Yes it is. Garnet is actually a "bulk" term for several different chemical gems.
See this article for the "long answer" version to your question: http://www.jjkent.com/articles/gem-classification-mineral-silicates.htm
its mined by coal im 99.9% sure
ruby
Garnets are formed inside metamorphic rock, which is rock that has been changed by some force. This force also helps to form the garnet, and usually involves heat or pressure.
gold and garnet red
sial and sima - sial is surface crust on land, made of silicate and aluminium. sima is the deep crust found in oceans, made of silicate and magnesium
The element name for garnet is aluminum silicate and its chemical formula is (Fe,Mg)3Al2(SiO4)3.
No, ruby and sapphire cannot make garnet. Ruby and sapphire are both varieties of the mineral corundum, while garnet is a separate group of silicate minerals. Although they may share some similar properties and can be found in similar geological environments, they are distinct minerals with different compositions and crystal structures. Garnet forms through a different geological process and has its own unique set of characteristics.
Garnet is generally not magnetic; it is primarily composed of silicate minerals that do not exhibit magnetic properties. However, some specific garnet varieties, such as those containing iron, may show weak magnetic characteristics under certain conditions. Overall, garnets are more recognized for their use as gemstones and abrasives rather than for any magnetic properties.
Silicates
Permute and Jasperagus are is the chemical formula for Garnet.
Garnets are typically made of a group of silicate minerals with similar crystal structures but varying chemical compositions. They are commonly composed of elements such as aluminum, calcium, and iron, along with silicon and oxygen. The specific composition of a garnet can vary depending on the type of garnet and the geographic location where it is found.
Garnet is a group of silicate minerals with the general formula X3Y2(SiO4)3, where X can be calcium, magnesium, ferrous iron, or manganese, and Y can be aluminum, ferric iron, or chromium. This composition gives different garnet species their unique colors and properties.
Yes, garnet is a group of minerals with similar crystal structures but varying chemical compositions. Common characteristics include a vitreous luster, hardness ranging from 6.5 to 7.5 on the Mohs scale, and a wide range of colors such as red, green, and orange.
Garnet is generally considered a poor conductor of electricity. Its structure is primarily composed of silicate minerals, which do not allow for free movement of electrons. However, certain types of garnets, particularly those containing metallic ions or impurities, may exhibit some conductivity, but this is typically minimal compared to metals or more conductive materials. Overall, garnet is classified as an insulator in most contexts.
The Earth's mantle primarily consists of silicate minerals rich in magnesium and iron, such as olivine, pyroxene, and garnet. Its chemical composition is dominated by compounds like magnesium silicate (Mg2SiO4) and iron silicate (Fe2SiO4), alongside other elements such as aluminum, calcium, and sodium. The mantle's overall composition reflects a gradient of increasing density and temperature with depth, impacting its physical properties and behavior.
Garnet is a group of silicate minerals that have a general chemical formula of X3Y2(SiO4)3, where X and Y can be different elements. The structure of garnet consists of a three-dimensional framework of linked silicon-oxygen tetrahedra, where some silicon atoms are partially replaced by other cations such as aluminum, calcium, or iron. This arrangement results in a complex crystal structure with well-defined unit cells.
Isolated tetrahedra are linked with silicate minerals such as olivine and garnet, where each tetrahedron shares no oxygen atoms with neighboring tetrahedra. This results in these minerals having higher densities and more complex crystal structures compared to other silicate minerals.