
sedimentary
Anthracite coal
Anthracite; predominantly carbon (C), with minor mineral impurities
AI-generated identification · may be incorrectHardness about 2.5–3 Mohs; black to steel-gray, bright submetallic luster, irregular blocky fracture, and very fine-grained structure. It is dense, brittle, and usually shows little clay or visible layering.
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Physical properties
Hardness about 2.5–3 Mohs; black to steel-gray, bright submetallic luster, irregular blocky fracture, and very fine-grained structure. It is dense, brittle, and usually shows little clay or visible layering.
Formation & geological history
A high-rank metamorphic coal formed when bituminous coal was subjected to intense heat and pressure, typically during mountain building. It commonly formed in Carboniferous coal basins, roughly 359–299 million years ago.
Uses & applications
Used as a high-temperature fuel, smokeless domestic heating coal, reducing agent in metallurgy, and occasionally as a carbon source for water filtration. It has little jewelry value.
Geological facts
Anthracite has the highest fixed-carbon content and lowest volatile matter of ordinary coal, commonly around 86–97% carbon. It burns with a short blue flame and produces relatively little smoke.
Field identification & locations
Identify it by its hard, shiny black appearance, high density, and conchoidal-to-blocky fracture; it generally does not smear easily like softer bituminous coal. Major sources include Pennsylvania, Vietnam, Russia, China, and Wales.
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