The South Isles of Aran (County Galway). Burke Oliver Joseph

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СКАЧАТЬ fairy flax, much relied on for its medicinal qualities. In several of the localities in the islands the tormentil root, which serves in place of bark for tanning, and another plant which gives a fine blue dye and which the islanders use in colouring woollen cloths manufactured by them for their own wear, are to be found. The Aran isles contain many rare plants; but, owing to the absence of turf bogs and scarcity of damp ground, there are neither marshy nor heathy plants, nor sedges, nor rushes. Even so, the flora of Aran is decidedly rich. On the hillsides are a great variety of flowering plants indigenous to the soil, which blossom at different times of the year. In the rocky dells there are several kinds of convolvulus of very rich florescence. The Madagascar periwinkle seems to be perfectly acclimatized and blossoms profusely, and we were happy to find an abundant growth of hops, the introduction of which is ascribed to the monks of the olden time.

      ORNITHOLOGY OF ARAN.

      The tillage of the islands comprises potatoes, mangold wurzel, vetches, rape, clover, oats, and barley. The potatoes almost exclusively planted are "the Protestants;" and a Protestant tourist unarmed felt somewhat alarmed at the startling intelligence that "dinner would be ready as soon as the Protestants that were on the gridiron would be roasted." The dinner brought up, need it be told that our Anglican friend enjoyed the joke of our witty waitress quite as much as we ourselves did?

      TANKS WANTING IN ARAN.

      The crops are greatly devastated by caterpillars and grubs. The abundance of these pernicious insects is attributed to the great scarcity of sparrows and other small birds. Starlings are seldom seen; but never a swallow. Sea gulls are numerous, and amongst the sea birds the osprey or sea eagle is a conspicuous object. Neither the raven, rook, crow, nor jackdaw visits the islands; but there is a handsome bird which is very numerous, especially in the north island. The chough, which, in addition to plumage dark and glossy like that of the jackdaw, displays a beak and legs of bright scarlet. It is said that this bird was formerly to be seen in flocks on various parts of the English coasts, and that now it cannot be found in any part of the United Kingdom except in Aran. Plovers, gannets, pigeons, duck, teal, and divers breed abundantly on the rocky ledges. The cliffs are the resort of countless puffins (Anas Leucopsis); the popular belief being that they spring from the driftwood1. Their flesh supplies a rich lamp oil, and their feathers fetch a high price in the London markets. The capture of these birds is a dangerous occupation for the cragsmen, who descend from the cliffs by means of a rope to the haunts of the puffin, and having spent the night in the dangerous occupation, ensnaring and killing them as they sleep on the rocky ledges, they are hauled up in the morning, having realized ten or twelve shillings during the night. In the summer of 1816, two unfortunate fellows engaged in this frightful occupation missed their footing, and falling, were dashed to pieces on the rocks below. The solitary bittern, called in Irish the Boonaun-Laynagh, frequents the low-lying ground on the Galway side of the island, and hares and rabbits are very plentiful also. On the barren sheets of rocks the peasants (denominated lazy and idle, by lazy and idle writers and speakers) have with tireless toil walled in and made numberless gardens in which potatoes mealy and dry are grown. The meteorological aspirations of the Aran peasant are for rain, diametrically the opposite of what their brethren on the mainland desire. A dry summer gives to Aran a parched and burnt-up hue, when the cattle faint and die if not removed to the mainland. Tanks, such as they have in Ceylon, are sadly wanting in those islands, and the expense of their construction must be a trifling matter indeed.

      ICE-CUT FURROWS.

      One of the most remarkable features in the conformation of Inishmore is, that between the overlapping strata or terraces of limestone, thirty-seven feet in thickness in some places and eighteen in others, are beds of shale. The highest of the terraces is 320 feet over high-water mark, on the perpendicular cliff overlooking the Atlantic. On the sixth lowest of these descending steps the village of Kilronan, the capital of the island, over against the Galway bay, is built, and under that terrace and over the seventh is a shale bed which contains the water supply for the glebe and upper village wells.

      BOULDERS.

      Those who delight in geological speculations will find in these isles much to interest them. Here are deep furrows in the hard rocks, cut as they say by passing icebergs. One of these ice-cut furrows may be seen near the shore of Killeany Bay, about two hundred yards north-east of Lough Atalia, and a quarter of a mile from Kilronan. It is about seven yards long, nearly a yard wide, having a bearing of east by north. Though the icebergs have left their striæ, and though their passage is marked by the deep furrows cut by them as they moved, nevertheless the patches of boulder drift on the surface are few; but the bergs in their passage from the north district did drop some huge metamorphic rocks, not one of which is indigenous, so to speak, to the islands, but have been carried from a district such as that of Oughterard. Strange that some limestone boulders have also been dropped, carried from some far-off limestone district. These boulders have withstood the wreck of ages, but the weather-beaten rocks under them are so worn as here and there to present the appearance of pedestals bearing up the superincumbent masses. Whilst there is much to arrest the attention as you look from the hotel windows towards Galway over the Galway bay, bounded on the north by the grotesque desolation of the Connemara mountains, and on the south by the rocky mountains of the county of Clare, it is on the south-west side of the islands of Aran that the scene is awfully sublime, terrific, and impressive – rendered more awful by reason of the confusion of the waters and of the roaring of the waves of the sea. The heavy swell of the Atlantic there rolls in angry billows against the cliffs dark and perpendicular, hundreds of feet in height – cliffs perforated by winding caverns worn by the violence of the waves, from one of which, having an aperture in the surface, was projected a column of water to the height of a ship's mast. Whilst many of these cliffs rise perpendicularly from the ocean, many of them have sea terraces or steps at foot below the high-water mark. At Illaun-a-naur, on the south-easterly side of the great island, are sea-terraced cliffs which are fendered by a rampart formed of enormous blocks of limestone upheaved from the depths of the ocean and hurled with violence on the rampart which now forms a foot barrier against the further encroachment of the Atlantic.

      SEA WEEDS.

      The seaweeds around the Aran islands are peculiarly fitted for the production and manufacture of kelp, of which there are two varieties, one made from the black weed, and the other from the red. The black usually grows above the low-water mark of the neap-tide, whilst all the red grows below it. The red weed kelp is the most valuable, as in general it gives salts containing iodine. Marine plants, such as the sea-anemones, the rock-grown samphire, and the sea-cabbage grow around the islands in great profusion.

      Another remarkable feature in Aran is the enormous amount of fine quartzose – moving sands which, blown in thick clouds by the winds, fill the nooks and corners and crevices of the islands. These sands, which are said to possess the property of preserving bodies uncorrupted after death, might be fixed and utilized in the same manner as the sands of Arcachon on the west coast of France have been fixed and utilized, by planting therein vast forests of the Pinus maritima, the interlacery of whose roots would do the twofold duty of fixing the sands and creating a soil enriched by the amount of nitrogen therein digested and deposited. At Trawmore, on the south of Killeany Bay, proofs have lately been discovered not only of the movement of the sand-hills, but also of the appearance of fields and buildings submerged on the sea-coast.

      MOVING SANDS IN ARAN.

      These islands in prehistoric times must have suffered much from the convulsions which then shook the world – in later times they appear to have suffered little, though Richard Kirwan the chemist relates that in his memory, in the year 1774, a fearful thunderstorm visited Inishmore, when a granite block of enormous dimensions, called the "Gregory," was struck by lightning, shattered to atoms, and flung into the sea.

      CHAPTER II

      "Remnants of things that have passed СКАЧАТЬ