At mid-oceanic ridges, plates are pulled apart in two separate directions. This creates a gap (rift valley), allowing for warm, buoyant magma to rise to the surface and cool. As the magma cools, it creates ridges along the rift valleys. The elevation is caused by the excess amount of newly created, less dense oceanic crust. This crust occupies more volume, which causes it to be higher up than the surrounding, older crust.
a ridge in the ocean
Along the mid oceanic ridges (sites of crustal generation)
a ridge in the ocean
New oceanic crust is being created at the mid-ocean ridges.
The youngest parts of the Earth's crust are found in the oceanic crust. This crust is continuously being created at the mid-oceanic ridges.
mountainous topography
New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.
At the oceanic ridges the age of igneous basalt rocks is approximately zero (as that is where they formed) and the rocks get older the farther away. The ages of sedimentary and metamorphic rocks does not correlate reliably with distance from the oceanic ridges like the ages of igneous rocks, because they can form anywhere not mainly at oceanic ridges. Igneous granite rocks are generally formed around continental volcanos not oceanic ridges.
2. Mid Ocean Ridges are the place where new crust is formed. 1. oceanic plates or oceanic crust
Magmatic upsurge from within the earths crust, and plumes.
Ridges of buoyant oceanic crust form at diverging oceanic plate boundaries.
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