It is a center at the bottom of the ocean that occurs at mid-ocean ridges
Spreading centers.
Volcanoes at spreading centers is referred to as spreading center volcanism. This usually takes place on mid-oceanic ridges where the plates diverge.
Both subduction zones and spreading centers.
Basaltic magma is the most abundant type erupted at oceanic spreading centers. It is low in silica content and flows easily due to its low viscosity, allowing it to create the characteristic volcanic features seen at mid-ocean ridges.
Seafloor spreading occurs at an average rate of about 2.5 centimeters per year, which translates to approximately 25 kilometers per million years. This rate can vary depending on the location and tectonic plate interactions, with some mid-ocean ridges spreading faster or slower. Overall, the average rate is generally consistent across the majority of oceanic spreading centers.
Spreading centers.
Volcanoes at spreading centers is referred to as spreading center volcanism. This usually takes place on mid-oceanic ridges where the plates diverge.
At spreading centers.
These ridges are spreading centers or divergent plate boundaries
It is the mid-ocean ridges.
It is a center at the bottom of the ocean that occurs at mid-ocean ridges
Both subduction zones and spreading centers.
spreading centers
spreading centers
These ridges are spreading centers or divergent plate boundaries
Basaltic/mafic lava.
Near the trenches, or in the seafloor furthest away from spreading centers.