I don't believe that is possible to figure out
Sediment closer to mid-ocean ridges is typically younger, coarser, and consists of more volcanic material compared to sediment farther away. This is because the closer proximity to the ridge results in a higher input of freshly erupted material from the underlying volcanic activity.
Scientists discovered that rocks farther away from the mid-ocean ridge were older than those near it through radiometric dating of the rocks. By measuring the age of the minerals within the rocks, they found that the farther rocks were older because they had been slowly moving away from the ridge as new crust formed at the ridge and pushed older crust farther out.
thye pulled rocks from a drill and studied them obviously
No, the farther from a mid-ocean ridge a rock sample is taken, the older the rock generally is. Mid-ocean ridges are sites of seafloor spreading, where new oceanic crust is formed as magma rises and cools. As tectonic plates move away from the ridge, the rocks gradually age, making those farther from the ridge older than those closer to it.
The age of rocks in the ocean crust depends on where the rocks are collected. Scientists collected rock samples from the sea floor. They found out that rock samples that were closer to mid-ocean ridges were younger than the samples farther away from the ridges. So pretty much you could get rocks that are thousands of years old to over millions of year old.
Closer
farther away
Scientists discovered that rocks farther away from the mid-ocean ridge were older through radiometric dating of the rocks. By analyzing the age of the minerals within the rocks, researchers found that the rocks closest to the ridge were younger, while those farther away were older, supporting the theory of seafloor spreading.
it is older
the alantic ocean is closer to alll parts of ohio therefore the pacific ocean is father away.
Oceanic crust that was farther away from a mid-ocean ridge was older that crust closer to the ridge
i never know
Sediment closer to mid-ocean ridges is typically younger, coarser, and consists of more volcanic material compared to sediment farther away. This is because the closer proximity to the ridge results in a higher input of freshly erupted material from the underlying volcanic activity.
oceanic crust that was farther away from a mid-ocean ridge was older than crust closer to the ridge
They measure how far away the rock is from the mid-ocean ridge. The farther, the older.
Scientists discovered that rocks farther away from the mid-ocean ridge were older than those near it through radiometric dating of the rocks. By measuring the age of the minerals within the rocks, they found that the farther rocks were older because they had been slowly moving away from the ridge as new crust formed at the ridge and pushed older crust farther out.
thye pulled rocks from a drill and studied them obviously