Types of Quartz: The Complete Variety Guide
By The Any Rock Identifier Team · Published 26 June 2026
The types of quartz split into two families. Macrocrystalline quartz grows crystals big enough to see, and it includes amethyst, citrine, rose quartz, smoky quartz, clear rock crystal, milky quartz, rutilated quartz and prasiolite. Cryptocrystalline quartz, also called chalcedony, is built from crystals too small for the eye, and it covers agate, jasper, carnelian, onyx and plain chalcedony. Every one of them is the same mineral underneath, silicon dioxide, so the differences come down to crystal size, trace impurities and how the stone formed.
That single mineral is the most abundant in the Earth's crust, which is why quartz turns up in so many shapes and colors that it can look like a dozen separate stones. This guide walks through what makes a quartz a quartz, the macrocrystalline varieties and the color cause behind each, the chalcedony family, and the quick tests that tell quartz apart from glass and calcite.
What makes a quartz a quartz
Quartz is silicon dioxide, written SiO₂, a framework of silicon and oxygen atoms locked in a rigid lattice. That structure gives every variety the same core properties no matter what it is called or what color it shows.
Three traits do most of the identifying work. Quartz sits at 7 on the Mohs hardness scale, hard enough to scratch glass and steel. It has no cleavage, so it does not split along flat planes the way calcite or feldspar do. Instead it breaks with a conchoidal fracture, the smooth curved shell-like surface you also see in flint and glass. It is also fairly light for a mineral, with a specific gravity near 2.65, and it leaves no streak on a porcelain tile.
Hold those four facts together, hardness 7, no cleavage, conchoidal fracture and a glassy luster, and you have the signature that runs through every entry below. The varieties differ in appearance; the mineral does not.
For the full mineral data, the Quartz reference on Mindat lists every documented property and locality.
The macrocrystalline types
Macrocrystalline quartz forms crystals you can see, often as six-sided prisms ending in a point. The colors come almost entirely from trace impurities and natural radiation acting on the silica, which is why one mineral produces purple, yellow, pink, gray and clear stones. These are the varieties most people picture when they hear the word crystal.
- Amethyst (purple) — the most prized quartz variety. Its violet color comes from trace iron plus natural irradiation deep in the host rock. Strong heat turns most amethyst yellow or orange, which is how a lot of commercial citrine is actually made.
- Citrine (yellow to orange) — colored by iron in a slightly different state. Genuine citrine is uncommon in nature, so most on the market is heat-treated amethyst; natural stone tends toward an even pale lemon, heated stone toward bright orange tips.
- Rose quartz (pink) — the soft, often cloudy pink comes from microscopic fibers of a borosilicate mineral threaded through the quartz. Rose quartz usually grows in massive form rather than clean points, which is why faceted pieces are rare.
- Smoky quartz (brown to gray-black) — the smoky tone comes from natural radiation acting on tiny amounts of aluminum in the lattice. Smoky quartz ranges from a light tea color to near black, and gem-quality dark stones are sometimes sold as morion.
- Clear quartz (colorless) — pure silica with no coloring impurity, also called rock crystal. Clear quartz is the textbook six-sided point and the reference everything else is compared against.
- Milky quartz (white) — the most common form, clouded white by countless microscopic fluid and gas bubbles trapped as it grew. It is the milky vein quartz you see running through granite and quartzite.
- Rutilated quartz — clear or smoky quartz shot through with golden or coppery needles of rutile, a titanium oxide. The needles formed alongside the quartz and are prized for the web of fine lines they create inside the stone.
- Prasiolite (leek-green) — a pale green quartz, almost always produced by heating or irradiating amethyst, since natural green quartz is very rare. Sometimes labeled green amethyst, though that name is a misnomer.
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The cryptocrystalline (chalcedony) types
Chalcedony is quartz built from crystals so small they cannot be resolved by eye, sometimes called cryptocrystalline or microcrystalline quartz. Because the grains are tiny and tightly packed, these stones look waxy or glassy rather than crystalline, take a high polish, and come in solid colors, bands and patterns instead of distinct points. They formed from silica-rich water seeping into cavities and cracks, often layer by layer.
Chalcedony itself is the umbrella term and also the name for the plain, translucent gray-to-blue or white material. The well-known stones below are all members of the family.
- Agate — banded chalcedony, where successive layers of silica deposited in a cavity create the concentric stripes and eyes. The bands can be natural earth tones or, in cheap decorative slices, dyed in vivid colors.
- Jasper — opaque chalcedony heavily stained by iron and other minerals, giving solid reds, browns, yellows and greens, often in mottled or picture-like patterns. The opacity and earthy color set it apart from translucent agate.
