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chalcedony

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chalcedony

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Chalcedony ( or ) is a cryptocrystalline form of silica, composed of very fine intergrowths of quartz and moganite. These are both silica minerals, but they differ in that quartz has a trigonal crystal structure, while moganite is monoclinic. Chalcedony's standard chemical structure (based on the chemical composition of quartz) is (silicon dioxide).

AI overview

Chalcedony is a type of mineral made from extremely fine mixtures of quartz and moganite, both forms of silicon dioxide, that are so tiny they can't be seen individually with the naked eye. It's composed of the same basic material as regular quartz, but has a different internal structure due to the way these two mineral components are interwoven together.

AI-generated from the Wikipedia summary — may contain errors.

Key facts

Mineral.name
Chalcedony
Mineral.category
Tectosilicate minerals
Mineral.group
Quartz group
Mineral.IMAstatus
Variety of quartz
Mineral.image
Quartz-46809.jpg
Mineral.imagesize
260px
Mineral.caption
A botryoidal geode specimen from Mexico
Mineral.formula
(silica)
Mineral.molweight
60 g/mol
Mineral.color
Various
Mineral.habit
Various
Mineral.system
Trigonal (quartz) or monoclinic (moganite)
Mineral.cleavage
Absent
Mineral.fracture
Uneven, splintery, conchoidal
Mineral.mohs
6–7
Mineral.luster
Waxy, vitreous, dull, greasy, silky
Mineral.streak
White
Mineral.gravity
2.59–2.61

via Wikipedia infobox

Wikidata facts

Image
Mineraly.sk - chalcedon.jpg
Show 3 more facts
Commons category
Chalcedony
Commons gallery
Chalcedony
Mohs' hardness
7.0
Sources (7)

via Wikidata · CC0

~9 min read

Article

18 sections
Contents
  • Varieties
  • Agate
  • Carnelian
  • Chrysoprase
  • Fire agate
  • Heliotrope
  • Moss agate
  • Chrome chalcedony
  • Onyx
  • Chalcedony ice-blue
  • History
  • Geochemistry
  • Structure
  • Solubility
  • Solubility of quartz and chalcedony in pure water
  • See also
  • References
  • External links

Chalcedony ( or ) is a cryptocrystalline form of silica, composed of very fine intergrowths of quartz and moganite. These are both silica minerals, but they differ in that quartz has a trigonal crystal structure, while moganite is monoclinic. Chalcedony's standard chemical structure (based on the chemical composition of quartz) is (silicon dioxide).

Chalcedony has a waxy luster, and may be semitransparent or translucent. It can assume a wide range of colors, but those most commonly seen are white to gray, grayish-blue or a shade of brown ranging from pale to nearly black. The color of chalcedony sold commercially is often enhanced by dyeing or heating.

Gallery (38)

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