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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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