Melanophlogite is a rare, silica-based mineral that crystallizes in the cubic system, which is unusual for common SiO₂ species. Collectors prize it for its sharp, small cube-like crystals and distinct, bright blue-white fluorescence under short-wave ultraviolet light.
Is this melanophlogite?
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 melanophlogite with a known reference. Melanophlogite sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Melanophlogite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Melanophlogite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow, brown.
- 5Look at form & habitCrystal system: cubic. Typical habit: pseudocubic crystals, cube-like, pyritohedral faces.
Often confused with
Melanophlogite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside melanophlogite
Minerals reported to co-occur with melanophlogite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SiO₂
- Mohs hardness
- 6-6.5
- Density
- 2.0-2.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Cubic
- Crystal habit
- Pseudocubic Crystals, Cube-like, Pyritohedral Faces
- Cleavage
- None
- Fluorescence
- Bright Blue-white Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sulfur-bearing Gypsum or Clay Deposits
- Typical price
- $50-500 depending on specimen size and clarity
Where rockhounds find melanophlogite
Classic worldwide localities
- Fortullino, Italy
- Santa Barbara County, California, USA
- Mount Hamilton, California, USA
- Mezzano, Italy
Field-hunting tip
Look in sulfur-bearing gypsum or clay deposits country, the host setting where melanophlogite typically forms. If you start seeing sulfur, calcite, gypsum in float, you are in the right ground. Field specimens usually show a pseudocubic crystals, cube-like, pyritohedral faces habit, so train your eye for that shape before scanning the outcrop.







