reform which has long been demanded by England seems at last about to be carried out. Señor Besada, Minister of Public Works, and one of the most eminent men in the Conservative party, is, we are told, about to give instructions for the provision of luminous buoys and fog-signals at the points of danger. A Commission of Engineers has already been nominated to study the question. It is here that the furious waves, working like yeast, break against the half-hidden rocks, and, rising to a stupendous height, swoop down upon them with thundering noise even in the most smiling weather. It is here that corpses of unfortunate fishermen are so constantly washed ashore that the local papers announce such events almost without comment. It is truly most appropriate that San Telmo, the patron saint of all Spaniards who go down to the sea in ships, should have had his birthplace in Galicia,[29] Spain’s breakwater against the Atlantic.[30] The last outposts of the Pyrenees advance a considerable distance into the sea. The Atlantic Ocean alone checks the spread of “the great dorsal chain which comes down from Tartary and Asia,”[31] whose highest peak within the boundaries of Galicia is the peak of Guina, in the Sierra de Ancares, which is only a little over two thousand metres high:[32] many winters pass without its once becoming covered with snow. A glance at the map of Galicia will show the reader that this province is entirely composed of alternating peaks, hills, and valleys. It has often been called on this account “the Switzerland of Spain.” The rock of which the mountains and boulders are formed is almost entirely of granite. In fact, all the higher levels of the province of Pontevedra are so covered with granite that it is impossible to tell what other formation this stone has replaced. The rocky soil possesses all the ingredients most favourable to rich vegetation. Galicia has many different climates, resulting from the varied heights of the different zones above sea-level. The differences in temperature and in the humidity of the air are very considerable. Central Galicia is in the same latitude as Russian Turkestan, as part of Albania, and as Pennsylvania, but her climate is infinitely more humid than that of these countries. Heavy and continuous rains soak through the earth and replenish the innumerable mountain springs which are the great cause of Galicia’s wonderful fertility; the springs, themselves perennial, feed in their turn the countless streamlets, each of which is again a fresh centre of evaporation. The vigorous vegetation which responds to these extremely favourable conditions helps to preserve, by the cool moisture of its rich and abundant foliage, the dampness of the atmosphere, and to the reunion of these three causes may be traced the remarkable humidity of the province.