The igneous rock peridotite has a very high color index. It is comprised of more than 95% mafic minerals (like olivine), giving it a dark green color.
There are many rock forming minerals but some examples are peridotite,gabbro,basalt etc.Olivine is used in jewellery and a rock forming mineral.
A "color hue collage" is one color, divided into different shades of that color.
· Asparagus (a Crayola Crayon color) · Blizzard Blue (a former Crayola Crayon color retired in 2003) · Cornflower (a Crayola Crayon color) · Dandelion (a Crayola Crayon color) · Eggplant (a Crayola Crayon color) · Fuchsia (a Crayola Crayon color) · Goldenrod (a Crayola Crayon color) · Harlequin · Inch Worm (a Crayola Crayon color) · Jazzberry Jam (a Crayola Crayon color) · Khaki · Lavender (a Crayola Crayon color) · Macaroni and Cheese (a Crayola Crayon color) · Neon Carrot (a Crayola Crayon color) · Outer Space (a Crayola Crayon color) · Plum (a Crayola Crayon color) · Quail · Razzmatazz (a Crayola Crayon color) · Sunglow (a Crayola Crayon color) · Tumbleweed (a Crayola Crayon color) · Unmellow Yellow (a Crayola Crayon color) · Vivid Violet (a Crayola Crayon color) · Wisteria (a Crayola Crayon color) · X - ??? · Yellow Green (a Crayola Crayon color) · Zinc
wall color
no, tigers don't see color because they are color blind
Peridotite is mainly composed of olivine, along with pyroxenes and minor amounts of other minerals like spinel and garnet. These minerals give peridotite its characteristic green color.
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 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.
Peridotite is a coarse-grained, dense igneous rock composed mainly of olivine and pyroxene minerals. It is typically green in color due to the high concentration of olivine. Peridotite is commonly found in the Earth's upper mantle and is important in the formation of oceanic lithosphere.
Peridotite is a dense, coarse-grained igneous rock.
The dominant rock type of the upper mantle is peridotite.
A peridotite is a dense, coarse-grained igneous rock
peridotite
Mafic, igneous rocks
Garnet peridotite is a type of rock that forms in the Earth's mantle and contains a high proportion of both garnet and peridotite minerals. It is commonly found in subduction zones where oceanic plates are forced beneath continental plates. Garnet peridotite is important in understanding the processes that occur in the Earth's mantle.
The layer composed of peridotite is the mantle, which is located between the Earth's crust and core. Peridotite is the main rock type found in the upper mantle and is rich in minerals such as olivine and pyroxene.
Peridotite rocks are coarse-grained, dark-colored igneous rocks. They are the main source of all chromium ore and naturally occurring diamonds. Their magnesium content helps mitigate global warming.