Peat
is not coal. It might be called a step in the process of making coal.
Coal itself is made of the remains of ancient
trees and plants that grew in swampy
jungles in warm, moist climates hundreds of millions of years ago. These trees and plants fell into the swamp waters. Bacteria changed some parts of the wood into gases
that escaped, leaving behind a black
mixture, mostly carbon. In time the pressure from mud and sand above squeezed
out most of the liquid, leaving behind a pasty mass that slowly hardened
into coal.
This process, from beginning to end, took
thousands of years. But the first
stages of that process of making coal can actually be seen going on
today. In the Great Dismal Swamp of Virginia and North Carolina and in thousands of swamps of the northern states of the U.S.A.
and Canada, peat is being made.
In
these swamps, plants are gradually decaying in a process that leaves most of the carbon in place. A few years of
such action produces a brown, matted
mass of twigs, branches, and leaves. This is known as peat. When the water is drained from such a swamp, the peat
can be cut into blocks, set out to dry, and then burned as fuel.
Drying is important because peat in the ground may
be three- fourths water. In Ireland, where peat is plentiful
and the higher forms of coal are expensive, more than half of the farms depend
entirely on peat for fuel.
The other forms of coal are developments from peat.
If peat is allowed to remain where it
forms, it gradually changes into lignite, or brown coal. It is more solid than
coal, but still soft enough to crumble when shipped long distances.
The next form of coal is
bituminous, or soft coal. It is formed from
lignite by chemical change and pressure in the earth over thousands
of years. This is the most important member of the coal family. It burns easily and is
abundant.
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