Coquimbite

3 in the gallery

Coquimbite is a hydrated ferric aluminum sulfate mineral in the sulfate family. It typically forms as colorless to yellow, gray, or pinkish crystals that can be transparent to translucent, with a vitreous luster and a prismatic, tabular, or granular habit. It is notably unstable, often converting to other hydrated sulfates when exposed to drying or heat, which influences how specimens are collected and stored. Specimens commonly show perfect cleavage and a conchoidal to uneven fracture, with a relatively low hardness around 2 to 2.5 on the Mohs scale, and a modest specific gravity near 2.1. Chrome‑bright or pale tints can appear due to trace impurities, and crystals may be relatively small but can form aggregates or granular masses.

Formula
AlFe₃(SO₄)₆(H₂O)₁₂·6H₂O
Rarity
Uncommon
Stability
Unstable
Collector interest
Moderate Interest
Classification notes
Sulfates; hydrated ferric aluminum sulfate mineral

Key characteristics

Crystal system
trigonal
Mohs hardness
2–2.5
Specific gravity
2.09–2.17
Luster
vitreous
Transparency
transparent, translucent
Color
colorless, white, gray, yellow, green, blue, violet, pink
Streak
white
Cleavage
perfect
Fracture
conchoidal, uneven
Crystal habit
prismatic, tabular, granular, massive

Where Coquimbite is found

Top localities

  1. Javier Mine1 specimen

About Coquimbite

Specimens sourced from Peru and Spain are well regarded by collectors for their rare occurrence and the mineral’s delicate, glassy appearance. Mineral enthusiasts value coquimbite for its vivid potential color range when the composition includes subtle variations, and for its association with layered sulfate assemblages found in arid volcanic or hydrothermal settings. The combination of its striking mineral beauty, fragility, and relatively limited yet steady availability makes coquimbite a desirable, if carefully stored, addition to a polished cabinet or display, where it can be appreciated without risking rapid dehydration or alteration.