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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.The unevenness of the country at the same time results in great differences of climate.The Spanish Peninsula has also been called the Iberian, from its original inhabitants, and (by synecdoche) the Pyrenean, from the mountains which bound it on the north.As the Spaniards named one part of America — Mexico — Nueva España (New Spain), we speak of "the Spains", in the plural, to signify the Spanish possessions.The contrast extends even to the seas surrounding Spain — the tranquil Mediterranean, the stormy Bay of Biscay, and the Atlantic with a character midway between.

The eastern portions of the Peninsula were built up during the Cretacean period, while, between these formations and the Granitic and Silurian, extensive lakes were left which have since disappeared but which may still be traced in the level steppes of Aragón and the two Castiles.The elevated plains of the centre are intersected by mountain ranges.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.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.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.

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