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At the mid-atlantic ridge, where the ocean floor is spreading.
You would be looking at the solidified magma closest to the fault between the ridges.
They are arranged in a pattern with magnetic strips having reversed polarities.
The rocks off of the east coast of North America are much older than those right along the mid-Atlantic ridge because sea-floor spreading is occurring where oceanic plates are diverging from one another. The rocks right along the ridge are the newest ones being formed, and the ones off the east coast of North America were formed a long time ago.
no
The farther away the rocks are, the older they are. When the lava bubbles up from the ridge, the tectonic plates move outward. As the process repeates itself and new lava comes up, the rocks are pushed farther and father away. As a result, the closest rocks are the newest, and the farthest rocks are the oldest!
parrell strips of igneous rocks on each side of the ridge show matching reversal of magnetic polity
they are much older than the mid atlantic rocks beacuse the rock works its way out and up the older it gets i might be rong so id double check
;klh
cuz rocks come up from the ridge and create land by the ridge
Sedimentary Rocks Don't forget pillow lavas, and water-chilled lavas. Mid-ocean ridge rocks are surely worth a mention. And flow silicates such as the 'Pink and White terraces' and similar elsewhere in the world.
1.) The age of the rocks- the oldest ones are found further away from the original mid-atlantic ridge. 2.) Magnetic clues. The rocks with iron in them have shown that the Earth's magnetic field has reversed itself several times. It is imprinted in the rock.