Santanaite is an extremely rare lead chromate mineral found primarily in the oxidized zones of lead mines. It typically occurs as small, straw-yellow tabular crystals or crusts associated with other lead-bearing secondary minerals. Due to its rarity and specific chemical requirements for formation, it is highly prized by advanced mineral collectors.
Is this santanaite?
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 santanaite with a known reference. Santanaite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Santanaite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Santanaite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: straw-yellow.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals, crusts.
Often confused with
Santanaite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Santanaite leaves yellow, Phoenicochroite leaves orange-yellow.

How to tell apart: Streak differs, so Santanaite leaves yellow, Wulfenite leaves white; luster reads adamantine on Santanaite and resinous to subadamantine to adamantine on Wulfenite.
Often found alongside santanaite
Minerals reported to co-occur with santanaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₁₁CrO₁₆
- Mohs hardness
- 2.5
- Density
- 9.15 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Tabular Crystals, Crusts
- Cleavage
- {0001} and {1120}, Very Good; {1010}, Rare
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-bearing Ore Deposits
Where rockhounds find santanaite
Classic worldwide localities
- San Rafael mine, Chile
Field-hunting tip
Look in oxidized lead-bearing ore deposits country, the host setting where santanaite typically forms. If you start seeing linarite, galena, anglesite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts habit, so train your eye for that shape before scanning the outcrop.



