Meliphanite is a rare beryllium silicate mineral that typically forms yellowish, tabular crystals in alkaline igneous environments. It is most frequently encountered by collectors in association with nepheline syenite pegmatites, where it can be distinguished from the very similar leucophanite by its slightly different crystal morphology and optical properties.
Is this meliphanite?
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 meliphanite with a known reference. Meliphanite sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow, colorless, yellowish red, red.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic, tabular.
Often confused with
Meliphanite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside meliphanite
Minerals reported to co-occur with meliphanite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄(Na,Ca)₄Be₄AlSi₇O₂₄(F,O)₄
- Mohs hardness
- 5-5.5
- Density
- 3.01-3.02 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic, tabular
- Cleavage
- Distinct on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In augite syenite (Fredriksvärn, Norway)
Where rockhounds find meliphanite
Classic worldwide localities
- Iron Mountain No. 2 mine, near Brown City, Sierra Co., New Mexico, USA
- Tvedalen, near Larvik, Norway
- Sakhariok massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: In augite syenite (Fredriksvärn, Norway). If you start seeing natrolite, mica, fluorite in float, you are in the right ground. Typical habit: prismatic, tabular. Train your eye for that shape before scanning the outcrop.





