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Aragonite

Mineral

Aragonite

Also known as: Flos Ferri (a specific variety), Sputnik Aragonite

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Description

Aragonite is a carbonate mineral, one of the two common naturally occurring crystal forms of calcium carbonate (CaCO3), the other being calcite. It crystallizes in the orthorhombic system, in contrast to calcite's trigonal system. This difference in crystal structure leads to distinct physical properties. Aragonite is typically found in acicular (needle-like), columnar, fibrous, or radiating crystal habits, often forming pseudohexagonal twins. It is less stable than calcite at standard temperature and pressure and will slowly convert to calcite over geological time, a process known as aragonite-calcite inversion. This inversion is accelerated by heat and pressure.

How to Identify

Color
Typically white, colorless, or gray, but can also be yellow, green, blue, violet, brown, or pink due to impurities.
Luster
Vitreous (glassy) to resinous.
Texture
Often fibrous, columnar, or radiating aggregates. Individual crystals can be prismatic or acicular.
Crystal Form
Orthorhombic system. Commonly forms pseudohexagonal twins, radiating aggregates, stalactitic, columnar, or fibrous masses. Acicular (needle-like) crystals are characteristic.
Cleavage
Distinct cleavage in one direction ({010}), and imperfect in two others ({110} and {011}). This is often difficult to observe in fine-grained or fibrous aggregates.
Geological Environment
Found in evaporitic deposits, hot spring deposits (tufa), speleothems (cave formations), mollusk shells, coral skeletons, serpentinites, and as a secondary mineral in altered igneous and metamorphic rocks. Also forms in high-pressure, low-temperature metamorphic facies (e.g., blueschist facies).

Key Facts

  • Hardness: 3.5 - 4 on the Mohs scale
  • Specific Gravity: 2.93 - 2.95 g/cm³
  • Crystal System: Orthorhombic
  • Color: White, colorless, gray, yellow, green, blue, violet, brown, pink
  • Luster: Vitreous to resinous
  • Transparency: Transparent to translucent
  • Fracture: Subconchoidal to uneven
  • Cleavage: Distinct on {010}, imperfect on {110} and {011}
  • Composition: Calcium Carbonate (CaCO3)

Quick Check

  • Color: White, colorless, gray, yellow, green, blue, violet, brown, pink
  • Luster: Vitreous to resinous
  • Streak: White

Physical Characteristics

  • Crystal Habit: Acicular, prismatic, columnar, fibrous, radiating, stalactitic, massive. Often forms pseudohexagonal twins.
  • Cleavage Type: Distinct in one direction ({010}), imperfect in two others ({110} and {011}).
  • Fracture Type: Subconchoidal to uneven.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy) to resinous.

Formation

Aragonite is a polymorph of calcium carbonate (CaCO3), meaning it has the same chemical composition as calcite but a different crystal structure. It forms under specific conditions of lower temperature and higher pressure than calcite, or in environments with high magnesium concentrations that inhibit calcite precipitation. Common formation environments include: biogenic precipitation (e.g., in mollusk shells, coral skeletons), speleothems (cave formations like stalactites and stalagmites), hot springs (forming tufa), serpentinites, and as a diagenetic mineral in sedimentary rocks, particularly in evaporitic settings or deep-sea sediments. It can also form in hydrothermal veins and as a secondary mineral in altered igneous and metamorphic rocks.

Usage

Aragonite has several uses. It is a common component in marine organisms' shells and skeletons, playing a crucial role in marine ecosystems. Industrially, it is used as a raw material for cement, lime, and as a filler in plastics and paints. High-quality specimens are prized by mineral collectors. It is also used in water treatment to remove heavy metals and in some agricultural applications as a soil conditioner. Its unique crystal structure makes it a subject of research in materials science.

Age Distribution

Found in geological formations ranging from the Precambrian to the present day, often associated with relatively recent low-temperature, low-pressure environments.

Where to Find

Spain

Molina de Aragón, Guadalajara, Spain, is the type locality and known for excellent pseudohexagonal crystals.

Slovakia

Ochtinská Aragonite Cave, a UNESCO World Heritage site, features unique aragonite formations.

United States

Various localities, including New Mexico (e.g., Santa Eulalia District), Arizona, and California, for cave formations and hydrothermal occurrences.

Mexico

Mines in Chihuahua are known for fine aragonite specimens.

Austria

Styria and Carinthia regions for various habits.

Czech Republic

Known for some historical occurrences.

Finding Tips

Cave Environments

Look for aragonite in caves, where it forms stalactites, stalagmites, and other speleothems, often alongside calcite. Aragonite speleothems tend to be more delicate and needle-like.

Hot Spring Deposits

Examine areas around hot springs and geysers for tufa deposits, which can contain aragonite.

Serpentinite Occurrences

Aragonite can be found in veins within serpentinite rocks, often associated with other secondary minerals.

Fossil Shells

Many modern and some fossil mollusk shells are composed of aragonite. However, older fossil shells often show aragonite that has inverted to calcite.

Hydrothermal Veins

Search for aragonite in hydrothermal veins, particularly in areas with low-temperature fluid circulation.

Acid Test

Like calcite, aragonite will effervesce (fizz) vigorously when a drop of dilute hydrochloric acid (HCl) is applied, due to the release of carbon dioxide. This distinguishes it from many non-carbonate minerals.

Similar Rocks

Calcite

Calcite

Also known as: Calcium Carbonate

Dolomite

Dolomite

Also known as: Calcium Magnesium Carbonate

Gypsum

Gypsum

Also known as: Hydrated Calcium Sulfate

Scientific Classification

Mineral Class
Carbonates
Group
Aragonite Group
Crystal System
Orthorhombic
Chemical Formula
CaCO3
Composition
Calcium Carbonate

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