In the tropical swamps of ancient Kentucky, no one was around to hear whether falling trees made a sound. About 300 million years later, though, the noise is inescapable — those trees are now coal, a fossil fuel that has long helped humans generate electricity, but whose inner demons also conjure climate change.
Coal still provides a large chunk of U.S. electricity, and since more than a quarter of global reserves sit under American soil, it's an understandably tempting power source. The organic rock is so potent and plentiful, in fact, that U.S. coal resources have a higher total energy content than all of the world's known recoverable oil.
But coal also has a dark side — its high carbon content means it emits more carbon dioxide than other fossil fuels, giving it a disproportionately big carbon footprint. Add in the ecological costs of mountaintop removal, fly-ash storage and coal transportation, and the black lump loses even more of its luster.
The U.S. Department of Energy and the electric power industry have invested heavily over the years to clean up coal, from its sulfur dioxide and nitrogen oxides to its particulates and mercury, with some success. Its greenhouse gas emissions, however, have so far defied cost-effective containment efforts.
With coal now generating almost as many headlines as megawatts, there aren't many chances to stop and consider where all this underground energy came from in the first place. But to fully understand the carbon-based ghosts now haunting our atmosphere, it helps to take a look at the fossils behind the fuel.
How is coal formed?
The basic recipe for any good fossil fuel is simple: Mix peat with acidic, hypoxic water, cover with sediment and cook on high for at least 100 million years. When these conditions occurred on land en masse during the Carboniferous Period — especially in the vast tropical peat swamps that gave the period its name — they launched the long, slow process of coalification.
"Most coals were formed close to the equator during the Carboniferous," says geologist Leslie Ruppert, who specializes in coal chemistry for the U.S. Geological Survey. "The land masses that have these thick coals were close to the equator, and the conditions were what we call 'ever-wet,' meaning tons and tons of rain."
While a supercontinent called Gondwanaland hogged much of Earth's land near the South Pole at the time, a few stragglers hovered around the equator, notably North America, China and Europe (see illustration at right). The warm, "ever-wet" weather helped create enormous peat swamps across these land masses, which are not coincidentally some of today's top coal producers. In what's now the United States, Carboniferous peat swamps blanketed much of the Eastern Seaboard and Midwest, providing fodder for today's Appalachian and Midwestern coal-mining operations.
Coal formation begins when lots of plants die in dense, stagnant swamps like the Carboniferous ones. Bacteria swarm in to eat everything, consuming oxygen in the process — sometimes a bit too much for their own good. Depending on the amount and frequency of bacterial feasting, the swamp's surface waters can become oxygen-depleted, wiping out the same aerobic bacteria that used it all up. With these decomposer microbes gone, plant matter stops decaying when it dies, instead piling up in mushy heaps known as peat.
"Peat was buried quickly enough and buried in an anaerobic environment, which happens fortuitously here and there," says USGS research geologist Paul Hackley. "An anaerobic environment prevented bacterial degradation. As the peat swamp continues to grow, you may have hundreds of feet of peat."
Peat itself has long been used as a fuel source in some parts of the world, but it's still a far cry from coal. For that transformation to happen, sediment must eventually cover the peat, Hackley explains, compressing it down into the Earth's crust. That sedimentation can occur in a variety of ways, and it swept over many peat swamps when the Carboniferous Period ended about 300 million years ago. As continents drifted and climates shifted, the peat was shoved down even deeper, with rock crushing it from above and geothermal heat roasting it from below. Over millions of years, this geological Crock-Pot pressure-cooked peat deposits to create coal beds.
While Appalachia's mountainous mines tap into some of the country's oldest, largest and most iconic coal beds, American coal didn't all form at once, Ruppert points out. The Carboniferous Period, which pre-dated dinosaurs, was peat bogs' heyday, but new coalification continued long into and after the age of the dinosaurs.
"Across the U.S., a lot of coal deposits are not Carboniferous," Ruppert says. "We have older, Carboniferous coals in the East — the Appalachians, the Illinois Basin — while in the West, coals are much younger."
