Seafloor spreading occurs at mid-ocean ridges where tectonic plates move apart, allowing magma to rise and create new oceanic crust. In contrast, subduction is the process where one tectonic plate is forced beneath another into the mantle, often resulting in volcanic activity and the formation of deep ocean trenches. While seafloor spreading generates new crust, subduction recycles old crust back into the Earth's interior. Together, these processes drive the dynamic nature of plate tectonics.
These zones are known as subduction zones where tectonic plates collide, forcing one plate to be pushed beneath the other. This process leads to the formation of deep ocean trenches and can result in earthquakes, volcanic activity, and the creation of mountain ranges.
They proved that the seafloor was spreading.
A diagram that shows how seafloor spreading works.
1. New sea-floor is created by the upwelling of magma at mid-ocean spreading centers; old ocean floor is destroyed by subduction at deep sea trenches. 2. The area is a subduction zone. Magma from underground comes up and destroys that crust. That crust is then recycled and the magma cools and hardens. That creates new land, that creates the trenches. Seafloor spreading is in the ocean and happens with convection currents. That is the relationship between. 3. As new seafloor is formed at mid-ocean ridges, the old seafloor is pushed down into trenches at subduction zones.
in a subduction trench, because of Harry Hess' theory of sea floor spreading. Meaning that the rock is formed new at the mid-ocean ridge, and moved out towards the coasts into a subduction zone years and years later.
Most volcanoes that cannot be ascribed either to a subduction zone or to a seafloor spreading at mid-ocean ridges are attributed to hot spots.
These zones are known as subduction zones where tectonic plates collide, forcing one plate to be pushed beneath the other. This process leads to the formation of deep ocean trenches and can result in earthquakes, volcanic activity, and the creation of mountain ranges.
Subduction and sea floor spreading are both a result of the movement of the tectonic plates.Plate Tectonics
They proved that the seafloor was spreading.
Yes, seafloor spreading is a process where new oceanic crust is formed at mid-ocean ridges, causing the Earth's crust to expand. This occurs as magma rises to the surface, solidifies, and pushes older crust away from the ridge, creating new seafloor.
A diagram that shows how seafloor spreading works.
1. New sea-floor is created by the upwelling of magma at mid-ocean spreading centers; old ocean floor is destroyed by subduction at deep sea trenches. 2. The area is a subduction zone. Magma from underground comes up and destroys that crust. That crust is then recycled and the magma cools and hardens. That creates new land, that creates the trenches. Seafloor spreading is in the ocean and happens with convection currents. That is the relationship between. 3. As new seafloor is formed at mid-ocean ridges, the old seafloor is pushed down into trenches at subduction zones.
in a subduction trench, because of Harry Hess' theory of sea floor spreading. Meaning that the rock is formed new at the mid-ocean ridge, and moved out towards the coasts into a subduction zone years and years later.
Gravity in the oceanic crust is responsible for seafloor spreading.
Seafloor spreading is triggered by a rift in a continental land mass.
A cause-events-and-effects graphic organizer can illustrate the relationship between convection currents, subduction, and seafloor spreading by identifying how each process influences the others. Convection currents in the Earth's mantle drive the movement of tectonic plates, leading to subduction, where one plate is forced under another. This process can create trenches and volcanic activity. Meanwhile, seafloor spreading occurs at mid-ocean ridges, where new oceanic crust is formed, contributing to the overall movement of plates and further influencing convection currents.
by: rift valleys subduction- volcanoes continental collision- mountain ranges seafloor spreading- cracks in ocean