subducting
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 Plate Boundary. (Seafloor Spreading).
Compressional stresses occur at convergent plate boundaries.
Its a divergent boundary
convergent boundary.
An invisible boundary, probably.An invisible boundary, probably.An invisible boundary, probably.An invisible boundary, probably.
It's a divergent plate boundary.
Without specific context about "slit b," it's challenging to provide an accurate answer. However, if "slit b" refers to a geological feature, it could represent a type of plate boundary such as a divergent, convergent, or transform boundary. Divergent boundaries occur where tectonic plates move apart, convergent boundaries occur where they collide, and transform boundaries occur where they slide past each other. Each type is characterized by distinct geological activity and landforms.
Most underwater volcanoes occur at divergent plate boundaries, where tectonic plates move away from each other, allowing magma to rise up and form new crust. This process creates underwater mountain ranges known as mid-ocean ridges.
The plate boundary that causes mountains to form is called a convergent boundary.
It is divergent between the North American and Eurasian plates. Volcanoes and earthquakes do occur along the boundary.
A convergent plate boundary forms a deep sea trench. This occurs when two tectonic plates are pushed towards each other, causing one to subduct beneath the other, creating a trench in the ocean floor.