Spain. Wentworth Webster
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and floods rush down, sweeping away dams which have stood for centuries, washing away towns and villages, and spreading destruction far and wide. To compute the rainfall of such floods into an average is only to play with figures. Murcia has an average temperature of 64°, maximum 112°, minimum 24°, and an extreme range of 120°. The rainfall averages about 12½ inches on the coast, but varies greatly; at Albacete it is said to average 13 inches. The directly southern coast, from the Cabo de Gata to Gibraltar, has a milder and more equable climate than that of the south-eastern coast; but in the inland valley of the Guadalquiver the range is more extreme, both for heat and cold. The dryness in the eastern district still continues from Cartagena to Almeria; the rainfall is said to be only 12 inches. At Malaga, while the average temperature is 66°, about the same as that at Valencia and Alicante, the maximum is said to be only 78°, and the minimum 53°. At Motril, between Malaga and Almeria, the maximum is 77°, and the minimum 52°. In Seville on the other hand, the average is 68°, with a maximum Of 118°, and a minimum of 30°. Cordova, somewhat colder, has a maximum of 93°, and a minimum of 27°. The rainfall is also more moderate at Malaga, 15½ inches, and 23 at Seville. Granada, in its upland but sheltered valley, at an elevation of 2681 feet, defended from the east and south by the snowy range of the Sierra Nevada, and by the mountains of Granada to the north, has still an average of 65°, with a maximum of 97°, and a minimum of 42°. The rainfall varies considerably in different years, and various geographers give its average as 23½ 33½, and the latest (Reclus) 48½. Cadiz has an Atlantic climate, which in temperature and greater rainfall, 37 inches, closely approximates to that of Madeira. Moving westward it decreases, at Gibraltar, 34½, San Fernando, 27; while at Huelva and Tarifa, where the moisture of the north-west gales is intercepted by the Portuguese mountains, it descends to 24½. We have now only to treat of the climate of the great central elevation, the plateau, which ranges at an average height of some 2000 feet above the sea. Thus, Madrid is 2148, Segovia 2299, Burgos 2873, Soria 3504, and the Escorial, 3683 feet above the sea-level. But even these altitudes do not wholly account for the rigour of the climate in the latitude of Naples, Rome, and Constantinople. We have seen how excellent is the climate of Granada at a nearly equal elevation, only three degrees further south. The extremes of heat and cold felt at Valladolid and Madrid are due more to the uncovered mountain ranges to the north, the treeless, waterless plains, over which the wind sweeps unchecked, than to mere elevation. The want of rain is greatly owing to the ranges of mountains parallel to the frontier and to the Atlantic in Portugal, which condense and wring all the moisture from the rain-clouds of the Atlantic, and distribute it almost wholly on the western slope. Thus at Lisbon the fall is 29, at Coimbra 35, at Oporto 63, in the mountains of Beira and Tras os Montes from 68 to 100 inches; while on the eastern slope, at Salamanca it is 9, Valladolid 12, at Badajoz 12½, Ciudad Real 14. From the bare granite range of the Guadarrama steals down the treacherous icy wind so fatal in Madrid—not sufficiently strong to extinguish a candle, but quite enough to destroy human life. It is the dislike of the Castilian peasant to trees, which would overshadow so much of his small property, the destruction of the mountain forests, and the want of good agriculture, which has embittered the climate of these plateaux. Were the hill-sides clothed with wood, the country dotted with farms, the wide and bare plains covered throughout the year with varied agricultural produce, the climate would soon be modified and become sensibly warmer, and no longer, as it at present is, an obstacle to civilization and to improvement. In spite of all neglect these plains grow some of the finest wheat in Europe, and the lower mountain ranges supply pasture in the summer for the immense flocks which return to winter in the plains of Estremadura. The average temperature of Madrid is 59°, its maximum 104° to 107°, and its minimum only 7°. That of Salamanca is said to be 57°, with a maximum of 97°, and a minimum of 12°. The average rainfall of Madrid is only from 9 to 14 inches, that of Salamanca 9, while Soria, nearer to the mountains, in some years reaches 25 inches.
