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, 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.







