Garnet refers to a large group of nesosilicate minerals that share a common crystal structure and general chemical formula. They are most easily identified by their characteristic dodecahedral or trapezohedral crystal forms and occur in a wide variety of metamorphic and igneous environments worldwide.
Spotting garnet in the field
Field marks- 1
Well-formed 12 or 24-sided ball-like crystals, often nearly spherical
- 2
No cleavage, so broken pieces have curved conchoidal surfaces
- 3
Hard at 6.5 to 7.5 and noticeably heavy for its size
Garnet is a group rather than one mineral, and the crystal shape is the family signature: those rounded many-faced balls are unmistakable once you have seen a few. It is a metamorphic mineral above all, so schist, gneiss and skarn are the ground to work, along with the stream gravels below them where garnet concentrates because it is hard and heavy. Weathered schist gives them up freely, and a screen in the creek below an outcrop is often more productive than hammering the rock.
Straight answers
- Is it worth cutting?
- Cuts and facets well, and the harder species take a fine polish. Its hardness and lack of cleavage make it a forgiving stone to learn faceting on.
- What is it really worth?
- Common almandine is cheap. Demantoid, tsavorite and fine spessartine are genuinely valuable.
- Can you legally keep it?
- Widely collectible on public land under ordinary personal-use rules. Some famous localities are commercial operations.
Often confused with
Garnet vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside garnet
Minerals reported to co-occur with garnet. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- X₃Y₂(SiO₄)₃
- Mohs hardness
- 6.5-7.5
- Density
- 3.5-4.3 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Dodecahedral and Trapezohedral Crystals, Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Gemstone, Abrasive, Collector
- Host rock
- Metamorphic Rocks Like Schist and Gneiss, Sometimes Igneous Rocks
- Typical price
- $5-50 thumbnail, $100-5000+ cabinet specimen
Where rockhounds find garnet
197 mapped spotsClassic worldwide localities
- USA
- India
- Madagascar
- Tanzania
- Brazil
- Czech Republic
U.S. states with garnet
Each link opens a state-specific list of mapped rockhounding spots that produce garnet.
- North Carolina43 spots
- Utah25 spots
- Georgia10 spots
- Virginia9 spots
- Idaho8 spots
- Maine8 spots
- Maryland8 spots
- Alabama7 spots
Field-hunting tip
Look in metamorphic rocks like schist and gneiss, sometimes igneous rocks country, the host setting where garnet typically forms. If you start seeing quartz, mica, feldspar in float, you are in the right ground. Field specimens usually show a dodecahedral and trapezohedral crystals, massive habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in North Carolina, Utah, Georgia. Start trip planning there.






