A peat bog is not always in a hollow, but often on a hillside, and
sometimes at considerable height, which contradicts the theory that bogs
are due to defective drainage. Science long ago determined that Irish
peat was the accumulation of a peculiar kind of moss which grows like a
coral bank in the damp soil, and continues to pile up in layers year
after year, century after century, until it forms a solid mass, several
feet thick, seventy per cent moisture and thirty per cent fibre, which
burns slowly and furnishes a high degree of heat. We see bogs on all
sides of us where the peat is three and four feet thick, and with a long
straight spade that is as sharp as a knife, it is cut into blocks about
eight or ten inches long and about four inches square. A sharp spade
will slice it just as a knife would cut cheese or butter, and after the
blocks have lain on the ground a while they are stacked up on end in
little piles to dry. Then, when they have been exposed to the weather
for three or four weeks, they are stacked in larger piles, from which
they are carted away and sold or used as they are needed.
[Illustration: THE ROCK OF CASHEL, COUNTY TIPPERARY]
Four tons of peat are equal in caloric energy to one ton of coal. I
noticed in the papers that a bill is pending before the House of Commons
to grant a charter to a company to erect a station in a bog near
Robertson, Kings County, twenty-five miles from Dublin, for generating
electricity from peat, the power to be transmitted to Dublin and the
suburban towns for lighting, transportation, and manufacturing
purposes. Several other projects of a similar sort have been suggested
for utilizing the peat at the bog instead of carting it into town.
Beyond the peat beds rises a chain of low mountains with a curious
profile that runs west of the town of Templemore. Like every other freak
of nature in Ireland, they are the scenes of many interesting legends.
The highest peak is called "The Devil's Bit," and the queer shape is
accounted for by the fact that the Prince of Darkness in a fit of hunger
and fatigue once took a bite out of the mountain, and, not finding it to
his taste, spat it out again some miles to the eastward, where it is now
famous as the Rock of Cashel.
Public-domain text, read in full here on John Shaqi.
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