Mineral field guide

How to identify calcite

Calcite is a relatively soft carbonate mineral recognized by Mohs hardness 3, three-direction rhombohedral cleavage, and vigorous reaction with dilute acid on a fresh surface.

mineralCarbonate mineral · CaCO₃

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Calcite mineral specimen with pale translucent crystals
Calcite crystal specimen; source image resized and re-encoded for web displayPhoto: Raimond Spekking · CC BY-SA 4.0 · Wikimedia Commons
Classification

What is calcite?

Calcite is calcium carbonate. Magnesium, iron, manganese, and other elements may substitute in small amounts, and inclusions can change color or transparency.

Appearance

What does calcite look like?

Calcite has many crystal habits, including rhombohedra and scalenohedra, and also occurs massive, granular, fibrous, or earthy.

Clear cleavage fragments may show double refraction, making a line viewed through the crystal appear doubled. Weathered calcite can be dull or chalky.

Field tests

Identification tests

Begin with observation and use the least destructive test first. Results can change with weathering, mixtures, coatings, and grain size. Review the step-by-step field-test methods before altering an unfamiliar specimen.

Hardness

3

Scratched by a copper coin or steel point; harder than a fingernail.

Streak

White

Helpful for colored samples but not unique.

Cleavage

Perfect in three directions, not at 90°

Produces repeated rhombohedral fragments.

Acid

Strong fizz on a fresh surface

A defining carbonate test when performed safely.

Comparison

Common lookalikes

Dolomite

Usually reacts weakly on an unpowdered surface and is slightly harder.

Quartz

Hardness 7, no cleavage, and no acid reaction.

Gypsum

Softer than a fingernail and does not effervesce with acid.

Geologic origin

How does it form?

Calcite forms in marine and freshwater sediments, shells and skeletons, caves, hydrothermal veins, altered rocks, and metamorphic marble.

It precipitates from water and also recrystallizes during burial or metamorphism, so the same mineral can record very different environments.

Where it occurs

Geologic setting and occurrence

Calcite is the principal mineral in most limestone and marble and is common in veins, geodes, travertine, cave deposits, and fossil material.

Optical clarity, color, and crystal shape vary. A hand-sample identification does not determine whether a specimen is natural, treated, or commercially valuable.

Human use

Uses and significance

Calcite-bearing rock supplies cement, lime, aggregate, agricultural lime, fillers, and dimension stone. Crystalline calcite also has optical and collecting uses.

Safety and limits

Field notes

  • Dilute acid can damage specimens and structures; use only where permitted with eye protection.
  • Never remove cave formations.
  • Do not lick or taste an unknown specimen.

This guide supports preliminary field identification, not a laboratory determination, appraisal, hazard assessment, or statement of ownership or collecting permission. Verify land status and local rules before handling or collecting material.

Source basis

Authoritative sources

LithoMap wrote this guide in original language using the scientific concepts and physical-property standards supported by these sources.

Editorial review: September 17, 2026.