The hot magma heats the ocean water that seeps underground. The heated water dissolves minerals. When the solution billows out of vents called "chimneys" the minerals crystallize in the cold sea water. I hope that answers your question ^^
Mineral formation can occur several ways along the MOR. Rising magma can cool and crystallize, forming igneous rock which contains various minerals. Heated seawater also percolates through the hot rock of the MOR, and can precipitate minerals on rock surfaces and at black smokers.
Fill in the graphic organization to explain the step of the formation of a mid-ocean ridge
it gets hot
The youngest part of the ocean floor is found at conservative plate boundaries where oceanic crust is pulled apart and magma rises from the mantle to form new oceanic crust.
The length of the Explorer Ridge is 150 miles. This mid-ocean ridge is a divergent tectonic plate that is located near Vancouver Island in Canada.
Near fault lines, it is there that rocks are created by the rubbing or colliding of the tectonic plates. Rocks could also be made by volcanoes via the cooling of magma and lava. The closer to the fault line you are the newer the rock and the farther away you get the older the rock becomes.
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
fault line
No. The newest ocean floor is at the mid-ocean ridge.
The youngest part of the ocean floor is found at conservative plate boundaries where oceanic crust is pulled apart and magma rises from the mantle to form new oceanic crust.
Near the mid-Atlantic ridge.
By determining the age of rock samples obtained by drilling on the sea floor.
Near ocean ridges such as the Atlantic ridge
hit the books!!
Its oceanic crust
The length of the Explorer Ridge is 150 miles. This mid-ocean ridge is a divergent tectonic plate that is located near Vancouver Island in Canada.
Near fault lines, it is there that rocks are created by the rubbing or colliding of the tectonic plates. Rocks could also be made by volcanoes via the cooling of magma and lava. The closer to the fault line you are the newer the rock and the farther away you get the older the rock becomes.
First of all, a body system does not support minerals. Minerals can be formed near the mid-ocean ridge or in magma chambers or in the earths crust. we asked bout body system not oceans and magma
haha i really dont know
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