The
Pyrenees (also spelled
Pyrenées) (; ; ; ; ; ) are a
range of mountains in southwest
Europe that form a
natural border between
France and
Spain. They separate the
Iberian Peninsula from the rest of continental Europe, and extend for about from the
Bay of Biscay (Cap Higuer) to the
Mediterranean Sea (
Cap de Creus).
For the most part, the main crest forms a massive divider between France and Spain, with the tiny country of
Andorra sandwiched in between.
Catalonia and the
Basque Country have historically extended on both sides of the mountain range, with small northern portions in France and much larger southern parts in Spain.
Etymology
Pyrene is the nymph of
classical mythology who, according to legend, gave its name to the Pyrenees.
This legend attempts to explain how a mountain range that was worshipped as a god by the early inhabitants came to be.
According to the legend, the hero
Heracles came
Iberia, with the purpose of stealing the oxen of Gerión, a monstrous giant who attempted to possess the nymph Pyrene. But Pyrene fled and hid in an area between Spain and France. Gerión then burned the entire area in order to find her. Pyrene, on the verge of burning to death, shrieked and cried in desperation, and her tears created the mountain lakes. Heracles heard her and came to her rescue. When he found her, the
nymph was already in agony and only had time enough to tell the hero what has happened.
Heracles, deeply moved by Pyrene’s tragic ending, erected a mausoleum over her dead body, by piling up all the stones and rocks he could find, thus creating a great mountain range that he called the Pyrenees in memory of Pyrene.
Geography
The
Spanish Pyrenees are part of the following
provinces, from east to west:
Girona,
Barcelona,
Lleida,
Huesca,
Navarra, and
Guipúzcoa.
The
French Pyrenees are also part of the following
départements, from east to west:
Pyrénées-Orientales,
Aude,
Ariège,
Haute-Garonne,
Hautes-Pyrénées, and
Pyrénées-Atlantiques (the latter two of which include
Pyrenees National Park).
The independent principality of
Andorra is sandwiched in the eastern portion of the mountain range between the
Spanish Pyrenees and
French Pyrenees.

Composite satellite image of the Pyrenees (
NASA)
Physiograpically, the Pyrenees are typically divided into three sections: the Atlantic (or Western), the Central, and the Eastern Pyrenees. Together, they form a distinct physiographic province of the larger Alpine System division.
The Central Pyrenees extend westward from the
Aran Valley to the
Somport pass, and they include the highest summits of this range:
In the Western Pyrenees, the average elevation gradually increases from the west to the east, from the
Basque mountains near the
Bay of Biscay of the
Atlantic Ocean. In the Eastern Pyrenees, with the exception of one break at the eastern extremity of the Pyrénées Ariégeoises, the mean elevation is remarkably uniform until a sudden decline occurs in the easternmost portion of the chain known as the Albères.
Geology
The Pyrenees are older than the
Alps: their
sediments were first deposited in coastal basins during the
Paleozoic and
Mesozoic eras. Between 100 and 150 million years ago, during the Lower
Cretaceous period, the Bay of Biscay
fanned out, pushing present-day Spain against France and putting large layers of
sediment in a vise grip. The intense pressure and uplifting of the Earth's crust first affected the eastern part and stretched progressively to the entire chain, culminating in the
Eocene epoch.
The eastern part of the Pyrenees consists largely of
granite and
gneissose rocks, while in the western part the granite peaks are flanked by layers of
limestone. The massive and unworn character of the chain comes from its abundance of
granite, which is particularly resistant to
erosion, as well as weak
glacial development.
Landscape
Conspicuous features of Pyrenean scenery are:
- the absence of great lakes, such as those that fill the lateral valleys of the Alps
- the rarity and great elevation of passes
- the large number of the mountain torrents locally called gaves, which often form lofty waterfalls, surpassed in Europe only by those of Scandinavia
- the frequency with which the upper end of a valley assumes the form of a semicircle of precipitous cliffs, called a cirque.
The highest
waterfall is
Gavarnie (462 m or 1,515 ft), at the head of the
Gave de Pau; the
Cirque de Gavarnie, in the same valley, together with the nearby Cirque de Troumouse and
Cirque d'Estaubé are notable examples of the
cirque formation. Low passes are lacking, and the principal roads and the railroads between France and Spain run only in the lowlands at the western and eastern ends of the Pyrenees, near sea level. Between the two ends of the range, the only passes worth mentioning are the
Col de la Perche, between the valley of the
Têt and the valley of the
Segre, the
Port d'Envalira, the highest mountain pass in the Pyrenees and one of the highest points of the European road network, and the Col de
Somport or Port de Canfranc, where there were old
Roman roads, but apparently, no modern highways.
A notable visual feature of this
mountain range is
La Brèche de Roland, a gap in the ridge line, which - according to legend - was created by
Roland.
Natural resources

