The Earth's upper mantle has a composition similar to the green mineral olivine. Olivine is a common mineral found in the upper mantle, making up a significant portion of its composition.
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 has a distinctive green color, making it easy to identify visually. It has a high hardness of 6.5-7 on the Mohs scale, aiding in its differentiation from other minerals. Olivine often occurs in tabular or elongate crystal shapes, which can help distinguish it from similar minerals.
The "Peridot(Olivine)" is the light green August birthstone.
Olivine is mined in various countries around the world, including the United States, Norway, Finland, and India. Some of the major olivine mining locations include Hawaii (forsterite-rich olivine), Norway (fayalite-rich olivine), and Finland. These regions have significant deposits of olivine due to their geological history and processes.
Some volcanoes appear green because of the growth of mosses, ferns, and other vegetation on their slopes, which thrive in the nutrient-rich volcanic soil. The green color is due to the chlorophyll in the plants, which reflects green light. It can also be caused by minerals such as olivine, which is green in color.
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.
The uppermost mantle rock is Peridotite, which is mostly olivine and pyroxene but varies somewhat in chemical composition. Generally it is a coarse grained greenish rock. The name peridotite is derived from the gemstone peridot, which is pale green olivine.
Mafic, igneous rocks
Olivine has a distinctive green color, making it easy to identify visually. It has a high hardness of 6.5-7 on the Mohs scale, aiding in its differentiation from other minerals. Olivine often occurs in tabular or elongate crystal shapes, which can help distinguish it from similar minerals.
The "Peridot(Olivine)" is the light green August birthstone.
Peridot is composed of the mineral olivine, which is a silicate mineral made up of iron and magnesium. It has a molecular formula of (Mg,Fe)2SiO4. The vibrant green color of peridot is due to its iron content.
Olivine is mined in various countries around the world, including the United States, Norway, Finland, and India. Some of the major olivine mining locations include Hawaii (forsterite-rich olivine), Norway (fayalite-rich olivine), and Finland. These regions have significant deposits of olivine due to their geological history and processes.
Some volcanoes appear green because of the growth of mosses, ferns, and other vegetation on their slopes, which thrive in the nutrient-rich volcanic soil. The green color is due to the chlorophyll in the plants, which reflects green light. It can also be caused by minerals such as olivine, which is green in color.
four common members of olivine family that is 1) FORSTERITE ((Mg) 2SiO4.2) fayalite(Fe) 2SiO43)olivineMn SiO44) tephorite( Mn2SiO4)
Dunite is typically a dark green to olive-green color due to its high concentration of the mineral olivine.
Because their basic cellular composition remains similar to the modern plants.