;klh
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.
Sediment closer to a mid-ocean ridge is typically younger, thinner, and composed of more volcanic material compared to sediment farther away. This is because the ridge is a site of active seafloor spreading where new oceanic crust is formed, leading to a higher rate of sedimentation near the ridge.
I don't have evidence, but oceanographers have evidence. In mid ocean ridges, more and more molten rocks come up from the surface and cool down. As a result, the rocks already there get pushed away. We did find molten rock coming up from the mantle. Also, when scientist carbon dated the rocks on mid ocean ridges, they found that the farther you go outward, the older the rock. That's another sign. There's more but i can't think of it now. Hope this helps.
Europe and North America are drifting farther apart at a rate of a few centimeters per year due to the movement of tectonic plates. This movement results from the spreading of the Atlantic Ocean, causing the two continents to move away from each other over time.
The evidence that supports Wegner's hypothesis is that in 1947 , a group of scientisits noticed two things about the Mid- Atlantic Ridge. The first thing that the scientists noticed was the sediment that covers the sea floor is thinner and younger closer to a ridge than it is farther from a ridge. Second, scientists learned that the ocean floor is very young. Radiometric dating shows that the sea floor closer to the mid-ocean ridge are younger, than the ones farther.
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.
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 newer rock is closer to the middle n th older ones spread along the sides
Oceanic crust that was farther away from a mid-ocean ridge was older that crust closer to the ridge
oceanic crust that was farther away from a mid-ocean ridge was older than crust closer to the ridge
Closer than what?
farther away
it is closer to the sun in june
Sediment closer to a mid-ocean ridge is typically younger, thinner, and composed of more volcanic material compared to sediment farther away. This is because the ridge is a site of active seafloor spreading where new oceanic crust is formed, leading to a higher rate of sedimentation near the ridge.
Closer
farther away