Rock Identifier
Anthracite Coal (Anthracite) — metamorphic
metamorphic

Anthracite Coal

Anthracite

Hardness: 2.5-3.0 (Mohs); Color: Black to steel gray; Luster: Sub-metallic to brilliant/greasy; Crystal Structure: Amorphous; Cleavage: Conchoidal fracture; Specific Gravity: 1.3-1.7.

Hardness
2
Color
Black to steel gray
Luster
Sub-metallic to brilliant/greasy
Identified More metamorphic

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Physical properties

Hardness: 2.5-3.0 (Mohs); Color: Black to steel gray; Luster: Sub-metallic to brilliant/greasy; Crystal Structure: Amorphous; Cleavage: Conchoidal fracture; Specific Gravity: 1.3-1.7.

Formation & geological history

Formed through the low-grade metamorphism of bituminous coal. It undergoes intense heat and pressure over millions of years, typically during mountain-building events (orogeny), resulting in the highest carbon content of all coals (86% to 98%).

Uses & applications

Historically used as a high-grade fuel for domestic heating and industrial steam production. Today, it is used in water filtration, as a reducing agent in metallurgy, and occasionally for carving into jewelry or artistic figurines.

Geological facts

Anthracite burns with a short, blue, smokeless flame. It is known as the cleanest-burning coal available because of its high carbon and low sulfur content. Large deposits are found in the Appalachian Mountains of Pennsylvania.

Field identification & locations

Identify by its hardness (doesn't soil fingers easily), brilliant high luster, and conchoidal fracture (curved breakages). It is primarily found in folded mountain belts. Collectors look for pieces with 'peacock' iridescence or unique shapes.