Opal is composed primarily of silica and water. It is a mineraloid, not a true mineral, because it lacks a crystalline structure.
No, not all minerals have crystalline structures. Some minerals, called amorphous minerals, do not have a regular crystalline structure and instead have a disordered atomic arrangement. Examples of amorphous minerals include opal and glass.
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.
Opal, being amorphous, is not really a mineral but a mineraloid. One of the scientifically accepted standards defining a mineral is that a mineral must have a crystal structure, which opal lacks. Many scientific groups and references, including the acclaimed Dana's System of Mineralogy, categorize Opal together with the "true" minerals. For this reason, Opal -- as well as other amorphous types that fall under the definition of a mineraloid.
Some minerals that exhibit a greasy luster include turquoise, serpentine, and nepheline. These minerals have a sheen that resembles the appearance of grease or oil on their surfaces.
Tourmaline opal belongs to the silicate class of minerals, specifically in the sub-group known as the cyclosilicates. It is characterized by its unique crystal structure and vibrant play-of-color caused by microscopic silica spheres within the stone.
Opal and amber are not minerals.
Opal and amber are not minerals.
Opals are actually not minerals, but are classed as mineraloids. This is because they lack a crystalline structure, yet are mineral in nature.
There are many minerals which can be found in the US, the rarest ones include Black Opal, Gold, Bauxite, Tin and Aluminium. There are other minerals which are extremely location specific.
There are 5 basic types of opal. These types are Peruvian Opal, Fire Opal, Girasol Opal, Common opal and Precious Opal.
Minerals by definition are solid, naturally occurring inorganic materials with a definite shape and crystalline structure. Opal water and mercury are both liquids lacking a definite shape and crystalline structre.
SiO2 .nH2O
The majority of minerals are crystalline materials.Examples: opal, halite, topaz.
Opal does not have a cleavage or fracture because it lacks a distinct cleavage plane like minerals such as mica or calcite. Instead, opal typically fractures conchoidally, meaning it breaks with smooth, curved surfaces similar to glass.
The streak of an opal is typically colorless due to its amorphous structure. It doesn't leave a visible streak on a streak plate like some other minerals do.
Opal is often referred to as a mineraloid because it lacks a crystal structure, which is a defining characteristic of minerals. Instead, opal is made up of tiny silica spheres arranged in a more random, non-repeating pattern, giving it its unique play-of-color. This amorphous structure sets it apart from traditional minerals.
The fracture of an opal can be hard or smooth , An opal can have as many fractures as any other mineral can . Sometimes opal can be smooth , sometimes they can be hard . The fracture of an opal is hard and smooth .