Magadiite is a rare layered silicate mineral primarily found in hypersaline, alkaline lake environments like the Lake Magadi basin. It typically forms delicate white, platy, or rosette-like crystal aggregates that can be visually distinguished by their association with evaporite minerals.
Is this magadiite?
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 magadiite with a known reference. Magadiite sits at Mohs 2, 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 to dull.
- 4Match the color rangeCompare against the expected color range: white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: microscopic crystals, platy, powdery.
Often confused with
Magadiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside magadiite
Minerals reported to co-occur with magadiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaSi₇O₁₃(OH)₃·3H₂O
- Mohs hardness
- 2
- Density
- 2.25 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous to dull
- Transparency
- Translucent to opaque
- Crystal system
- Monoclinic
- Crystal habit
- Microscopic crystals, platy, powdery
- Cleavage
- Perfect
- Fluorescence
- Yellow-white under SW and LW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In silts of upper Pleistocene to recent age, precipitated by evaporation of saline brines (Lake Magadi, Kenya)
Where rockhounds find magadiite
Classic worldwide localities
- Alkali Lake Playa, Lake Co., Oregon, and about five km north of Trinity Lake, Trinity Co., California, USA
- Lake Magadi and Lake Bogoria, Rift Valley, Kenya
- Kanem area, Lake Chad, Chad
- Mont Saint-Hilaire and near Saint-Amable, Quebec, Canada
Field-hunting tip
Where it forms: In silts of upper Pleistocene to recent age, precipitated by evaporation of saline brines (Lake Magadi, Kenya). If you start seeing kenyaite, calcite, kanemite in float, you are in the right ground. Typical habit: microscopic crystals, platy, powdery. Train your eye for that shape before scanning the outcrop.




