Actually, the rock taken the farthest away from the ridge is older.
The further from the ridge, the older the oceanic crustal rock.
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.
Since it is called the 'mid ocean ridge' , it is in the middle of the ocean, far from land/countries. However, with one exception, Iceland. The mid Atlantic ocean ridge continues above the surface of the ocean, and has formed the island of Iceland.
The mid ocean ridge support it becuase your find similar sample of rock type on opposite side of the ridge which has thesame age. Mid-Oceanic ridge are where new sea floors are created which is usually called a divergent boundary. As these places move apart they push the other plates to collide and slide pass each other. That is why it is a cycle
Ridge push is a gravitation force that causes a plate to move away from the crest of an ocean ridge, and into a subduction zone.
Mid Ocean Ridge
Younger. The mid-ocean ridge is formed from new material being thrust up from inside the Earth.
yes
It gets younger.
no
hit the books!!
The closer the sediment is to the mid-ocean ridge, the younger it is. The oldest bedrock is found the farthest away from it.
A ridge is a geological feature that features a continuous elevational crest for some distance. If the ridge is under the ocean or sea, then it is called a submarine ridge.
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Mid Ocean Ridge
Glomar challenger
The further from the ridge, the older the oceanic crustal rock.