- Carnelian — translucent chalcedony in warm orange to deep red, colored by iron oxide. It grades into the browner sard, and the line between the two is loose.
- Onyx — chalcedony with straight, parallel bands rather than the curved bands of agate. True onyx is black and white; the solid black version is the most familiar in jewelry.
- Chalcedony (plain) — the base material itself, usually a soft translucent blue, gray or white with a smooth waxy sheen and no banding or pattern.
How to tell quartz from look-alikes
Two materials fool people most often: glass and calcite. The properties from the first section settle both cases quickly.
Glass mimics clear and colored quartz, especially in tumbled stones and beads. The fastest tells are temperature and bubbles. Quartz is dense and pulls heat from your skin, so it feels cold and warms slowly; glass warms fast in the hand. Hold the piece to a bright light and look for trapped round bubbles, a dead giveaway for poured glass, since natural quartz inclusions are angular or needle-like, never neat spheres. Hardness confirms it: quartz at 7 scratches glass, and glass near 5.5 cannot scratch quartz.
Calcite is the classic mineral mix-up, because clear calcite and clear quartz can look alike on a shelf. Two properties separate them cleanly. Calcite is much softer, at 3 on the Mohs scale, so a steel knife or even a copper coin marks it while quartz is untouched. Calcite also has perfect cleavage and splits into neat rhombs with flat faces, whereas quartz has no cleavage and breaks with a curved conchoidal fracture. A drop of vinegar fizzes on calcite and does nothing on quartz.
When a photo is all you have, an AI crystal identifier reads the color, luster and crystal form and flags likely look-alikes, which points you to the right physical test instead of a guess. Confirm anything valuable with a hardness or fracture check in person, since a picture cannot measure either.
Value notes
Quartz is common, so most varieties are affordable, and that is part of the appeal. Clear, milky and smoky quartz are inexpensive even in large pieces. Amethyst and citrine carry a modest premium for strong, even color, and deep-purple amethyst from a few classic localities fetches the most among the everyday types.
A few things lift price beyond the variety itself. Rutilated quartz with fine, well-arranged golden needles is sought after. Natural untreated citrine commands more than the heated kind once it is verified. Among chalcedony, fine agate, vivid carnelian and well-patterned jasper are valued for the pattern and polish rather than rarity of the mineral.
Treatment matters more than name. Heated amethyst sold as citrine, dyed agate and irradiated prasiolite are still real quartz, but they should be priced and disclosed as treated. The stone is genuine; the only issue is a seller who hides the enhancement. For the wider context on quartz varieties and their naming, the Quartz entry on Wikipedia is a solid reference. If you want to see how the named varieties fit into the bigger picture, our guide to the types of crystals groups them alongside the other mineral families.
Frequently asked questions
What are the main types of quartz?
Quartz splits into two families. Macrocrystalline quartz has visible crystals and includes amethyst, citrine, rose quartz, smoky quartz, clear rock crystal, milky quartz, rutilated quartz and prasiolite. Cryptocrystalline quartz, or chalcedony, has microscopic crystals and includes agate, jasper, carnelian, onyx and plain chalcedony. All of them are the same mineral, silicon dioxide.
What gives each type of quartz its color?
Trace impurities and natural radiation. Amethyst is purple from iron plus irradiation, citrine is yellow from iron, smoky quartz is brown from radiation acting on aluminum, and rose quartz is pink from microscopic mineral fibers. Pure quartz with no impurity is colorless clear quartz, and milky white quartz gets its cloud from countless tiny trapped bubbles.
Is amethyst a type of quartz?
Yes. Amethyst is the purple variety of macrocrystalline quartz, the same silicon dioxide as clear quartz but colored violet by trace iron and natural irradiation. Heating most amethyst turns it yellow or orange, which is how a large share of commercial citrine is actually produced.
Is agate a type of quartz?
Yes. Agate is a banded form of chalcedony, which is cryptocrystalline quartz, meaning quartz built from crystals too small to see. The concentric bands form as silica-rich water deposits layer after layer inside a rock cavity. Jasper, carnelian and onyx belong to the same chalcedony family.
How can I tell real quartz from glass?
Use temperature, bubbles and hardness. Quartz feels cold and warms slowly because it is dense; glass warms fast in the hand. Held to a light, glass often shows round trapped bubbles, while quartz inclusions are angular or needle-like. Quartz is hardness 7 and scratches glass, whereas glass near 5.5 cannot scratch quartz.
What is the difference between quartz and calcite?
Hardness and cleavage. Quartz is hardness 7 with no cleavage and breaks with a curved conchoidal fracture. Calcite is much softer at 3, so a steel knife marks it easily, and it has perfect cleavage that splits it into flat-faced rhombs. A drop of vinegar fizzes on calcite and does nothing on quartz.
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