Subduction and sea floor spreading are both a result of the movement of the tectonic plates.Plate Tectonics
Sea floor spreading is where new oceanic crust is formed through volcanic activity and then moves away from the ridge. Subduction is when one tectonic plate moves under another tectonic plate. Hope this helped :)
The most violent earthquakes are generally associated with subduction zones where tectonic plates collide and one is forced beneath the other. These subduction zones can produce very large and destructive earthquakes, such as the 2004 Indian Ocean earthquake and tsunami. Spreading centers, on the other hand, usually produce smaller earthquakes due to the gradual separation of tectonic plates.
The area where two tectonic plates meet is called a plate boundary. At plate boundaries, interactions between the plates can result in processes like subduction, seafloor spreading, or continental collision.
A transform fault is a boundary where two tectonic plates slide past each other horizontally. A subduction zone is where one tectonic plate is being forced beneath another. Subduction zones are associated with the occurrence of deep oceanic trenches and volcanic arcs, while transform faults are usually characterized by earthquakes.
Spreading center earthquakes are always shallow, subduction zone earthquakes can be very deep.Spreading center earthquakes are typically of lower magnitude than subduction zone earthquakes.
Subduction and sea floor spreading are both a result of the movement of the tectonic plates.Plate Tectonics
Subduction zones are also known as convergent boundaries, there is no difference.
spreading subduction translation
it is the study of making sanwhichs
they dont affect it
Both subduction zones and spreading centers.
Subduction and sea floor spreading are both a result of the movement of the tectonic plates.Plate Tectonics
subduction and sea floor spreading.
A subduction zone occurs at convergent plate margins where an oceanic plate is going underneath a continental plate or a less dense oceanic plate. A mid-ocean ridge is a divergent plate boundary on the ocean floor with a mountain range and a rift running through the center of it. Sea floor spreading also occurs at mid ocean ridges.
In subduction zones, one tectonic plate is forced beneath another, causing the plates to converge. In contrast, at spreading boundaries, tectonic plates are moving apart from each other, which results in the formation of new crust as magma rises and solidifies. Thus, subduction zones involve plate convergence, while spreading boundaries involve plate divergence.
a constructive (divergent) plate boundary, new crust is being created to infill the gaps caused by spreading plates. At a destructive (subduction-convergent) plate boundary, old, dense oceanic crust is diving into, and becoming part of the mantle.Read more: What_is_the_difference_between_a_constructive_plate_boundary_and_a_destructive_plate_boundary