A mineraloid is a naturally occurring substance that does not have a crystalline structure like minerals. Instead, mineraloids have an amorphous or non-crystalline structure. Examples of mineraloids include opal and obsidian.
A mineraloid is a naturally occurring substance that does not have a crystalline structure. Examples include amber, opal, and obsidian. These substances are often formed through geological processes but lack the ordered atomic structure of true minerals.
Opals are not truly minerals (because they don't have a crystalline structure), they are in a class called mineraloid. A mineraloid is an amophous, inorganics substance that lacks a crystalline structure, but are mineral in nature. You will find that in many older reference systems, they may well be classed as minerals.
Opals are classified as mineraloids, not rocks. They are made up of silica and water, with a unique internal structure that diffracts light to display a play of colors.
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.
they are obsidian, opal, limonite
A mineraloid is a naturally occurring substance that does not have a crystalline structure like minerals. Instead, mineraloids have an amorphous or non-crystalline structure. Examples of mineraloids include opal and obsidian.
A mineraloid is a naturally occurring substance that lacks a crystalline structure, which distinguishes it from minerals that have a well-defined atomic structure. They may have a chemical composition similar to minerals but do not exhibit the same regularity in their internal arrangement of atoms. Amber and opal are examples of mineraloids.
A mineraloid is a naturally occurring substance that does not have a crystalline structure. Examples include amber, opal, and obsidian. These substances are often formed through geological processes but lack the ordered atomic structure of true minerals.
nothing
Opal is an amorphous form of silica related to quartz, a mineraloid form, not a mineral. A mineraloid is a mineral-like substance that does not demonstrate crystallinity.Now you get it?
There really isnt a crystal form. Therefore it is a mineraloid.
Opal is a hydrated amorphous form of silica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as minerals Opal is a hydrated amorphous form of silica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as minerals silica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as mineralssilica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as minerals
A mineraloid is a naturally occurring mineral-like substance that lacks a crystalline structure. Unlike minerals, mineraloids do not have a specific chemical composition or definite atomic arrangement. Some examples of mineraloids include obsidian, opal, and amber.
Neither. Opal is a mineraloid, as it does not have a sufficiently organized structure to be considered a mineral.
Opal is a hydrated amorphous form of silica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as minerals Opal is a hydrated amorphous form of silica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as minerals silica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as mineralssilica; its water content may range from 3 to 21% by weight, but is usually between 6 and 10%. Because of its amorphous character, it is classed as a mineraloid, unlike crystalline forms of silica, which are classed as minerals
3 examples of what?