Caswellsilverite is an extremely rare sulfide mineral found almost exclusively in enstatite achondrite meteorites. It typically occurs as microscopic inclusions or small anhedral grains associated with other sulfides and pyroxenes. Due to its extraterrestrial origin and scarcity, it is highly sought after by meteorite collectors.
Is this caswellsilverite?
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 caswellsilverite with a known reference. Caswellsilverite sits at Mohs 1-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: yellow gray.
- 5Look at form & habitCrystal system: trigonal. Typical habit: anhedral grains.
Often confused with
Caswellsilverite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside caswellsilverite
Minerals reported to co-occur with caswellsilverite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCrS₂
- Mohs hardness
- 1-2
- Density
- 3.21 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Anhedral grains
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As inclusions in enstatite crystals and in the brecciated matrix of a meteorite (Norton County meteorite); between coarse pyroxene grains in chondrules in a meteorite (Qingzhen meteorite)
Where rockhounds find caswellsilverite
Classic worldwide localities
- In the Norton County enstatite achondrite and the Qingzhen enstatite chondrite meteorites (type locality)
Field-hunting tip
Where it forms: As inclusions in enstatite crystals and in the brecciated matrix of a meteorite (Norton County meteorite); between coarse pyroxene grains in chondrules in a meteorite (Qingzhen meteorite). If you start seeing enstatite, cronusite, daubréelite in float, you are in the right ground. Typical habit: anhedral grains. Train your eye for that shape before scanning the outcrop.






