The Major Varieties of Quartz (Photos)
There are many different varieties of quartz, several of which are semi-precious gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Europe and the Middle East.
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The Major Varieties of Quartz |
Some macrocrystalline (large crystal) varieties are well known and popular as ornamental stone and as gemstones.
- Amethyst is the purple gemstone variety.
- Citrine is a yellow to orange gemstone variety that is rare in nature but is often created by heating Amethyst.
- Milky Quartz is the cloudy white variety.
- Prasiolite is a leek-green gemstone variety that is rare in nature but is created by heating Amethyst from certain locations.
- Rose quartz is a pink to reddish pink variety.
- Smoky quartz is the brown to gray variety.
The primary varieties of chalcedony are as follows:
- Agate is a banded variety (sometimes with translucent bands)
- Bloodstone is green with red speckles
- Carnelian is yellow to orange
- Chrysoprase is green
- Flint is generally black with a fibrous microscopic structure
- Jasper is any colorful agate
- Onyx is black, white, or alternating black and white
- Sard is yellow to brown
- Sardonyx is banded, alternating sard and (usually white) onyx
The primary varieties of quartz
Agate
Agate Multi-colored, banded chalcedony, semi-translucent to translucen. Although agates may be found in various kinds of rock, they are classically associated with volcanic rocks and can be common in certain metamorphic rocks.
Onyx
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onyx contain bands of black and/or white. Copyright © Rob Lavinsky |
Onyx Agate where the bands are straight, parallel and consistent in size. A typical onyx consists of two or more black and white strata.
Jasper
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Rough of Kaleidoscope Jasper from Oregon |
Jasper Opaque cryptocrystalline quartz, typically red to brow. The common red color is due to iron(III) inclusions. The mineral aggregate breaks with a smooth surface and is used for ornamentation or as a gemstone.
Tiger's eye
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Polished tiger's eye gemstone |
Tiger's eye is a chatoyant gemstone that is usually a metamorphic rock with a golden to red-brown color and a silky lustre. As members of the quartz group, tiger's eye and the related blue-colored mineral hawk's eye gain their silky, lustrous appearance from the parallel intergrowth of quartz crystals and altered amphibole fibers that have mostly turned into limonite. It is a classic example of pseudomorphous replacement by silica of fibrous crocidolite (blue asbestos). An incompletely silicified blue variant is known as hawk's eye.
Amethyst
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Amethyst Photo by @luminous.element |
Rutilated quartz
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Quartz with Rutile inclusions from Novo Horizonte, Bahia, Northeast Region, Brazil Copyright © Rob Lavinsky |
Rutilated quartz is a type of quartz that contains acicular (needle-like) inclusions of rutile. It is used for gemstones. These inclusions mostly look golden, but they also can look silver, copper red or deep black. They can be distributed randomly or in bundles, which sometimes are arranged star-like, and they can be sparse or dense enough to make the quartz body nearly opaque. While otherwise inclusions often reduce the value of a crystal, rutilated quartz is valued for the quality and beauty of these inclusions.
Citrine
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Giant Citrine faceted gem from Minas Gerais, Brazil. |
Citrine is a variety of quartz whose color ranges from a pale yellow to brown due to ferric impurities. Natural citrines are rare; most commercial citrines are heat-treated amethysts or smoky quartzes.
Prasiolite
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Raw natural prasiolite
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Prasiolite (or vermarine) is the name for any quartz crystal or cluster that is green in color. It is a rare stone in nature; artificially produced Prasiolite is heat treated amethyst.
Rose quartz
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Rose quartz |
Rose quartz Pink, translucent, may display diasteris. The color is usually considered as due to trace amounts of titanium, iron, or manganese, in the massive material.
Milky Quartz
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Milky Quartz Cluster
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Milky Quartz is any quartz crystal or cluster that is white in color and cloudy. The cloudy white character of the crystals is what lead to the variety name, milky. Milky quartz is the most common variety of crystalline quartz. The white color is caused by minute fluid inclusions of gas, liquid, or both, trapped during crystal formation, making it of little value for optical and quality gemstone applications
Smoky quartz
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Amazonite, Smoky Quartz with Goethite Onegite from Colorado, USA Photo : © Dorrisfamily |
Smoky quartz is the brown to black, and sometimes smoky gray version of quartz. It ranges in clarity from almost complete transparency to a brownish-gray crystal that is almost opaque. Smoky quartz, a variety itself of quartz, has a few varieties of its own. Read about it here.
Carnelian
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Polished Carnelian |
Carnelian Reddish orange chalcedony, translucen. The color can vary greatly, ranging from pale orange to an intense almost-black coloration. Similar to carnelian is sard, which is generally harder and darker.
Chalcedony
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Chalcedony |
vChalcedony is a cryptocrystalline quartz and moganite mixture. The term is generally only used for white or lightly colored material. Otherwise more specific names are used. 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.
Mtorolite
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Mtorolite zimbabwe |
Mtorolite is a green variety of chalcedony, which has been colored by chromium. Also known as chrome chalcedony, it is principally found in Zimbabwe.
Chrysoprase
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(chrysoprase). An amazing new find from Australia. Photo by: Australian Outback Mining |
Heliotrope
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Heliotrope photo courtesy of R. Weller
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Heliotrope is a green variety of chalcedony, containing red inclusions of iron oxide that resemble drops of blood, giving heliotrope its alternative name of bloodstone.
See also How Do Agates Form?
Types of agate with photos
Types of Mineral Inclusions with Photos
Why Fluorite Comes in Different Colors? With Examples