Metahaiweeite is a rare secondary uranium silicate typically found as yellow, radiating bladed aggregates or thin crusts in sedimentary deposits. It is best identified by its strong green fluorescence under ultraviolet light and its close association with silica-rich lake beds.
Is this metahaiweeite?
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 metahaiweeite with a known reference. Metahaiweeite sits at Mohs 2-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Metahaiweeite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Metahaiweeite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: radiating aggregates, platy crystals, crusts.
Often confused with
Metahaiweeite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Metahaiweeite is noticeably harder (Mohs 2-3 vs. 1).

How to tell apart: Streak differs — Metahaiweeite leaves white, Autunite leaves pale yellow.

How to tell apart: Streak differs — Metahaiweeite leaves white, Meta-autunite leaves yellow.
Often found alongside metahaiweeite
Minerals reported to co-occur with metahaiweeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(UO₂)₂(Si₂O₅)₂·nH₂O
- Mohs hardness
- 2-3
- Density
- 2.8 g/cm³
- Colors
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Radiating Aggregates, Platy Crystals, Crusts
- Cleavage
- Perfect
- Fluorescence
- Bright Green Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Lake Beds
- Typical price
- $20-150 thumbnail
Where rockhounds find metahaiweeite
Classic worldwide localities
- Coso Mountains, California, USA
- Haiwee Reservoir, California, USA
- Utah, USA
Field-hunting tip
Look in sedimentary lake beds country — that is the host setting where metahaiweeite typically forms. If you start seeing opal, quartz, uranophane in float, you are in the right ground. Field specimens usually show a radiating aggregates, platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.



