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.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Quartzite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Quartzite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, pink, red, yellow.
- 5Look at form & habitTypical habit: massive.
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
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Construction, Decorative, Lapidary
- Host rock
- Metamorphic Terranes
- Typical price
- $1-20 for decorative slabs or landscaping specimens
Where rockhounds find quartzite
7 mapped spotsClassic worldwide localities
- USA
- Brazil
- Norway
- Canada
- United Kingdom
Field-hunting tip
Look in metamorphic terranes country, the host setting where quartzite typically forms. If you start seeing quartz, muscovite, hematite in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Wisconsin, California, New Mexico. Start trip planning there.





