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The major source of oceanic salinity is the dissolution of ions from rocks on land that are carried into the ocean by rivers. This process adds various salts to seawater, contributing to its overall salinity. Additionally, hydrothermal vents on the ocean floor can also introduce elements and minerals that affect salinity.
Earth's oceanic crust is primarily made up of basalt, which contains minerals such as plagioclase feldspar, pyroxene, and olivine. These minerals form from the solidification of magma that emerges from mid-ocean ridges.
Two types of minerals found in Earth's crust are silicate minerals and nonsilicate minerals. Silicate minerals are the most abundant type and contain silicon and oxygen. Nonsilicate minerals do not contain silicon and oxygen in their chemical composition.
Basalt rock with a layer of sedimentary rock overlaying that, covered with water saturated sediments.
No, the magnetic stripes on the ocean floor form due to the alignment of magnetic minerals in the crust as it solidifies from the mantle. The oceanic crust is eventually consumed in subduction zones and recycled back into the mantle, but the magnetic stripes themselves do not sink back into the mantle.
The major source of oceanic salinity is the dissolution of ions from rocks on land that are carried into the ocean by rivers. This process adds various salts to seawater, contributing to its overall salinity. Additionally, hydrothermal vents on the ocean floor can also introduce elements and minerals that affect salinity.
Yes, oceanic crust is typically found below sea level. It forms the Earth's ocean basins and is covered by seawater.
the oceanic plate
Two metamorphic minerals that can form along oceanic ridges are chlorite and epidote. Chlorite forms from the metamorphism of basaltic rocks, while epidote is commonly found in hydrothermally altered oceanic crust.
A hydrothermal vent is formed when seawater seeps into cracks in the oceanic crust, gets heated by magma underneath, and then rises back to the seafloor. The high temperatures and pressure at these vents cause minerals and metals to dissolve in the hot water, creating unique underwater ecosystems.
Earth's oceanic crust is primarily made up of basalt, which contains minerals such as plagioclase feldspar, pyroxene, and olivine. These minerals form from the solidification of magma that emerges from mid-ocean ridges.
There are far more than two minerals that form rocks. You have to consider that there are about 3800 known minerals found on Earth. However, two minerals that are extremely abundant in continental and oceanic rock are feldspar and quartz.
The oceanic crust is thought to approximate the average composition of the upper mantle, which is mainly composed of silicate minerals such as basalt and gabbro. These minerals are rich in elements like silicon, magnesium, and iron, which are common in the Earth's mantle.
Two types of minerals found in Earth's crust are silicate minerals and nonsilicate minerals. Silicate minerals are the most abundant type and contain silicon and oxygen. Nonsilicate minerals do not contain silicon and oxygen in their chemical composition.
Basalt rock with a layer of sedimentary rock overlaying that, covered with water saturated sediments.
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 ^^
Continental crust is generally lighter in color than oceanic crust. This is because continental crust is composed of lighter-colored rocks such as granite, which contain lighter minerals like quartz and feldspar. In contrast, oceanic crust is made up of darker-colored rocks like basalt, which contain heavier minerals like pyroxene and olivine.