Coal is a very useful rock that formed over millions of years from the remains of plants. Is coal a mineral?

Yes, coal is considered a mineral because it is a naturally occurring, inorganic solid with a crystalline structure. Although it is not a traditional mineral like quartz or diamond, it meets the criteria to be classified as a mineral.

No, coal is not a mineral. While coal is indeed a useful rock formed from plant fossils, it does not meet the criteria to be classified as a mineral. Minerals are naturally occurring, inorganic substances with a specific chemical composition and a crystalline structure. Coal, on the other hand, is composed primarily of carbon and other organic matter, and its formation involves biological processes rather than geological ones.

To determine whether coal is a mineral or not, we need to understand the characteristics of minerals. A mineral is a naturally occurring, inorganic solid substance with a definite chemical composition and a regular atomic structure.

Now, let's examine coal based on these criteria:

1. Naturally occurring: Yes, coal is formed naturally over millions of years through a geological process.

2. Inorganic: Coal is derived from the remains of organic matter (plants), so it is considered organic rather than inorganic. Therefore, it does not meet this criterion.

3. solid substance: Coal is solid; it is not a liquid or a gas.

4. Definite chemical composition: While coal consists mainly of carbon, its composition can vary, including impurities such as sulfur, nitrogen, and minerals like clay, silica, and quartz. However, it lacks a precise or well-defined chemical formula like typical minerals. So, it does not meet this criterion either.

5. Regular atomic structure: Minerals have a crystalline atomic structure, which coal lacks. Instead, coal has an amorphous or non-crystalline structure.

Based on these characteristics, coal does not meet all the criteria to be classified as a mineral. Instead, it is often described as a sedimentary rock formed from the accumulation and transformation of organic material.