Rock Identifier
Orange Calcite (Calcite (Calcium Carbonate, CaCO3)) — Mineral
Mineral

Orange Calcite

Calcite (Calcium Carbonate, CaCO3)

Hardness: 3 on the Mohs scale (very soft, can be scratched by a copper coin). Color: Ranges from pale yellow to deep orange/amber due to iron inclusions. Luster: Vitreous to resinous. Crystal Structure: Trigonal, often forming rhombohedral crystals, but can also be granular, massive, or columnar.…

Luster
Vitreous to resinous
Identified More mineral

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Physical properties

Hardness: 3 on the Mohs scale (very soft, can be scratched by a copper coin). Color: Ranges from pale yellow to deep orange/amber due to iron inclusions. Luster: Vitreous to resinous. Crystal Structure: Trigonal, often forming rhombohedral crystals, but can also be granular, massive, or columnar. Cleavage: Perfect rhombohedral (three directions at 75°). Specific Gravity: 2.71.

Formation & geological history

Calcite is a very common mineral formed in various geological environments. Orange calcite specifically gets its color from trace amounts of iron. It forms from the precipitation of calcium carbonate from supersaturated aqueous solutions. This can happen in sedimentary environments (e.g., forming limestone, marble from metamorphism of limestone), hydrothermal veins, caves (stalactites and stalagmites), or as a component of igneous rocks. Its geological age varies widely depending on the specific deposit.

Uses & applications

Industry: Used in cement, lime, and glass production; as a filler in paints, plastics, and rubber; and in agriculture for soil conditioning. Jewelry/Decor: Polished into cabochons, beads, or carved into ornamental objects; specimens are popular with collectors. Construction: A primary component of limestone and marble, used as building materials, dimension stone, and aggregate.

Geological facts

Calcite is one of the most common minerals on Earth and is the primary constituent of limestone and marble. It exhibits double refraction, meaning if you place a clear piece of calcite over text, the text will appear doubled. This property is particularly strong in Iceland Spar, a clear variety of calcite. Calcite reacts vigorously with dilute acids (like vinegar or hydrochloric acid), producing effervescence (fizzing) due to the release of carbon dioxide gas.

Field identification & locations

In the field, identify calcite by its relative softness (scratches easily with a knife or copper coin), its perfect rhombohedral cleavage, and its reaction to acid (fizzes). The orange color is a key identifier for this specific variety. It is commonly found worldwide in sedimentary rocks (limestone, dolostone), metamorphic rocks (marble), and as vein fillings in various rock types. Notable occurrences for vibrant orange calcite include Mexico, the USA (Missouri, Oklahoma), and China. For collectors, well-formed crystals or translucent, richly colored masses are sought after.