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Domingo de la Calzada, Haro, and Briviesca, another lake which then covered the sites of Burgos, Valladolid, León, Zamora, and Salamanca.Another extension of the Eocene formation was from the region where Madrid now stands to that of Albacete and Murcia.The general structural form of the Peninsula is somewhat that of a truncated pyramid, sloping abruptly towards the west, but gently towards the east.The elevated plains of the centre are intersected by mountain ranges.The upheaval of the land went on during the Devonian and Silurian epochs until it formed what is now the whole of Galicia, part of the Asturias, León, and Zamora, and as far down as Toledo, Ciudad Real, Cordova, Huelvas, and the Algarves, while, to the east and north, were formed the Catalonian coast and a great part of the Pyrenees.Large islands arose in the neighbourhoods of Burgos, Soria Daroca, Granada, Malaga, and Gibraltar.To the south-east of this was another island, where is now Bejar and Sierra de Gredos, comprising part of the Provinces of Avila, Segovia, and Toledo.To the north-east, the Pyrenees and the Catalonian coast took the form of islets, while in other directions other islets occupied the sites of Lisbon, Evora, Cáceres, Badajoz, Seville, Cordova, and Jaén.

Since the political separation of Portugal, however, the name has gradually come to be restricted to the largest of the four political divisions of the Peninsula: (1) Spain; (2) Portugal; (3) the Republic of Andorra; (4) the British possession of Gibraltar, at the southern extremity.The mountain masses may be divided into six groups: (1) the northern, consisting of the Pyrenees on the east and the Cantabrian Range on the west, and terminated by Capes Creus and Finisterre; (2) the Iberic, or eastern, comprising the mountains which bound the basin of the Ebro and extend as far as Cape Gate; (3) the central system, the Carpetan, or Carpeto-Vetonic, Range, so called from the Carpetani and Vetones who inhabited its slopes in ancient times; (4) the Mountains of Toledo, or Cordillera Oretana; (5) the Betic system, or Cordillera Mariánica, forming the right-hand side of the basin of the Betis, or Guadalquivir, and the chief part of which is the Sierra Morena; (6) the Penibetic system, extending from the Sierra Nevada to Cape Tarifa.The highest elevations are: Maladeta (11,004 ft.) and Pico de Nethou (11,168 ft.), in the Pyrenees: Peña de Corredo (8784 ft.), and Moncayo (7593 ft), in the Cantabrian Range; Plaza del Moro Almanzor (8692 ft.), in the Carpetan Range; the plateau of Corocho de Rocigalgo (4750 ft.), in the Toledo Mountains; Estrella (4260 ft.), in the Betic Range; Mulhacen (11,417 ft.) and Veleta (11,382 ft.) in the Penibetic.Its four extreme points are: on the north, the Estaca de Vares, in N. 43° 47' 32"; on the south, the southern extremity of the Island of Tarifa, in S. 35° 59' 49"; on the east, Cape Creus, in longitude 3 ° 20' 16" E.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.

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