The County Louth, and all that part of the County Down bordering on it, have not had their due share of attention from those who go in search of the picturesque and beautiful. Although the direct route between the two largest cities in Ireland, northern Louth and southern Down are not at all known as well as they should be. There are, even in Kerry or Connemara, few places in which finer views of mountain, bay, and plain can be had, and all within less than two hours by rail from Dublin or Belfast. And as for antiquities, no county of its size in Ireland possesses so many as Louth.
THE WILD WEST COAST
By the west coast is meant the whole of that wondrous succession of far-penetrating fiords and bays, cliff-guarded shores, and sea-washed mountains from Bantry Bay to Malin Head, a distance of over four hundred miles. There may be wilder scenery on the coasts of Norway, Labrador, or Scotland, but for wildness, sublimity, and beauty combined, there is hardly in Europe, or in the world, another four hundred miles of coast equal to it. Its variety is one of its principal charms. There is the grandeur and wildness of Norwegian coast scenery, together with scenes of radiant beauty which cannot be found on the coasts of Norway or of Scotland. The more southern latitude of the Irish west coast, and its consequently milder climate, give it a great advantage over the coasts of Norway or of Scotland. Its grass is greener and more luxuriant, and its flowers bloom earlier in spring and later in autumn than those of more northern climes. The mild climate of the southern part of the Irish west coast is almost phenomenal. Winter, in its real sense, or as it generally is on the coasts of Norway, or even of Scotland, may be said to be unknown on the west coast of Munster. Snow is seldom seen, and frost still less frequently. Rain and wind are about all the climatic disagreeableness that those living on the south-west coasts of Ireland have to contend against. It is, however, a fact that the rainfall is not so heavy immediately on the coast as it is some ten or twenty miles inland. This is owing to the fact that the higher mountains are generally some distance from the sea; and it is well-known that mountains are great attractors of rain.
Bantry Bay is the first great sea loch of the south-western coast. It is one of the finest natural harbours in Europe, but, unfortunately, ships are seldom seen in it except when they take shelter from the “wild west wind,” which blows on these storm-beaten shores with a fury hardly known anywhere else in the world. The whole of the coast of Kerry, up to the mouth of the Shannon, is a succession of the wildest and grandest scenery, with here and there land of only slight elevation, with level meads and pastures of perennial green. Still further north, we come to the mouth of the Shannon, which forms another very fine harbour. About twenty miles north of the Shannon the famous cliffs of Moher appear. There are higher isolated cliffs than those on the west coast, but there is no long range of cliffs so high. They average between six and seven hundred feet in perpendicular height above the sea. To be seen in all their grandeur they should be seen from the sea, but to be seen in all their terribleness, they should be seen in a storm. Such is the force of the west wind on these coasts, sweeping over three thousand miles of unbroken, islandless sea, that the waves sometimes break over the cliffs of Moher in spite of their nearly seven hundred feet of perpendicular height. In no other part of the world is the force of the sea, when driven before a gale from the west, more terrific than on the west coast of Ireland. Old men who lived close to this iron-bound coast on the night of the great storm of January 6, 1839, known over the most of Ireland as the “Night of the Big Wind,” say that none but those who were near these coasts on that awful night could have even a faint idea of what the Atlantic is when a storm from the south-west drives it against the rocky barriers that seem to have been placed where they are to prevent it from overwhelming the whole island. They say that when some gigantic wave of millions of tons of water was hurled against these cliffs, the noise made was so loud that it could be heard miles inland above the roar and din of the storm; and that the very earth would tremble at every assault of the waves on those tremendous barriers to their fury.
Recent soundings taken off the west and south-west coast of Ireland have fully proved that a very large part of the island has been washed away by the fury of the west wind and the sea, and that at some far-back epoch it extended nearly three hundred miles further towards the south-west. The sea, for some two or three hundred miles west and south-west of Ireland, is shallow—hardly deeper than the Channel between Great Britain and Ireland—but at that distance there is a sudden increase of over two thousand feet in the depth of the sea. Scientists think that this submerged mountain was once the south-west coast of Ireland, and that the shallow sea between the present coast and the deep sea, about three hundred miles south-west, was once dry land, and, of course, part of Ireland. There do not seem to be any reasonable grounds to doubt this theory, for the fury of the sea is every year washing away both land and rock on these western coasts, and the way it has encroached, even in the memory of living persons, is very remarkable. Not a year passes during which hundreds of thousands of tons of rocks are not washed away from cliff and mountain by the ceaseless assaults of the stormy sea that beats with such force on the western coast of Ireland. Were it not for the cliffs and mountains that guard the whole of the west coast, the probability is that thousands of acres would be submerged every year, until there would be very little of the country left in the long run. It may be said that there must be a time coming when those barriers of cliff and mountain that now guard almost the entire west coast will be swept away, seeing that they are being constantly broken down and washed into the sea. Such a time must certainly come, unless some unforeseen event should alter the course of the Gulf Stream, or change the prevailing west and south-west winds to opposite points of the compass. The question is, How long will it be until there is real danger from the encroachment of the sea on the west coast of Ireland? This is a question which the most profound geologist living could not answer with even approximation to correctness. It is impossible to know what amount of erosion takes place every year, or what amount has taken place in any given number of years; but that not only the cliffs of Moher, but the still more gigantic ones of Slieve More in Achill, and Slieve League in Donegal, must finally succumb to the fury of the Atlantic’s waves there can hardly be a doubt. Thousands of years may elapse before the cliff barriers on the western coast become so weakened that the island will be in danger from the assaults of the sea.
