Warwickite is a rare borate mineral that typically forms elongated or prismatic dark-colored crystals in metamorphosed limestones. It is most famous for its occurrence in the contact metamorphic zones of the New York Highlands, where it appears alongside various magnesium-rich silicates.
Is this warwickite?
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 warwickite with a known reference. Warwickite sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Warwickite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Warwickite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black, dark brown, reddish-brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, elongated, acicular.
Often confused with
Warwickite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside warwickite
Minerals reported to co-occur with warwickite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Ti,Fe³⁺,Al)₂(O,OH)BO₃
- Mohs hardness
- 3-4
- Density
- 3.36-3.41 g/cm³
- Streak
- Black
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic Crystals, Elongated, Acicular
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Limestone, Skarn Deposits
- Typical price
- $20-150 per specimen
Where rockhounds find warwickite
Classic worldwide localities
- Warwick, New York, USA
- Amity, New York, USA
- Glenelg, Scotland
- Ladoga Lake, Russia
Field-hunting tip
Look in metamorphosed limestone, skarn deposits country — that is the host setting where warwickite typically forms. If you start seeing spinel, calcite, serpentine in float, you are in the right ground. Field specimens usually show a prismatic crystals, elongated, acicular habit, so train your eye for that shape before scanning the outcrop.







