Anglesite is a secondary mineral formed by the oxidation of lead-rich ore deposits, most notably galena. Collectors value it for its high brilliance and distinct adamantine luster, though its softness and perfect cleavage make it fragile. It is most commonly found in the oxidation zones of mines alongside cerussite and other lead-rich secondary minerals.
Is this anglesite?
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 anglesite with a known reference. Anglesite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Anglesite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Anglesite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: colorless, white, yellow, gray, blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular, prismatic, or blocky crystals; also granular or massive.
Often confused with
Anglesite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside anglesite
Minerals reported to co-occur with anglesite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbSO₄
- Mohs hardness
- 2.5-3
- Density
- 6.3-6.4 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular, Prismatic, Or Blocky Crystals; Also Granular or Massive
- Cleavage
- Good in 3 Directions
- Fluorescence
- Bright Yellow Under SW UV
- Rarity
- Common
- Uses
- Collector, Scientific Research
- Host rock
- Oxidized Zones of Lead-bearing Ore Deposits
- Typical price
- $10-50 for small specimens, $100-500+ for high-quality crystals
Where rockhounds find anglesite
14 mapped spotsClassic worldwide localities
- Anglesey, Wales
- Tsumeb, Namibia
- Broken Hill, Australia
- Touissit, Morocco
- Arizona, USA
Field-hunting tip
Look in oxidized zones of lead-bearing ore deposits country — that is the host setting where anglesite typically forms. If you start seeing galena, cerussite, pyromorphite in float, you are in the right ground. Field specimens usually show a tabular, prismatic, or blocky crystals; also granular or massive habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Missouri, North Carolina — start trip planning there.







