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seafloor spreading
Yes sea floor spreading and or undersea volcanic eruptions can cause a tsunami or huge ocean wave.
The tectonic plates are separating and growing more ocean floor (seafloor spreading).
suduction or sea floor spreading
The typical rates of seafloor spreading is 5 centimeters per year. Seafloor spreading is a process that occurs at mid ocean ridges.
Ocean currents have no effect whatsoever. Seafloor spreading is caused by convection currents in the rock of the earth's mantle.
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
It is called Seafloor Spreading, which comes under the Divergent Plate Movement.
Convergence supports the theory of seafloor spreading. Samples of the deep ocean floor are evidence of seafloor spreading because the basaltic oceanic crust and overlapping sediment become younger as the mid-ocean ridge is approached. Also, the rock that makes up the floor of the ocean is younger than the continents.
seafloor spreading
Near the trenches, or in the seafloor furthest away from spreading centers.
seafloor spreading, age of the sea floor and ocean trenches.
Yes sea floor spreading and or undersea volcanic eruptions can cause a tsunami or huge ocean wave.
The tectonic plates are separating and growing more ocean floor (seafloor spreading).
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
The ages of the rocks become older the farther the way they are from the ridges. The closer they are the younger it is. This leaves evidence to the seafloor spreading theory.
Seafloor spreading is a process that occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge. Seafloor spreading helps explain continental drift in the theory of plate tectonics.