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Granitic crust does not form at the mid-oceanic ridge. Rather another type of igneous rock Basalt is formed at the Mid-Oceanic ridge. Both are silicate rocks and have a high oxygen and silica content. The difference is that Granite is formed intrusively, that is within the Earth's crust. Basalt is extrusive, that is it is formed above the Earth's surface, such as at the bottom of the ocean at the Mid-Oceanic ridge.
Geothermal activity has revealed new characteristics of Earth's crust near Lake Myvatn, Iceland. In places like Iceland, new research has shown volcanoes and hot springs forming as the result of activity between the crust and the mantle.
At ocean spreading ridges, new oceanic crust is formed. The magma that forms this new crust emerges from the ridge and pushes the pre-existing rocks away from the ridge laterally. This results in a strip of new rock cutting through the older rock. As formation of the crust continues, the older rocks will be pushed further away from the ridge, while younger, newly produced rocks will occupy the area closest to the ridge.
Creates
Its oceanic crust
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Oceanic crust that was farther away from a mid-ocean ridge was older that crust closer to the ridge
No farther away
oceanic crust that was farther away from a mid-ocean ridge was older than crust closer to the ridge
The oldest rock in oceanic crust is that which is found the greatest distance from a mid-ocean-ridge.
The Oceanic Crust close to the Mid Ocean Ridge is thinner than that Oceanic Crust far away from the ridge. This is due to tensional forces, as a result of crustal expansion and rock fracturing during the formation of the ridge.the oceanic crust is thinner
Magma rises and slidifies and creates a new crust.
Magma rises and slidifies and creates a new crust.
Magma rises and slidifies and creates a new crust.