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.
Emerald, Malachite, and Chrysoberyl etcReference: What_minerals_are_used_to_make_a_bright_green_color_or_special_effect
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.
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 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.
Peridot belongs to the mineral group called olivine. Olivine minerals are known for their green coloration and are commonly found in igneous rocks like basalt and peridotite.
The mineral name of peridot is olivine. It is a silicate mineral that is typically a bright green color due to its iron content. Peridot is used as a gemstone in jewelry due to its attractive color and clarity.
Mafic, igneous rocks
The mineral olivine is present in much greater quantities in peridotite compared to gabbro. Olivine is a common mineral in peridotite and gives it its characteristic green color, while gabbro contains less olivine and more plagioclase feldspar.
olivine
Dunite is typically a dark green to olive-green color due to its high concentration of the mineral olivine.
Peridot is composed of the mineral olivine, which is a silicate mineral containing magnesium and iron. Its characteristic green color is due to the presence of iron in its crystal structure.
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.
Olivine
Ophiolites form when the ocean crust is young and buoyant. At this point, it is less dense than the continents and is pushed on the continental crust when tectonic action occurs. Ophiolites are a part of the oceanic crust and upper mantle that have been placed on a continent.