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For hydrographic purposes the surface of Spain is divided by the Instituto Geográfico into the following ten basins: (1) the Eastern Pyrenees, basin of the Rivers Muga, Fluvía, Ter, Tordeva, Besós, Llobregat, Foix, and Francolí; (2) the basin of the Ebro, to the south and west of the preceding, containing the Nela, Zadorra, Ega, Arga, Aragón, Arba, Gallego, Cinea, and Segre, affuents of the Ebro, on its right side, and the Oca, Tiron, Oja, Najerilla, Iregua, Alhama, Jalon, Huerva, Aguas, Martin, Guadalope, Matarrana, and other smaller affuents on its left; the south-eastern region, watered by the Cenia, Migares, Palancia, Turia (or Guadalaviar), Jucar, Serpis, Vinalopó, Segura, and Almanzora; (4) the southern region, intersected by small streams, the most important rivers being the Almería, Adra, Guadalfeo, Guadalhorce, Guadiaro, and Guadalete; (5) the basin of the Guadlaquivir, the affluents of which are, on the right, the Rivers Borosa, Guadalimar, Rumblar, Jandula, Yeguas, Guadamellato, Guadiato, the Brook of Huesna, the River Viar, and the Brooks of Cala, Huelva, and Guadiamar, and on the left, the Guadiana Menor, Genil, Guadabullón, Guadojoz, Corbones, Guadaira, and Salado de Morón; (6) the basin of the Guadiana, with its tributaries, the Záncara, or Cigüela, Bullaque, and Gévora, on the right, and the Javalón, Zujar, Ardila, and Chanza, on the left; (7) the basin of the Tagus, which river rises in the Province of Teruel, in the Sierra de Molina, and receives, on the right, the Gallo, Jarama, Guadarrama, Alberche, Tiétar, Alagón, and Eljas, and, on the left, besides other streams of slight importance, the Guadiela and the Almonte.The Jarama, in its turn, receives the Lozoya, Guadalix, Manzanares (which flows by Madrid), Henares, and Tajuña; (8) the basin of the Douro, which rises in the Peña (Rock) Urbion, in the Province of Logroño, 7216 feet above the sea level.Owing to the diversity of formations described above, and the elevation of the central portions, the surface of the Peninsula is, in general, of an uneven character with a very unequally distributed irrigation, some regions enjoying a wonderful fertility, while others are nothing but steppes.In other parts, again, the abrupt slope of the ground is such that the rains produce torrential floods in the rivers and thus negative their beneficial action.No Permian formation is to be found in Spain, nor does there appear any Triassic worth mentioning, the formations of these two periods having been submerged during later periods.During the Jurassic period long parallel tracts were formed along the present courses of the Ebro and the Turia, as well as a great mass between Jaén, Granada, Malaga, Osuna, and Montilla.


of Greenwich, on the west, Cape Tirinana, in longitude 9° 17' 33" W. The total area of the Spanish territory in the Peninsula is 194,563 square miles, with a coast line of 2060 miles in length.

The Quaternary formations are found chiefly on the east coast and the Provinces of Madrid (northwest), Segovia, Valladolid, Palencia, and Asturias, and the basins of the principal rivers.



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