Coquimbite is a hydrated iron(III) sulfate, Fe2(SO4)3·9H2O, found as purple, red-violet or pink crusts and drusy crystal mats. Its most useful identifying trait is softness: at Mohs 2.5 it scratches easily and the crystal layer can rub off, unlike similarly colored quartz. It is named for the Coquimbo region of Chile.
Most commonly confused with
- Amethyst: Amethyst is much harder quartz and usually has glassy transparent to translucent crystals rather than soft sulfate crusts.
- Erythrite: Erythrite is typically brighter pink to crimson and commonly forms radiating or fibrous cobalt-arsenate aggregates.
- Kornelite: Kornelite is another hydrated iron sulfate that may appear pinkish to violet but has different chemistry and crystal forms.
- Alunogen: Alunogen is usually white to pale and fibrous or crusty, lacking the stronger violet to red-violet tone typical of many coquimbite specimens.
Coquimbite vs. Common Lookalikes
| Mineral | Typical color | Key difference | Durability |
|---|---|---|---|
| Coquimbite | Purple to red-violet | Hydrated ferric sulfate; often fragile crusts or trigonal crystals | Soft and water-sensitive |
| Amethyst | Purple | Quartz with glassy luster and much higher hardness | Durable |
| Erythrite | Pink to crimson | Cobalt arsenate, often fibrous or radiating | Soft and fragile |
| Kornelite | Pale violet to pinkish | Hydrated iron sulfate with different composition | Soft and moisture-sensitive |
| Alunogen | White to pale pink | Aluminum sulfate, commonly fibrous or powdery | Very fragile |
Advanced recommendations
- Coquimbite
- Kornelite
- Erythrite
Buying and Authenticity Checks
A credible coquimbite listing should include locality, specimen size, clear natural-light photos, and notes about storage conditions. Be cautious of listings that use only broad labels such as “purple crystal” or “healing stone” without mineral data. Because coquimbite is soft and moisture-sensitive, intact sharp crystals or clean crusts from documented localities are more meaningful than polished shapes.
Photo Tips for Identification
Photograph coquimbite in indirect natural light on a neutral background to avoid exaggerating violet or red tones. Include close-up images of crystal surfaces, the underside or matrix, and any associated minerals. A scale reference such as a ruler helps distinguish tiny sulfate crusts from larger quartz crystals.
Locality Clues
Coquimbite is commonly associated with arid mine environments and oxidation zones where iron sulfates can form. Specimens may occur with other sulfate minerals, so a locality label can be an important part of identification. Locality alone does not prove identity, but it can narrow the list of likely lookalikes.
What Is Coquimbite?
Coquimbite is a hydrated iron(III) sulfate mineral, Fe2(SO4)3·9H2O. It most often occurs as crusty coatings or drusy, sparkling crystal mats in purple, red-violet or pinkish shades. The color can look artificial until the piece is tilted under a lamp and the crystal faces catch the light. The color is natural.
A specimen lacks the heft of quartz and feels lighter in the hand. The edges can be chalky, and the crystal crust can shed when rubbed with a thumb. In some specimens the strongest color is only a thin, sugary skin over dull brown gossan, and that contrast is part of the mineral's appeal.
Most collection pieces are cabinet specimens, not something you toss in your pocket. It’s soft, it doesn’t like humidity swings, and if you treat it like a tough carry-around stone you’ll end up with purple dust in the bag. Why risk it?
Origin & History
Chile’s right there in the name. Coquimbite got its first proper description in 1841 from August Breithaupt, and the species name points straight to the Coquimbo region in northern Chile, where people first recognized the material.
Collectors often use the name coquimbite loosely in the field, because it occurs with other hydrated iron sulfates that can look nearly identical at a glance. The underlying origin is the same oxidized-zone chemistry: iron sulfides break down, sulfate-rich water moves through the rock, and hydrated sulfates grow in place as conditions alternate between wet and dry.
Where Is Coquimbite Found?
It turns up in arid to semi-arid oxidized mine settings and volcanic fumarolic areas where sulfate-rich fluids evaporate and rehydrate repeatedly.
Formation
At first glance, coquimbite looks like something cooked up in a lab. But it’s actually a pretty natural setup: iron, sulfate, and a whole lot of water locked into the structure. It forms as a secondary mineral in the oxidation zones of sulfide deposits, especially where pyrite and other iron sulfides weather, and the runoff turns acidic and loaded with sulfate.
Its habitat explains its behavior. Coquimbite is a salt-type mineral that crystallizes from evaporating solutions on mine walls, in fractures, or as a druse on gossan. It changes hydration state when humidity shifts, so a specimen that looks crisp and sparkling one day can become dull and powdery a season later, as if left near damp air. Hydrated sulfates like this record the conditions of their environment directly.
How to Identify Coquimbite
Color: Usually purple to red-violet, sometimes pinkish or lilac; paler material can look almost whitish with a purple cast. Color is often strongest in drusy coatings and fades toward the matrix.
Luster: Vitreous to pearly on fresh crystals, turning dull as it powders or dehydrates.
