Connellite is a rare, striking copper sulfate chloride mineral that typically forms as delicate, needle-like blue sprays or tufts. It is most famous from the mines of Cornwall, England, where it occurs as a secondary mineral in oxidized copper-rich environments. Collectors value it for its vivid blue color and complex, acicular crystalline habit.
Is this connellite?
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 connellite with a known reference. Connellite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Connellite leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Connellite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: bright blue, azure blue, deep blue.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular or fibrous radial sprays, prismatic crystals.
Often confused with
Connellite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside connellite
Minerals reported to co-occur with connellite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₁₉(SO₄)(OH)₃₂Cl₄·3H₂O
- Mohs hardness
- 3
- Density
- 3.4-3.5 g/cm³
- Streak
- Pale Blue
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular or Fibrous Radial Sprays, Prismatic Crystals
- Cleavage
- Good On {10-10}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Copper Ore Deposits
- Typical price
- $20-150 thumbnail, $200+ cabinet specimen
Where rockhounds find connellite
Classic worldwide localities
- Cornwall, England
- Bisbee, Arizona, USA
- Tsumeb, Namibia
- Chuquicamata, Chile
Field-hunting tip
Look in oxidized copper ore deposits country, the host setting where connellite typically forms. If you start seeing cuprite, malachite, brochantite in float, you are in the right ground. Field specimens usually show a acicular or fibrous radial sprays, prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