From the cliffs of Moher to the Killaries, or Killary Bay, or Harbour, for it is known by all these names, there are many scenes of very great beauty; but to take even passing notice of all of them would be entirely beyond the scope of a work of the size of this. The coasts of Connemara, if not remarkable for very striking cliff scenery, are wild, sea-indented, strange, and interesting in a very high degree. But Killary Bay is one of the glories of the wild west coast. It has more the character of a Norwegian fiord than any other sea loch in Ireland. It divides the counties of Galway and Mayo. Some put it before the famed Clew Bay, and Inglis said, over half a century ago, that if the shores of the Killaries were as well wooded as Killarney, the latter might tremble for the supremacy it enjoys of being the fairest lake either of fresh or salt water in Ireland. The Killaries run some ten or fifteen miles inland, between some of the highest hills in the province of Connacht, with Maolrea, the king of Connacht mountains, on its northern side. This fiord, or narrow sea loch, is one of the most splendid harbours, not only in Ireland, but in the world, with not only complete shelter from winds from all points, but with depth of water enough to float the biggest ship that ever has been or ever will be built. But, unfortunately, there is little to attract commerce to these desolate shores, where there are no large towns, and only a sparse population. It has been said by some who have seen almost all the fiords of Norway, that there are few of them superior to the Killaries in everything that constitutes beauty, sublimity, and wildness. That this sea loch is, in a certain degree, dark and gloomy has to be admitted, because the mountains come so close to it that they seem in some places to rise almost perpendicularly out of the water. But Killary harbour is a glorious place on a clear, sunny mid-day, when its sombre mountains cast but little shade on its ever calm waters; for no matter how rough the sea may be outside, this mountain fiord is ever calm, as it is sheltered on all sides by towering heights. As an enchanting bay it is the only one on all the Irish coasts of which Clew Bay or Dublin Bay, were they living things and tormented with human passions, could possibly feel jealous.
We now approach the queen, not alone of Irish bays, but of all bays in these islands, and, according to its most ardent admirers, of all bays in Europe. This is the glorious sheet of salt water, presided over by the most symmetrical and beautiful of Irish mountains, Croagh Patrick, and guarded from the stormy Atlantic by the rocky shores of Clare Island. This is Clew Bay, the radiant beauty, the “matchless wonder of a bay,” that not one in a hundred of those in search of the beautiful know anything about. It is indeed strange that this gem of sea lochs is not better known, now that a railway brings one to its very shores.
It is almost impossible to draw a comparison between Clew Bay and the many magnificent arms of the sea that penetrate the west coasts of Ireland and Scotland, for it is so unlike most of them: Dublin Bay, while less grand and not so beautiful as Clew Bay, is the one that is most like it. Howth has somewhat the same position with regard to Dublin Bay that Clare Island occupies with regard to Clew Bay, and Slieve Coolan—in the name of all that’s decent let that abominable name “Sugarloaf” be dropped for ever—is the presiding mountain genius of Dublin Bay, just as Croagh Patrick is the presiding mountain genius of Clew Bay. Both bays are beautiful rather than sublime; they are bright and cheerful rather than dark and frowning. With all the wildness and grandeur of the many far-entering fiords of the coast of Scotland, with all the Alpine glories of their shores, there is not one of them that for beauty alone can be compared with Clew Bay. It is shrouded by no terror-striking precipices. No cataracts pour into it even in flood time. No mountains overhang it. It seems to have been made to cheer and to delight, and not to terrify or to startle. It seems to have said to the mountains round it—“Stand back; come not too near me lest your shadows should fall on me and hide, even for an instant, one gleam of my radiant loveliness.” So the mountains round it do stand back, and this is the one cause of its winsomeness, brightness, and cheerfulness. When the tide is full on a sunny day, Clew Bay seems absolutely to laugh. No shadow of surrounding hills can fall upon it, for they are too far away. It is as bright and as radiant a bay as there is in the world, and the glory of the coasts of Connacht.