Anhydrite specimens for sale

20 for sale · $250–$2,800 USD

159 in the gallery

Anhydrite is a mineral composed of calcium sulfate (CaSO4) that occurs in colorless, white, or gray crystals. It commonly forms elongated prisms or tabular crystals with a glassy to vitreous luster and a transparent to translucent appearance. In many localities, including notable deposits in Mexico and Peru, specimens can display well-developed single crystals or twinned formations, sometimes intergrown with other sulfate minerals. The mineral can occur in massive to prismatic habits and may appear in pale blue to colorless hues when impurity-free, though it often looks milky or smoky in aggregate.【Note: descriptive line preserved to fit style; no speculative features】

Formula
CaSO4
Rarity
Common
Stability
Stable
Collector interest
Moderate Interest
Classification notes
Sulfates; calcium sulfate (Anhydrite group)

Key characteristics

Crystal system
orthorhombic
Mohs hardness
3–3.5
Specific gravity
2.89–2.98
Luster
vitreous, pearly, greasy
Transparency
transparent, translucent, opaque
Color
colorless, white, gray, blue, violet, pink, brown, red
Streak
white
Cleavage
perfect
Fracture
uneven, splintery
Crystal habit
prismatic, tabular, fibrous, granular, massive
  • Gem mineral

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Where Anhydrite is found

Top localities

  1. Prospect Park Quarry32 specimens
  2. Naica24 specimens
  3. Simplon Railway Tunnel22 specimens
  4. Empire State No. 4 Mine11 specimens
  5. Sweetwater Mine6 specimens
  6. Tenke-Fungurume area5 specimens
  7. Naica Mine3 specimens
  8. Rumipata3 specimens
  9. Upper New Street Quarry3 specimens
  10. Iraí2 specimens

About Anhydrite

Collectors value anhydrite for its clear, often sharp crystallization and its association with evaporite environments. It is frequently found in hydrothermal veins and contact metamorphic zones, where it can crystallize alongside gypsum, dolomite, and halite. While it may be confused with gypsum due to similar composition, anhydrite remains less soluble and tends to retain its crystallographic integrity in drier, high-temperature settings. When exhibited as pristine crystals or as part of mineral aggregates from strong localities, anhydrite makes appealing cabinet specimens and complements collections focused on sulfate minerals and evaporite mineralogy.