Rock Identifier
Calcite (Calcium carbonate (CaCO3))
mineral

Calcite

Calcium carbonate (CaCO3)

An extremely common calcium carbonate mineral that comes in nearly every color and shows strong double refraction in clear crystals.

Mohs hardness
3
Color
Colorless or white; also yellow, orange, blue, green, pink, and many tints
Type
mineral

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Overview

Calcite is one of the most widespread minerals on Earth and the main constituent of limestone and marble. It is calcium carbonate, the same chemistry as aragonite but with a different crystal structure.

Calcite is famous for its huge variety of crystal forms (over a thousand are known) and its full rainbow of colors, from water-clear Iceland spar to orange, blue, green, and pink varieties. Clear calcite shows dramatic double refraction, splitting an image into two.

It is a defining mineral of hardness 3 on the Mohs scale and reacts vigorously with dilute acid.

Formation & geology

Calcite forms in an enormous range of environments. It precipitates from marine and fresh water to build limestone, and recrystallizes under heat and pressure into marble. It also grows in caves as stalactites, stalagmites, and flowstone.

It forms in hydrothermal veins, as a cement in sedimentary rocks, around hot springs (travertine), and as the shells and skeletons of countless marine organisms. This versatility makes it ubiquitous worldwide.

Notable specimen sources include Mexico (orange and honey calcite), Iceland (optical Iceland spar, historically), England, the United States, and many other countries.

How to identify it

The key tests for calcite are its hardness of 3 (scratched easily by a knife) and its strong fizz when a drop of dilute hydrochloric acid is applied, releasing carbon dioxide. It has perfect rhombohedral cleavage, so broken pieces form slanted rhomb shapes.

Clear calcite shows obvious double refraction: lines viewed through it appear doubled. Luster is vitreous, and the streak is white.

Look-alikes include aragonite (same chemistry, different crystal habit and cleavage), dolomite (fizzes only in warm or powdered acid), and quartz (much harder, no acid reaction, no rhombic cleavage).

Uses & significance

Calcite, as limestone and marble, is fundamental to construction, cement, and lime production. Crushed limestone is used in agriculture, steelmaking, and as aggregate; marble is a prized building and sculpting stone.

Clear Iceland spar was historically vital for polarizing optical instruments. Calcite is also used in chemical industries, as a soil conditioner, and as a colorful specimen for collectors.

Metaphysically, different colors of calcite are linked to different energies (orange for creativity, blue for calm), though these are spiritual beliefs. Specimen value depends on color, clarity, crystal form, and fluorescence.

Frequently asked questions

How do you identify calcite?

Calcite is soft (Mohs 3), fizzes in dilute acid, has perfect rhombohedral cleavage, and clear crystals show strong double refraction.

What is the difference between calcite and aragonite?

Both are calcium carbonate, but they have different crystal structures: calcite is trigonal with rhombic cleavage, while aragonite is orthorhombic and often forms needle-like or coral-like crystals.

Why does calcite split images in two?

Clear calcite has strong birefringence (double refraction): light entering the crystal splits into two rays, so objects viewed through it appear doubled.

Is calcite the same as limestone?

Limestone is a rock made largely of calcite, while calcite is the individual mineral. Marble is metamorphosed limestone, also composed of calcite.

Calcite identified by the community

Real specimens identified with Rock Identifier.

Optical CalciteCalcite (Iceland Spar)