In fact, the West is now America's top coal-producing region, churning out a steady stream of less mature coals from the Mesozoic and Cenozoic eras. The country's most prolific coal mines are in the Powder River Basin, a subterranean bowl that straddles the Montana-Wyoming state line. Unlike Carboniferous coals, Ruppert says, younger deposits in the West were mostly formed inside large basins that rose out of shallow seas and gradually slipped back underground.
"North America was no longer at the equator [when Western coals formed], but it also had rapidly subsiding basins that were tectonically active," she says. "Deep sedimentary basins were formed, and vegetation was eventually transformed to peat because the basins were so deep and continued subsiding for a long time. The rainfall was right, the climate was right, and then everything got buried."
What are the types of coal?
Coalification is an ongoing process, with many of the coals we currently dig up and burn still considered "immature" by geologic standards. The four main types are listed below, in order of maturity:
• Lignite: This soft, crumbly and light-colored fossil is the least mature peat product to be considered coal. Some of the youngest lignite still contains visible pieces of bark and other plant matter, although USGS geologist Susan Tewalt says that's rare in the United States. "There are some lignites where you can still see woody structures, but most of our lignite is a little bit higher grade than that," she says. Lignite is low-grade coal to begin with, containing only about 30 percent carbon since it hasn't experienced the intense heat and pressure that forged stronger types. It's found across much of the Gulf Coastal Plain and northern Great Plains, but there are only 20 operating U.S. lignite mines, most in Texas and North Dakota, since it's often not economical to excavate. Lignite makes up about 9 percent of demonstrated U.S. coal reserves and 7 percent of overall production, most of which is burned in power plants to generate electricity.
• Sub-bituminous: Slightly harder and darker than lignite, sub-bituminous coal is also more powerful (up to 45 percent carbon content) and older, usually dating back at least 100 million years. About 37 percent of the United States' demonstrated coal reserves are sub-bituminous, all of which are located west of the Mississippi River. Wyoming is the country's top producer, but sub-bituminous deposits are scattered throughout the Great Plains and eastern Rocky Mountains. The Powder River Basin, the largest single source of U.S. coal, is a sub-bituminous deposit.
• Bituminous: As the most abundant type of coal found in the United States, bituminous accounts for more than half of the country's demonstrated reserves. Formed under extreme heat and pressure, it can be 300 million years old and contain anywhere from 45 to 86 percent carbon, giving it up to three times the heating value of lignite. West Virginia, Kentucky and Pennsylvania are the main producers of U.S. bituminous coal, which is mostly concentrated east of the Mississippi. It's widely used to generate electricity, and is also an important fuel and raw material for the steel and iron industries.
• Anthracite: The grandaddy of coals isn't easy to come by. Anthracite is the darkest, hardest and usually oldest type, with a carbon content of 86 to 97 percent. It's so rare in the United States that it accounts for less than half a percent of overall U.S. coal production and just 1.5 percent of demonstrated reserves. All of the country's anthracite mines are located in northeastern Pennsylvania's Coal Region.
The United States has the world's largest known overall coal reserves, a total of nearly 264 billion tons. As miners exhume these ancient tropical swamps and power plants release their vapors into the air, a national and global clamor is developing over the future of coal. Regardless of what happens with future energy regulations, though, coal's nonrenewability will eventually fuel the search for alternatives if nothing else does — at current usage, even U.S. reserves are only expected to last another 225 years.
For more info about the formation, deposits or cleanliness of coal, check out these links:
- EPA: Coal and Clean Energy
- EIA: U.S. Coal Production
- EIA: U.S. Coal Reserves
- EIA: Major U.S. Coal Mines
- EIA Kids Energy Page: Coal Energy
- USGS: Coal Resources
- DOE: A Brief History of Coal Use
- DOE: Clean Coal Power Initiative
- DOE: FutureGen Initiative
- California Energy Commission: Coal, Oil and Natural Gas
Photos courtesy NASA, DOE, USGS