A waterfall in the Spanish Pyrenees
The metallic
ores of the Pyrenees are not in general of much importance now, though there were
iron mines at
Vie de Sos in Ariège and at the foot of
Canigou in
Pyrénées-Orientales long ago.
Coal deposits capable of being profitably worked are situated chiefly on the Spanish slopes, but the French side has beds of
lignite. The open pit of Trimoun (Ariège) is one of the greatest sources of
talc in Europe.
Mineral springs are abundant and remarkable, and especially noteworthy are the
hot springs, of which the Alps are very deficient. The hot springs, among which those of
Panticosa,
Lles,
Bagnères-de-Luchon and
Eaux-Chaudes may be mentioned, are
sulphurous and mostly situated high, near the contact of the granite with the stratified rocks. The lower springs, such as those of
Bagnères-de-Bigorre (
Hautes-Pyrénées),
Rennes-les-Bains (
Aude) and
Campagne (Aude), are mostly selenitic and not very cold.
Climate
The amount of the
precipitation the range receives, including
rain and
snow, is much greater in the western than in the eastern Pyrenees, because of the moist air that blows in from the
Atlantic Ocean over the
Bay of Biscay. After dropping its moisture over the western and central Pyrenees, the air is usually dry over the eastern Pyrenees.
This all leads to a marked contrast between different sections of the mountain range in more than one respect. Some
glaciers are found in the western and especially the snowy central Pyrenees, but the eastern Pyrenees are without any glaciers - with the quantity of snow falling there being insufficient to cause their development. The glaciers are confined to the northern slopes of the central Pyrenees, and do not descend, like those of the Alps, far down into the valleys, but have their greatest lengths along the direction of the mountain chain. They form, in fact, in a narrow zone near the crest of the highest mountains. Here, as in the other great mountain ranges of central Europe, there is great evidence of a much wider extension of the glaciers during the
Ice Ages. The case of the glacier in the valley of Argeles Gazost, between Lourdes and Gavarnie, in the
département of Hautes-Pyrénées is the best-known instance.
The snow-line varies in different parts of the Pyrenees from about 2,700 to 2,800 meters above sea level.
Flora and fauna

A mountain stream
A still more marked effect of the preponderance of rainfall in the western half of the chain is seen in the vegetation. The lower mountains in the extreme west are wooded, but the extent of forest declines eastwards, and the eastern Pyrenees are peculiarly wild and barren, all the more since it is in this part of the chain that granitic masses prevail. There is a change, moreover, in the composition of the flora in passing from west to east. In the west the flora resembles that of central Europe, while in the east it is distinctly Mediterranean in character, though the difference of latitude is only about 1°, on both sides of the chain from the centre whence the
Corbières stretch north-eastwards towards the central plateau of France. The Pyrenees are relatively as rich in
endemic species as the Alps, and among the most remarkable instances of that endemism is the occurrence of the monotypic genus
Xatardia (family
Apiaceae), only on a high alpine pass between the
Val d'Eynes and
Catalonia. The genus most abundantly represented in the range is that of the
saxifrages, several species of which are endemic here.
The
Pyrenean Ibex mysteriously became extinct in January 2000; the native Pyrenean
brown bear was hunted to near-extinction in the 1990s, but it was re-introduced in 1996 when three bears were brought from
Slovenia. The bear population has bred successfully, and there are now believed to be about 15 brown bears in the central region around Fos, but only four native ones are still living in Aspe valley.
In their
fauna the Pyrenees present some striking instances of
endemism. The
Pyrenean Desman is found only in some of the streams of the northern slopes of these mountains, but the only other member of this genus are confined to the rivers of the
Caucasus in southern
Russia. The Pyrenean euprocte (
Euproctus pyrenaicus), an endemic relative of the
salamander, also lives in streams and lakes located at high altitudes. Among the other peculiarities of the Pyrenean fauna are blind insects in the
caverns of Ariège, the principal genera of which are
Anophthalmus and
Adelops.
Protected areas

Ordesa y Monte Perdido National Park, Spain
Principal nature reserves and national parks:
Demographics and culture
The Pyrenean region possesses a varied ethnology,
folklore and history: see
Andorra;
Aragon;
Ariege;
Basque Country;
Béarn;
Catalonia;
Navarre;
Roussillon. For their history, see also
Almogavars,
Marca Hispanica.
The principal languages spoken in the area are
Spanish,
French,
Catalan (in
Catalonia and
Andorra),
Basque, and
Aragonese. Also spoken, to a lesser degree, are the
Occitan language (the
Gascon and
Languedocien dialects in France and the
Aranese dialect in the
Aran Valley).
Sports and leisure
Both sides of the Pyrenees are popular spots for winter sports such as
alpine skiing and
mountaineering. The Pyrenees are also a good place for European and North African athletes to do high-altitude training in the summertime, such as by
bicycling and cross-country running.
In the summer and the autumn, the Pyrenees are usually featured in two of cycling's epic grand tours, the
Tour de France held annually in July and the
Vuelta a España held in September. The stages held in the Pyrenees are often crucial legs of both tours, drawing hundreds of thousands of spectators to the region, too.
Three main
long-distance footpaths run the length of the mountain range; the
GR 10 across the northern slopes, the
GR 11 across the southern slopes, and the
HRP which traverses peaks and ridges along a high altitude route. In addition, there are numerous marked and unmarked trails throughout the region.
Pirena is a dog-
mushing competition held in the Pyrenees.
Ski resorts
Ski resorts in the Pyrenees include:

Formigal (Spain), one of the major ski resorts
Highest summits

Monte Perdido
Notable summits below 3,000 meters

Pic du Midi d'Ossau
See also
thumb|250px|Posets peak seen from Viadós.