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, so Zavalíaite leaves yellow, Vivianite leaves white to light blue.

How to tell apart: Zavalíaite is noticeably harder (Mohs 3 vs. 2); streak differs, so 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, 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.


