Londonite is a rare cesium-dominant member of the rhodizite group, typically found as small, sharp dodecahedral crystals in highly evolved pegmatites. It is visually indistinguishable from its potassium-rich counterpart rhodizite without chemical analysis, though londonite is generally rarer. Collectors prize these hard, lustrous crystals for their exceptional clarity and high-index brilliance.
Is this londonite?
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 londonite with a known reference. Londonite sits at Mohs 8, 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: white, colorless, yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: euhedral crystals.
Often confused with
Londonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside londonite
Minerals reported to co-occur with londonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CsBe₅Al₄B₁₁O₂₈
- Mohs hardness
- 8
- Density
- 3.34 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Cubic
- Crystal habit
- Euhedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- An uncommon component of granite pegmatites, in the central zones and in miarolitic cavities
Where rockhounds find londonite
Classic worldwide localities
- Antandrokomby, near Mt. Bity, Manandona Valley, Antsirabe district, Madagascar
- Antsongombato and Ampanivana, south of Mahaiza, and from Manjaka, Betafo region, Madagascar
Field-hunting tip
Where it forms: An uncommon component of granite pegmatites, in the central zones and in miarolitic cavities. If you start seeing rhodizite, danburite, elbaite–liddicoatite–schorl in float, you are in the right ground. Typical habit: euhedral crystals. Train your eye for that shape before scanning the outcrop.




