(mineralogy) A naturally occurring, inorganic material that is amorphous and is therefore not considered to be a mineral. Also known as gel mineral.
| Sci-Tech Dictionary: mineraloid |
(mineralogy) A naturally occurring, inorganic material that is amorphous and is therefore not considered to be a mineral. Also known as gel mineral.
| 5min Related Video: Mineraloid |
| Wikipedia: Mineraloid |
A mineraloid is a mineral-like substance that does not demonstrate crystallinity. Mineraloids possess chemical compositions that vary beyond the generally accepted ranges for specific minerals. For example, obsidian is an amorphous glass and not a crystal. Jet is derived from decaying wood under extreme pressure. Opal is another mineraloid because of its non-crystal nature. Pearls, considered by some to be a mineral because of the presence of calcium carbonate crystals within their structure, would be better considered a mineraloid because the crystals are bonded by an organic material and there is no definite proportion of the components.
| This article about a specific mineral or mineraloid is a stub. You can help Wikipedia by expanding it. |
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
| Archerite | |
| Telluride mineral | |
| Yttrocolumbite |
| What is the differents between a mineral and a mineraloid? Read answer... | |
| What is a mineraloid? Read answer... | |
| What are some mineraloids? Read answer... |
| Is there another name for a mineraloid? | |
| What are three examples of a mineraloid? | |
| What are the three examples of a mineraloid? |
Copyrights:
![]() | Sci-Tech Dictionary. McGraw-Hill Dictionary of Scientific and Technical Terms. Copyright © 2003, 1994, 1989, 1984, 1978, 1976, 1974 by McGraw-Hill Companies, Inc. All rights reserved. Read more | |
![]() | Wikipedia. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article "Mineraloid". Read more |