Ireland: The People's History of Ireland, Volume 1 (of 2)Finerty, John F. (John Frederick)
History
Ireland: The People's History of Ireland, Volume 1 (of 2)
Finerty, John F. (John Frederick)
Ireland -- History
One-seventh of the surface of Ireland is computed to be under
bogs—semi-spongy formations, claimed by some naturalists to be the
decomposed relics of mighty forests with which Ireland was covered in
remote ages. The aspect of these “moors,” as they are called by the
British, is dreary enough in winter, but at other periods they have
their charms; the heather and mosses with which they are, in many
places, thickly clothed, changing hue, as on the mountains, with every
season. Nearly all of these bogs are capable of being reclaimed for
agricultural uses, but the people do not desire their reclamation, for
the reason that they furnish cheap fuel to most of the rural districts,
where there is neither coal nor timber supply. Owing to the mildness of
the climate, the cut and dried sods of “peat,” called “turf,” which
resemble brown bricks, take the place of coal and wood, and make quite a
comfortable fire. “Stone turf,” produced by artificial pressure, and an
extra drying process, makes almost as hot a fire as anthracite, but is
much dearer than the ordinary article, which is softer and lighter.
Indeed, the common Irish turf would be almost useless in our fierce
winter weather. These fuel “reservoirs” can not be exhausted for ages to
come. It is claimed that, by some mysterious process of nature, they
renew themselves from time to time, after they have been “given a rest”
by the turf-cutters. Many large bogs occupy the summits and sides of the
mountains, and seem to be of the same character as those on the level
land. Occasionally the high morasses shift their positions, like
glaciers, only with a much quicker movement, and overwhelm, like the
avalanche, everything in their path. These are called “the moving bogs.”
The last phenomenon of the kind occurred in the County Kerry a few years
ago, when much property was destroyed and several lives were lost.
Scientists claim that these bogs are undermined by bodies of water,
which, when flooded, lift the crust and carry it with them, in their
effort to find their natural level. It is well known in Ireland that
several small, but deep, lakes now occupy places that were formerly
covered by these strange formations. We will devote a separate chapter
to other features of this interesting country.
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CHAPTER II
Further of the Characteristics and Resources of the Island—Present Form
of Government
Public-domain text, read in full here on John Shaqi.
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