If you scratch it with a copper penny, it’ll usually mark because it’s soft. The real test is the feel: real coquimbite stays cool like a mineral, but the surface can feel slightly sugary and fragile, like a thin crust that doesn’t want to be handled. And don’t lick it or taste it like old-timers did with “salts”. It’s a sulfate and you don’t need that in your life.
Common Look-Alikes
Coquimbite is sometimes confused with these materials:
- Purpurite (massive purple crusts and earthy coatings that get lumped together with “purple sulfate” material)
- Amethyst druzy/quartz coated with purple dye (the dye loves the tiny drusy pits and fractures)
- Lepidolite mica flakes in lilac-purple (sparkly, but it’s platy and greasy-feeling instead of a sugary crust)
- Cobaltoan calcite (hot pink druse, usually on dark matrix, but it’s a carbonate and behaves way differently in water)
- Purple botryoidal chalcedony or dyed agate “druzy” (often sold as bright purple crystal mats)
- Purple glass “druzy” or resin-coated clusters (too uniform, warm in the hand, and the sparkle looks like glitter)
Market Cautions & Treatments
Properties of Coquimbite
Physical Properties
| Crystal System | Trigonal |
| Hardness (Mohs) | 2.5 (Soft (2-4)) |
| Density | 2.10-2.20 g/cm3 |
| Luster | Vitreous |
| Diaphaneity | Transparent to translucent |
| Fracture | Uneven |
| Streak | White |
| Magnetism | Non-magnetic |
| Colors | Purple, Red-violet, Pink, Lilac, Colorless, White |
Chemical Properties
| Classification | Sulfates |
| Formula | Fe2(SO4)3·9H2O |
| Elements | Fe, S, O, H |
| Common Impurities | Al, Mg, Mn |
Optical Properties
| Refractive Index | 1.52-1.55 |
| Birefringence | 0.020 |
| Pleochroism | Weak |
| Optical Character | Uniaxial |
Coquimbite Health & Safety
Handle it gently, and try not to kick up any dust. And don’t drop it into drinking water or use it in elixirs, because it can dissolve and make the water more acidic.
Safety Tips
Wash your hands after you handle it. Keep it where kids and pets can’t get to it. And don’t brush or scrape the surface, since even a “gentle” brush can grind little bits in; if you need to clear off debris, use a soft air puffer (the kind that gives a light puff of air) instead of a stiff brush.
Coquimbite Value & Price
Price Range
Rough/Tumbled: $20 - $250 per specimen
Price follows color and how “fresh” the piece still looks. A bright purple druse with sharp, clean trigonal crystals (the kind that catch light on those flat little faces when you tilt it in your hand) and a stable storage history will sell for more than crumbly coatings or material that’s brown-stained and patchy.
Durability
Fragile — Scratch resistance: Poor, Toughness: Poor
It can dehydrate or break down in dry heat, and it can soften or shed in high humidity, so stability depends a lot on storage.
How to Care for Coquimbite
Use & Storage
Store it in a padded specimen box so it cannot rattle. Keep it in a cabinet away from sunny windows, because heat and dry air can roughen the crystal crust over time.
Cleaning
1) Skip water and chemicals. 2) Use a bulb air blower to remove loose dust. 3) If grit is stuck, nudge it with a very soft artist brush while supporting the matrix so the crust doesn’t flake.
Cleanse & Charge
For a metaphysical reset, use smoke, sound, or a dry selenite plate nearby rather than rinsing. Keep sessions short if you’re using any heat-producing light source.
Placement
Best as a shelf or cabinet specimen where nobody’s going to touch it every day. If you display it, keep it away from bathrooms and kitchen steam.
Caution
Don’t soak it. If you do, it can partly dissolve and you’ll end up with crystals shedding off. And keep it away from big humidity swings. Don’t tumble it, and don’t try to polish it either.
Works Well With
Uses, Symbolism and Collecting Notes
Coquimbite has no long history as a talisman or jewelry stone. Its fragility keeps it in the cabinet specimen category, where it is valued for color and crystal sparkle against brown gossan. It was described in 1841 by August Breithaupt, and its name refers to the Coquimbo region of northern Chile. Collectors tend to treat it as a display piece, kept in a padded box away from sunny windows, heat and humidity swings.
Crystal traditions link coquimbite with the Third Eye and Crown chakras and with the signs Virgo and Aquarius, and list Earth and Storm as its elements. Practitioners who use it generally treat it as a visual focus placed where it can be seen, rather than a stone to hold, because repeated handling wears away the crystal crust. These are cultural beliefs, not proven effects, and they do not replace medical care or professional help for anxiety, sleep problems or other health concerns.
Common mistakes
- Assuming every purple mineral is amethyst or every pale violet crust is coquimbite.
- Testing a specimen with water, which can damage hydrated sulfate minerals.
- Buying polished coquimbite without questioning whether the label is accurate.
- Ignoring matrix and associated minerals, which often provide important identification clues.
- Relying on color alone instead of checking hardness, luster, habit, and locality.
- Storing the specimen in a humid case or near materials that may release moisture.
Identify Coquimbite from a photo
Compare Coquimbite traits, care tips, value clues, and common lookalikes with a clear photo.