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Sixth
community in extension, 6,3 % of the Spanish territory and
the second most populated, with 15,6 % for what the first
positions occupies in population density. The industrialization
of the zone has done that to the natural growth is necessary
to add the great immigration, principally in the sixties and
beginning of the seventies. In the 13th century, under the
Hispanic Mark authority the Autonomous government of Catalonia
is created, inside the Catalan Spanish Parliament, being promulgated
the first civil laws. In the Low Middle Ages it joins the
Wreath of Aragon, the trade being stimulated by the Mediterranean
and the emergence of the middle class, sat down the bases
of an industrial development. The Catalan language is previous
to the political institutions. The first written texts, of
religious character, go back to the 10th century.
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They
alternate the mountain landscapes (Pyrenees and Coastal -
Catalan Mountain chain), the interior plains and the littoral.
The Aigües Tortes's national Park and Lake San Mauricio
(1.957) stand out in the Pyrenees, importantly for its quaternary
glacierism. In the interior plains Montserrat's mountain range
stands out with strong differences, composed by conglomerates,
which hardness stands out in the middle of the landscape,
though with some showy fractures.
The
units of relief arise with the Alpine orogenia. The following
ones can be distinguised:
Catalan
Pyrenees: it spreads from the Monte Perdido and the Maladeta
up to Creus's Cape, where it is possible to distinguish the
axial zone and the pre- Pyrenee is limy. Higher summits are
in the bordering zone with Aragon.
The
Central Depression crossed by the river Ebro in its North-East
sector
The
Coastal - Catalan Mountain chains, in the north zone predominance
of granitic and slaty materials of paleozoic origin, whereas
in the south zone they predominate over limy mesozoic sediments.
The interior zone reaches heights of 1.500 m and in the littoral
of 200 m.
To
mention the Transverse Catalan Mountain chain, which
joins the Pyrenees with the coastal - Catalan Mountain chain,
its reliefs close for the North-East the Ebro Depression coming
up to the gulf of Roses, and the coastal plains that include
the delta of the Ebro and of the Llobregat.
High
Earths of the Pre- Pyrenees,
with rainfalls over the 600 mm/year. In this zone the basin
of the Segre is the one that has a drier summer.
Mediterranean
with oceanic influence, with a maximum of rainfalls in
the equinoxes and risk of torrential rains in autumn. A dry
and warm summer and a winter with soft temperatures in general.
Continental
Mediterranean in the Central Depression, which is most
accused in the western zones. Of minor rainfalls, in any areas
they do not come to the 300 mm/year. The thermal daily and
annual extent is marked.
Mountain,
which it is possible to define like Alpinly and subAlpinly,
is characterized by a bigger quantity of rainfalls, regularly
distributed the whole year and in occasions in the snow shape.
It
changes depending on the relief units :
Pyrenees
zone : it begins with the grove of evergreen oaks followed
by the oak with scots pines, sometimes the black pine appears
in height, alternating with beeches in more humid or colder
zones. In bigger heights we enter the fir and the top meadows
and perpetual snow.
In
the Littoral, the oak forest is very degraded by the
repopulation with pines very adapted to the drought and stone
pines, on Silica soils the blockhead.
In
the Central Depression the forest is absent and it
gives the bushes with thyme, lavender, etc up to connecting
with the Aragonese steppe.
The
rivers cut transversely the mountains in E-O, NE and SO direction
, facilitating the communications among the regions. The Pyrenean
rivers are short, save big unevennesses and are taken advantage
for the obtaining of hydroelectric energy. Among the Pyrenean
rivers we can emphasize the Fluviá, Ter, Llobregat,
etc, among the properly Mediterranean ones there are the Congost
and Mogent, which contribute its waters in the Besós,
and the Francolí, without forgetting the river Ebro
that ends on the Catalan coast after crossing several Autonomies.
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