Melanterite is a secondary sulfate mineral typically formed by the oxidation of iron sulfides like pyrite in damp mine environments. It is characterized by its bright green color and sweet, astringent taste, though it is highly unstable and will crumble into a white powder if exposed to dry air for too long.
Is this melanterite?
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 melanterite with a known reference. Melanterite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Melanterite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Melanterite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellowish-green, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, stalactitic, or massive crusts.
Often confused with
Melanterite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside melanterite
Minerals reported to co-occur with melanterite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeSO₄·7H₂O
- Mohs hardness
- 2
- Density
- 1.89 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, Stalactitic, Or Massive Crusts
- Cleavage
- Distinct On (001)
- Rarity
- Common
- Uses
- Collector, Educational
- Host rock
- Oxidized Zones of Iron-rich Ore Deposits
- Typical price
- $10-60 for small mineral specimens
Where rockhounds find melanterite
4 mapped spotsClassic worldwide localities
- Rio Tinto, Spain
- Goslar, Germany
- Chuquicamata, Chile
- Bisbee, Arizona
Field-hunting tip
Look in oxidized zones of iron-rich ore deposits country — that is the host setting where melanterite typically forms. If you start seeing pyrite, chalcopyrite, copiapite in float, you are in the right ground. Field specimens usually show a fibrous, stalactitic, or massive crusts habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Missouri, Arizona — start trip planning there.