From the above sketch of the climate the reader will expect to find the productions vary greatly in the different districts. The north and north-west are the lands of cattle and of pasture. In Galicia and in the Asturias the products are almost like those of the warmer parts of the south-west of England and of Ireland, save that in the more sheltered valleys the orange, citron, and pomegranate flourish; a palm is even now and then to be seen; and the wine, especially on the confines of Portugal, is excellent, and needs only more care in preparation to be a rival to the famous Port of the neighbouring country. In the eighteenth century, that of Ribadavia was considered to be the finest wine in all Spain. Maize, too, is freely grown; but on account of their extreme poverty, rye and spelt often replace both it and wheat as food for the peasantry. The upland plateaux afford excellent pasture, especially for cattle and horses; the hardy and sure-footed hacks of Galicia and the Asturias are celebrated. The mountains here are often clothed with wood; oaks of various kinds, and the edible chestnut, and the hazel-nut—of which over 1000 tons, value 23,000l., are annually exported from Gijon—grow on the lower spurs, giving food to herds of swine; beech, and pine, and fir appear as we approach the tops. In the lower woods the arbutus especially flourishes, and the young wild boars in autumn are said to become half stupefied with its narcotic berries. As we proceed eastward from Galicia to the Asturias the climate becomes sensibly colder—the valleys face the north instead of the west; the orange is less known, the mulberry will not flourish sufficiently well to pay for silk cultivation, the olive will not grow, and the cork does not pay for cultivation; the wines lose somewhat of their strength and lusciousness; and cider, made from the excellent apples of the country, rivals the juice of the grape in popularity. The mountains are covered with heath, and fern, and furze, but the aromatic plants are fewer than in Galicia. This description applies to the northern slope of the Cantabrian chain and to the rolling hills and plateaux of the Basque provinces; but the southern slopes of the chain, towards the Ebro, are again a land of vine and olive, and of maize, which is everywhere the staple. In the Basque provinces the plough is replaced by the ancient "laya," an instrument as old, at least, as Roman times. It is a heavy two-pronged steel or iron fork, with prongs one and a half to two feet long. A strong man will work two of them at once, one in each hand, driving them into the ground to their full depth, then with a backward strain turning up the deep soil. Usually, four or five men work together, and raise their arms, plunge the fork downwards, and heave, in perfect time. The cultivation thus effected is excellent, but the expenditure of labour is immense The productions do not vary greatly along the slopes of the Pyrenees from those above described until we reach Catalonia; but in the lower valley of the Ebro, where rain is rare, in the Bardeñas reales of Navarre, and in the monegros, or despoblados of Aragon, we meet with a phenomenon only too frequent in Spain—tracts of almost utter barrenness. The Bardeñas reales are low spurs of the Pyrenees, with table-lands, bluffs, and deep gorges, and these could scarcely be brought under cultivation; but the "despoblados" (dispeopled lands) of Aragon might be irrigated, either by the Ebro or by its tributaries, if the water of the canal of Charles V. were but economically applied. The sterility of some parts seems to have been the slow result of an oppressive land tenure; for as Don Vicente de la Fuente has remarked, the lands which belonged to the ancient señors (the feudal lords) lie barren, while the lands of the comunidades, the free districts, are still fertile. In treating, of the cultivation and the products of eastern and southern Spain two facts become evident at once—how many of the products are exotic, and how much of the cultivation is still Arabian. We shall see in another chapter how deep a mark the Moor or Arab has left on the population and toponymy of Spain; and the agriculture of the greater part of central and southern Spain is still Arabian. The methods of the Spanish peasant are almost all Arabian; often he uses the Arabian hoe in preference to the Roman plough. The noria, or water-wheel; the sha'doof, or swipe, the pole and bucket for lifting water; the huge dams and reservoirs, the canals and ditches (acequias), the regulations for the fair distribution of the water,—all these, and even the very superstitions as to times of sowing, the rotation of crops, the treatment of his animals—for all these the Spanish peasant of the South is indebted to the Moors. The treatise of Abu Zaccaria, with its traditions of Nabathean agriculture, is still one of the manuals of agriculture in Spain. It is the Moors, too, who first made the winter gardens in the sands near San Lucarde Barameda, at the mouth of the Guadalquiver, and which supply Cadiz and Seville with the earliest and latest vegetables. The Roman, with his lofty aqueducts, brought water to the towns; but it was the Moor who gave that blessing to the thirsty soil of the country districts of Spain. And not only the methods of agriculture, but