
Anthracite
Carbon-rich coal (high-rank, >86% fixed carbon)
The highest-rank coal, a hard, lustrous black rock that burns cleanly with little smoke and high heat output.
- Mohs hardness
- 2-2.5
- Color
- Iron-black to brownish-black, often with a submetallic sheen
- Type
- metamorphic
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Overview
Anthracite is the highest grade of coal, formed when bituminous coal is subjected to elevated heat and pressure during regional metamorphism. It is the hardest and most carbon-rich coal, containing more than 86% fixed carbon and very little moisture or volatile matter.
Unlike softer coals, anthracite has a bright, almost glassy submetallic luster and a conchoidal fracture. It does not soil the fingers the way bituminous coal does. Because it ignites with difficulty but then burns steadily at high temperature with almost no smoke, it was historically prized as a clean domestic and industrial fuel.
The most famous deposits lie in northeastern Pennsylvania, with other significant fields in Wales, Ukraine, China, and Russia.
Formation & geology
Anthracite begins as peat that accumulates in ancient swamps, which is buried and compacted into lignite and then bituminous coal. Continued deep burial, heat, and especially the directed pressure of mountain-building (orogeny) drive off remaining volatiles and water, concentrating carbon and raising the coal to anthracite rank.
For this reason anthracite is genuinely a metamorphic rock, typically found in folded and faulted belts. The Pennsylvania anthracite fields, for example, formed where Carboniferous coal beds were caught up in the Alleghenian orogeny. Tectonic deformation explains why anthracite seams are often steeply tilted, contorted, and harder to mine than flat-lying softer coals.
How to identify it
Look for a black, hard, brittle rock with a distinctive bright submetallic to vitreous luster and a conchoidal fracture that produces sharp, curved surfaces. It is notably clean to handle and does not leave black smudges on your hands, which separates it from sooty bituminous coal.
Its streak is brownish-black. Anthracite is denser and harder than other coals and rings slightly when tapped. Look-alikes include obsidian (which is glassier, harder, and translucent on thin edges) and jet (which is lighter and warm to the touch). A simple burn test confirms it: anthracite is hard to light but burns with a short blue, nearly smokeless flame.
Uses & significance
Anthracite's main value is as a premium fuel. It burns hot, long, and clean, making it ideal for home heating, blacksmithing, and metallurgical processes. Crushed anthracite is also widely used as a filter medium in water treatment plants.
Historically it powered the Industrial Revolution in the eastern United States and remains important in steelmaking and ferroalloy production. Polished pieces are occasionally carved into small ornaments, and it is sometimes substituted for jet in mourning jewelry, though it is more brittle. Metaphysically it is associated with grounding and protection, though such claims are not scientifically supported.
Frequently asked questions
Is anthracite a rock or a mineral?
It is classified as a rock, specifically the highest-rank coal. Because it forms under metamorphic heat and pressure, it is best described as a metamorphic rock rather than a true mineral, which would require a fixed crystal structure.
How is anthracite different from regular coal?
Anthracite is harder, denser, and contains far more carbon and less moisture than bituminous or lignite coal. It burns hotter and cleaner with little smoke, and it does not smudge your hands.
Why is anthracite so hard to ignite?
Its very low volatile content means there are few easily flammable gases to catch fire. Once it does reach ignition temperature, however, it burns steadily and very hot for a long time.
Where is anthracite mined?
The most famous deposits are in northeastern Pennsylvania, USA. Other major sources include Wales, Ukraine, Russia, China, and South Africa.
Anthracite guides
In-depth guides for identifying, valuing, and understanding Anthracite.
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