sedimentary

Bituminous Coal

Organic sedimentary rock (humic coal)

AI-generated identification · may be incorrect

Hardness: 0.5-2.5; Color: Black or dark brown; Luster: Dull to sub-vitreous (somewhat shiny); Crystal Structure: Amorphous (non-crystalline); Specific Gravity: 1.1-1.4. Often shows banded layers.

Hardness: 0
Color: Black or dark brown
Luster: Dull to sub-vitreous (somewhat shiny)

Identified April 19, 2026More sedimentary →

Explore Bituminous Coal in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

Physical properties

Hardness: 0.5-2.5; Color: Black or dark brown; Luster: Dull to sub-vitreous (somewhat shiny); Crystal Structure: Amorphous (non-crystalline); Specific Gravity: 1.1-1.4. Often shows banded layers.

Formation & geological history

Formed through the deep burial and biochemical alteration of plant matter (peat) in ancient swamp environments. Subjected to heat and pressure over millions of years, typically dating from the Carboniferous or Cretaceous periods.

Uses & applications

Primary fuel source for electric power generation, used in the manufacturing of cement, and processed into 'coke' for steel production.

Geological facts

Bituminous coal is the most abundant rank of coal. It contains roughly 60–80% carbon. It is often referred to as 'soft coal' despite being harder than lignite.

Field identification & locations

Identify by its blocky fracture, dirty smudging (black streak) when rubbed, and layered appearance. Commonly found in massive sedimentary basins (Appalachians, Midwest US). Collectors value specimens with fossil plant imprints.