Zavalíaite is a rare cadmium phosphate mineral known primarily from its type locality in Argentina. It typically occurs as small, yellow granular masses within phosphate-rich zones of pegmatites.
Is this zavalíaite?
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 zavalíaite with a known reference. Zavalíaite sits at Mohs 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Zavalíaite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Zavalíaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular aggregates.
Often confused with
Zavalíaite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Zavalíaite is noticeably harder (Mohs 3 vs. 1.5-2); streak differs — Zavalíaite leaves yellow, Vivianite leaves white to light blue.

How to tell apart: Zavalíaite is noticeably harder (Mohs 3 vs. 2); streak differs — Zavalíaite leaves yellow, Bobierrite leaves white; luster reads vitreous on Zavalíaite and pearly on Bobierrite.
Often found alongside zavalíaite
Minerals reported to co-occur with zavalíaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cd₃(PO₄)₂
- Mohs hardness
- 3
- Density
- 3.32 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Granular Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Pegmatites
- Typical price
- $50-300 per specimen
Where rockhounds find zavalíaite
Classic worldwide localities
- Zavalía, Argentina
Field-hunting tip
Look in pegmatites country — that is the host setting where zavalíaite typically forms. If you start seeing apatite, triplite in float, you are in the right ground. Field specimens usually show a granular aggregates habit, so train your eye for that shape before scanning the outcrop.


