Chert is a sedimentary rock primarily composed of microcrystalline silica (SiO₂) and typically exhibits a cryptocrystalline structure. This means that its silica content is present in extremely fine grains, making it difficult to see under a microscope. Chert can form in various environments, often from the accumulation of siliceous organisms or through the precipitation of silica from water. Its structure is generally dense and hard, with a smooth texture and a range of colors due to impurities.
Chert has a hard, smooth texture with a conchoidal fracture, meaning it breaks with curved surfaces similar to glass. It can feel dense and compact due to its microcrystalline structure.
Yes, the mineral malachite does have a crystal structure.
The crystal structure of phosphorous is monoclinic.
Chert has no streak, it is too hard.
The formula of chert is generally expressed as SiO2, which indicates that chert is primarily composed of silicon dioxide. However, chert can also contain impurities or trace elements that may alter its composition slightly.
Because the structure of chert varies greatly, I would recommend that you access the related link listed below- and refine your question.
There is no crystal structure.
Chert has a hard, smooth texture with a conchoidal fracture, meaning it breaks with curved surfaces similar to glass. It can feel dense and compact due to its microcrystalline structure.
Yes, the mineral malachite does have a crystal structure.
Beryllium's crystal structure is hexagonal.
The crystal structure of phosphorous is monoclinic.
The crystal structure of fermium was not determined.
a crystal structure is a turtle in disguise
Chert is a microcrystalline or cryptocrystalline sedimentary rock composed of silica (primarily quartz). It often forms as nodules or layers within other rocks, such as limestone, and is known for its hardness and conchoidal fracture.
The crystal structure of radium is cubic, body-centered.
Yes. Diamond is isometric, graphite is hexagonal.
a crystal.