No, it's a type of silica, and is classed as a mineraloid.
Opal is neither a sedimentary, igneous, nor metamorphic rock. It is actually a mineraloid composed of hydrated silica that is formed from silica-rich solutions at low temperature, often found in sedimentary rocks like sandstone or volcanic areas.
SiO2 .nH2O
The type of rock that likely formed first to initiate the rock cycle is igneous rock.
Yes, stone is considered a type of rock.
Opal is typically extracted from the earth through open-cut mining or underground mining methods. Miners use heavy machinery to remove overburden and dig into the opal-bearing layers, where they extract the opal-bearing rocks. These rocks are then processed to extract the opal gemstones.
Its a rock. Just a shiny one.
yes
Neither. Opal is a mineraloid, as it does not have a sufficiently organized structure to be considered a mineral.
igneous
No, it's actually a form of silica.
Geyserite is a type of rock that is formed by the precipitation of silica from hot spring water, typically around geysers and hot springs. It is composed mainly of siliceous material and resembles opal or chalcedony in appearance.
Yes, diatomite is a type of sedimentary rock made up of the fossilized remains of diatoms, a type of single-celled algae. Opal silica, on the other hand, refers to a non-crystalline form of silica that can be found in amorphous, hydrated, or gel-like states. While diatomite contains opal silica, they are not the same thing.
The types of Opal that i am familiar with are White Opal, Fire Opal, Boulder Opal, Black Opal, Crystal Opal, Light Opal, Doublet Opal, Triplet Opal, Common Opal, Synthetic Opal, and Immitation Opal.
An opal is considered to be a mineraloid, meaning that it has all of the properties of a mineral-- solid, inorganic, naturally forming, has a chemical composition-- but does not demonstrate crystallinity. Other examples of mineraloids include obsidian, an amorphous glass (that is not a crystal).
opal
No. Peridot is olivine.
Opal is amorphous mineraloid, occurrence : Sedimentary and secondary from the alteration of high silica igneous extrusive rocks