Olivine appears green because of its iron content. The iron in olivine absorbs certain wavelengths of light, especially in the red part of the spectrum, giving it a green hue. This characteristic color is why olivine-rich rocks like peridot have a distinct green color.
Olivine typically exhibits a glassy or vitreous luster. This is due to its composition of magnesium, iron, and silicate minerals, which create a smooth, reflective surface when light interacts with the crystal structure. The luster of olivine can vary depending on the specific composition and crystal structure of the mineral.
Olivine does not contain Gabbro. Gabbro can contain olivine. Usually no more than a few percent.
Olivine weathers quickly when exposed to water and air, transforming into other minerals like clay minerals. This rapid weathering process results in olivine being rare in sandstone found on beaches, even in volcanic islands where olivine is abundant in the rocks.
The value of olivine can vary significantly based on factors such as quality, size, and market demand. Generally, olivine used for industrial purposes may range from $10 to $200 per ton, while high-quality gemstones, like peridot (the gem variety of olivine), can sell for $50 to $400 per carat or more, depending on their clarity and color. Overall, the worth of olivine depends on its application and market conditions at the time.
Olivine rock got its name from its olive-green color, which comes from the mineral olivine found within it. Olivine is a common mineral in the Earth's mantle and is often found in igneous rocks like basalt and gabbro.
Olivine appears green because of its iron content. The iron in olivine absorbs certain wavelengths of light, especially in the red part of the spectrum, giving it a green hue. This characteristic color is why olivine-rich rocks like peridot have a distinct green color.
Olivine typically exhibits a glassy or vitreous luster. This is due to its composition of magnesium, iron, and silicate minerals, which create a smooth, reflective surface when light interacts with the crystal structure. The luster of olivine can vary depending on the specific composition and crystal structure of the mineral.
Olivine fractures.
Olivine typically exhibits conchoidal fracture, which is a type of fracture characterized by smoothly curving, shell-like surfaces. It does not have distinct cleavage planes due to its orthorhombic crystal structure.
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Olivine is the mineral that is present in much greater quantities in peridotite compared to gabbro. Peridotite is rich in olivine, which gives it its characteristic green color, while gabbro contains less olivine and more dark minerals like pyroxene.
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