and it covers seafloor spreading, continental drift, plate boundaries and so on.
seafloor spreading
Seafloor is created at divergent plate boundaries called the mid-ocean ridges.
The mid-ocean ridge system is the longest continuous divergent plate boundary on Earth.