Editing Quartz

'''Quartz''' (from German "Quarz") is the most abundant mineral in the [[Earth]]'s continental crust. It is made up of a lattice of silica (SiO2) tetrahedra. Quartz has a hardness of 7 on the Mohs scale and a density of 2.65 g/cm³.

Quartz belongs to the rhombohedral crystal system. The ideal crystal shape is a six-sided prism terminating with six-sided pyramids at each end. In nature quartz crystals are often twinned, distorted, or so intergrown with adjacent crystals of quartz or other minerals as to only show part of this shape, or to lack obvious crystal faces altogether and appear massive. Well-formed crystals typically form in a 'bed' that has unconstrained growth into a void, but because the crystals must be attached at the other end to a matrix, only one termination pyramid is present. A quartz geode is such a situation where the void is approximately spherical in shape, lined with a bed of crystals pointing inward.

Pure quartz is colorless or white, colored varieties include rose quartz, amethyst, smoky quartz, milky quartz, and others. Quartz goes by an array of different names. The most important distinction between types of quartz is that of macrocrystalline (individual crystals visible to the unaided eye) and the microcrystalline or cryptocrystalline varieties (aggregates of crystals visible only under high magnification). Chalcedony is a generic term for cryptocrystalline quartz. The cryptocrystalline varieties are either translucent or mostly opaque, while the transparent varieties tend to be macrocrystalline.

Although many of the varietal names historically arose from the color of the mineral, current scientific naming schemes refer primarily to the microstructure of the mineral. Color is a secondary identifier for the cryptocrystalline minerals, although it is a primary identifier for the macrocrystalline varieties. This does not always hold true.

{| class="wikitable"
|+ '''Major Varieties'''
|  Chalcedony  || Any cryptocrystalline quartz, although generally only used for white or lightly colored material. Otherwise more specific names are used.
|-----
| Agate        || Multi-colored, banded chalcedony, semi-translucent to translucent
|-----
| [[Onyx (Material)|Onyx]]         || Agate where the bands are straight, parallel and consistent in size.
|-----
| Jasper       || Opaque chalcedony, typically red to brown
|-----
| Aventurine   || Translucent chalcedony with small inclusions (usually mica) that shimmer.
|-----
| Tiger's eye  || Fibrous gold to red-brown coloured quartz, exhibiting chatoyancy].
|-----
| Rock crystal     || Clear, colorless
|-----
| Amethyst     || Purple, transparent
|-----
| Citrine      || Yellow to reddish orange to brown, greenish yellow
|-----
| Prasiolite   || Mint green, transparent
|-----
| Rose quartz  || Pink, translucent, may display asterism 
|-----
| Rutilated quartz || Contains acicular (needles) inclusions of rutile
|----
| Milk quartz  || White, translucent to opaque, may display diasterism
|-----
| Smoky quartz  || Brown to grey, opaque
|----
| Morion        || Dark-brown, opaque
|----
| Carnelian    || Reddish orange chalcedony, translucent
|}

Quartz is found on the planet [[Onyx]]. This was reported on in [[ENGCORP Field Report A79052]].<ref>''[[Halo: Ghosts of Onyx]]'' pg. 124</ref>

A pink quartz monolith was on display at the [[Côte d'Azur Museum of Natural History]] on [[Sigma Octanus IV]]. Upon first engaging two [[Hunter]]s in the room, [[Spartan-II|SPARTAN]] [[Blue Team]] used [[Shredder Rounds]] to blow the floor under the Hunters' feet. When the Hunters fell to the floor below, [[John-117]], [[Kelly-087]], [[Fred-104]], and [[Spartan-James|James]] pushed the quartz monolith onto the Hunters, pinning them.<ref>''[[Halo: The Fall of Reach]]'' pgs. 204-208</ref>

==Sources==
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[[Category:Materials]]