One Irish Summer

by William Eleroy Curtis

We could not see much from the car window, but we saw enough on the journey to understand why it is called “The Emerald Isle” and why the Irish people are so enthusiastic over its landscapes. The river is walled in nearly all the distance to Cork, and there are many factories, storehouses, and docks on both sides. Quite a fleet of steamers ply between Queenstown and Cork, and trains on the railroad are running every hour. Small seagoing vessels can go up as far as Cork, but the larger ones discharge and receive their cargoes at Queenstown. We couldn’t see much of the towns because the railway tracks are either elevated so that only the roofs and chimney pots are visible, or else they are buried between impenetrable walls or pass through tunnels on either side of the station. But when the train passed out into the open a succession of most attractive landscapes was spread before us as far as the horizon on either side, and the fields were alive with bushes of brilliant orange-colored gorse, or furze, as it is sometimes called. They lit up the atmosphere as the burning bush of Moses might have done. Very little of the ground is cultivated. Only here and there is a field of potatoes and cabbages, but the pastures are filled with fine looking cattle and sheep, for this is the grazing district of Ireland, from whence her famous dairy products and the best beef and mutton come.

Beyond Portarlington we got our first glimpses of the bogs, with which we are told one-sixth of the surface of Ireland is covered, an area of not less than 2,800,000 acres. Bogs were formerly supposed to be due to the depravity of the natives, who are too lazy to drain them and have allowed good land to run to waste and become covered with water and rotten vegetation, but this theory has been effectively disposed of by science. Everybody should know that the bogs of Ireland are not only due to the natural growth of a spongy moss called sphagnum, but furnish an inexhaustible fuel supply to the people and have a value much greater than that of the drier and higher land. The report of a “bogs commission” describes them as “the true gold mines of Ireland,” and estimates them as “infinitely more valuable than an inexhaustible supply of the precious metal.” The average Irish bog will produce 18,231 tons of peat per acre, which is equivalent to 1,823 tons of coal, thus making the total supply of peat equivalent to 5,104,000 tons of coal, capable of producing 300,000 horse power of energy daily for manufacturing purposes for a period of about four hundred and fifty years. With coal selling at $2 a ton in Ireland to-day, this makes the bogs of Ireland worth $10,000,000,000. The “bog trotter” is an individual to be cultivated, for when our coal deposits in the United States are exhausted we may have to send over and buy some of his peat for fuel. It is proposed to utilize these deposits and save transportation charges by erecting power-houses at the peat beds and furnish electricity over wires to the neighboring towns and cities for lighting, power, and other purposes, “for anybody having work to do from curling a lady’s hair to running tramways and driving machinery.” The writer refers to recent installations of electric works in Mysore, India, for working gold fields ninety miles distant, and quotes the late Lord Kelvin’s opinion that the city of New York will soon be getting its power from Niagara, four hundred miles away. We saw them digging peat in the fields and piling it up like damp bricks to dry in the sun. Freshly dug peat contains about seventy per cent of moisture, but when cured the ratio is reduced to fifteen or twenty per cent.

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.

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.

Cashel, at present a miserable, deserted village, was once the rich and proud capital of Munster. Adjoining the ruins of the cathedral is the ancient and weather-worn “Cross of Cashel,” which was raised upon a rude pedestal, where the kings of Munster were formerly crowned. The ruins are more extensive than anywhere else in Ireland, for Cashel at one time was the ecclesiastical capital of Ireland and its greatest educational centre. Here the Pope’s legates resided and here Henry II., in 1172, received the homage of the Irish kings. But what gives the place its greatest sanctity is the fact that St. Patrick spent much time there and held there the first synod that ever assembled in Ireland, about the middle of the fifth century. That is supposed to have been the reason for the erection of so many sacred edifices and monasteries in early days. St. Declan lived there, too, and commemorated his conversion to Christianity by the erection of one of the churches. Donald O’Brien, King of Limerick, erected another, and his son Donough founded an abbey in 1182. Holy Cross, beautifully situated in a thick grove on the banks of the River Suir, was built in 1182 for the Cistercian order of monks. It derived its name because a piece of the true cross, set with precious stones and presented to a grandson of Brian Boru by Pope Pascal II., was kept there for centuries, and made the abbey the object of pilgrimages of the faithful from all parts of Ireland. This precious relic is now in the Ursuline convent at Cork.

Cashel was destroyed during the civil wars. The famous Gerald Fitzgerald, the great Earl of Kildare, had a grudge against Archbishop Cragh and burned the cathedral and the bishop’s palace. He excused the act before the king on the ground that he “believed the archbishop was in it.”