Quartzite is a hard, non-foliated metamorphic rock that was originally pure quartz sandstone. It is characterized by its granular, sugary texture and a tendency to fracture across grain boundaries rather than around them, distinguishing it from sandstone.
Is this quartzite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch quartzite with a known reference. Quartzite sits at Mohs 7, softer than the next harder reference, harder than the previous one.
- 2Read the textureLook at a fresh break with a hand lens. Texture: Hard and non-foliated.
- 3Pick out the mineralsComposition: Originally pure quartz sandstone; nearly pure silica. Identify the two or three most abundant grains.
- 4Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 5Match the color rangeCompare against the expected color range: white, gray, pink, red, yellow.
Often confused with
Quartzite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside quartzite
Minerals reported to co-occur with quartzite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 7
- Density
- 2.6-2.7 g/cm³
- Luster
- Vitreous
- Transparency
- Translucent
- Rarity
- Common
- Uses
- Construction, Decorative, Lapidary
- Host rock
- metamorphic terranes
- Texture
- Hard and non-foliated
- Composition
- Originally pure quartz sandstone; nearly pure silica
Where rockhounds find quartzite
7 mapped spotsClassic worldwide localities
- USA
- Brazil
- Norway
- Canada
- United Kingdom
Field-hunting tip
Where it forms: metamorphic terranes. If you start seeing quartz, muscovite, hematite in float, you are in the right ground. In the U.S., the densest reported localities are in Wisconsin, California, New Mexico. Start trip planning there.







