Granite is a coarse-grained, intrusive igneous rock formed primarily from quartz, alkali feldspar, and plagioclase. It is recognized by its speckled appearance of light and dark minerals and is the most common rock of the continental crust, widely used in construction and sculpture.
Is this granite?
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 granite with a known reference. Granite sits at Mohs 6-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Granite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Granite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, pink, red.
- 5Look at form & habitTypical habit: granular.
Often confused with
Granite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside granite
Minerals reported to co-occur with granite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6-7
- Density
- 2.6-2.7 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Common
- Uses
- Decorative, Construction, Architecture, Monumental
- Host rock
- Continental Crust
- Typical price
- $5-50 for slabs and hand specimens
Where rockhounds find granite
1 mapped spotsClassic worldwide localities
- United States
- Brazil
- India
- China
- Norway
Field-hunting tip
Look in continental crust country — that is the host setting where granite typically forms. If you start seeing quartz, feldspar, mica in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Maine — start trip planning there.







