Aragonite

Aragonite specimens for sale

195 for sale · $90–$10,000 USD

521 in the gallery

Aragonite is a carbonate mineral that crystallizes in the orthorhombic system, commonly forming acicular, radiating, or tabular habits. It can exhibit a wide range of colors due to trace impurities, and often shows a vitreous to resinous luster. Notable specimens are frequently pale to brownish, with blades or clusters that display a subtle, glassy sheen under light. In many collections, aragonite appears as pale, needle-like sprays or chunky, bladed aggregates that reveal its granular interior when cut or fractured.

Formula
CaCO3
Rarity
Abundant
Stability
Stable
Collector interest
High Interest
Classification notes
Carbonates; Strunz 5.A (Carbonates and Nitrates)

Key characteristics

Crystal system
orthorhombic
Mohs hardness
3.5–4
Specific gravity
2.93–2.95
Luster
vitreous, resinous
Transparency
transparent, translucent, opaque
Color
colorless, white, gray, brown, red, orange, yellow, green, blue, violet, pink
Streak
white
Cleavage
distinct
Fracture
subconchoidal, uneven
Crystal habit
prismatic, acicular, fibrous, radiating, botryoidal, stalactitic, druzy, granular, massive
  • Gem mineral
  • Fluorescent: white, blue, green, yellow, orange, pink
  • Classic / historic

Buy Aragonite specimens

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Where Aragonite is found

Top localities

  1. Agrigento24 specimens
  2. Wenshan Mine20 specimens
  3. Queen of Green Pocket12 specimens
  4. Cianciana9 specimens
  5. Hilarion Mine9 specimens
  6. Imam Rabat aragonite/azurite occurrence8 specimens
  7. Minglanilla8 specimens
  8. Santa Eulalia Mining District7 specimens
  9. Tsumeb7 specimens
  10. Christiana Mine5 specimens

About Aragonite

Significant specimens originate from locales such as Namibia, the USA, Italy, the UK, and Spain, where unique geological conditions produced striking crystal formations. Collectors value aragonite for its structural variety and its ability to form dramatic, radiating sprays that contrast with other carbonate minerals. Its occurrence in vugs and cavities within sedimentary and volcanic rocks adds to its appeal, offering both aesthetic geometry and a glimpse into the mineral’s crystallization history.