A History of Spain: founded on the Historia de España y de la civilización española of Rafael AltamiraChapman, Charles E. (Charles Edward)
History
A History of Spain: founded on the Historia de España y de la civilización española of Rafael Altamira
Chapman, Charles E. (Charles Edward)
Spain -- Civilization; Spain -- History
The greatest average elevation in Spain is found in the centre, in
Castile and Extremadura, whence there is a descent, by great steps as it
were, to the east and to the west. On the eastern side the descent is
short and rapid to the Mediterranean Sea. On the west, the land falls by
longer and more gradual slopes to the Atlantic Ocean, so that central
Spain may be said to look geographically toward the west. There is an
even more gentle decline from the base of the Pyrenees to the valley of
the Guadalquivir, although it is interrupted by plateaus which rise
above the general level. All of these gradients are modified greatly by
the mountain ranges within the peninsula. The Pyrenean range not only
separates France from Spain, but also continues westward under the name
Cantabrian Mountains for an even greater distance along the northern
coast of the latter country, leaving but little lowland space along the
sea, until it reaches Galicia in the extreme northwest. Here it expands
until it covers an area embracing northern Portugal as well. At about
the point where the Pyrenees proper and the Cantabrian Mountains come
together the Iberian, or Celtiberian, range, a series of isolated
mountains for the most part, breaks off to the southeast until near the
Mediterranean, when it curves to the west, merging with the Penibética
range (better known as the Sierra Nevada Mountains, the name of that
part of the range lying south of the city of Granada), which moves
westward near the southern coast to end in the cape of Tarifa.
[Sidenote: Geographical divisions of the peninsula.]
Public-domain text, read in full here on John Shaqi.
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