Ordesa Valley

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File:Bosque Fanlo-Sarvisé (Huesca, Pirineo Aragonés).JPG
In autumn, Bosque de La Pardina del Señor, between Fanlo and Sarvisé.
File:Parque nacional de Ordesa y Monte Perdido, Huesca, España, 2015-01-07, DD 09-10 HDR.JPG
River in Cotatuero

The Ordesa Valley is a glacial valley in Aragon, in the Spanish Pyrenees, forming part of the Ordesa y Monte Perdido National Park. The valley is approximately Script error: No such module "convert". long.[1]

History

The Ordesa Valley was first documented in 1820 and was later mapped in detail during the 1920s.[1] It became part of the Ordesa y Monte Perdido National Park in 1918, making it one of Spain's earliest protected natural areas.[2]

Geography

The valley's east–west orientation, which is unusual in the Pyrenees, allows Atlantic Ocean influences, contributing to its moderate climate.[3]

The Arazas River flows through the valley, creating multiple waterfalls, such as the Cola de Caballo (Horsetail Waterfall).[4]

Ecology and conservation

The valley hosts diverse ecosystems, ranging from subalpine forests to high-mountain meadows. Notable tree species include Scots pine (Pinus sylvestris), Silver fir (Abies alba), and European beech (Fagus sylvatica).[5]

It also has one of Europe’s largest populations of the Pyrenean Chamois (Rupicapra pyrenaica).[6] Other wildlife includes griffon vultures (Gyps fulvus), golden eagles (Aquila chrysaetos),[7] and brown bears (Ursus arctos),[8] though the latter are extremely rare.

Designated a UNESCO Biosphere Reserve in 1997, the park implements measures to balance tourism with habitat protection, including restricted access zones.[9][10]

Geology

The valley's formation stems from the collision of the Iberian and Eurasian tectonic plates during the Alpine orogeny, creating folds and faults in its limestone and dolomite bedrock.[11] Erosional processes further shaped the terrain:  

  • Glacial activity carved the U-shaped Ordesa and Pineta valleys, while river erosion formed the Añisclo and Escuaín canyons.[9]
  • Karstification produced features like underground drainage systems and sinkholes, contributing to the valley’s aridity at higher elevations.[11]

At the north-east end of the valley, several prominent peaks can be seen, including:

These three peaks form part of the Monte Perdido Massif, dominating the northeastern end of the valley.[12]

Tourism

The valley’s trails attract over 600,000 annual visitors:  

  • Cola de Caballo Route: A 17.5 km round-trip trail leads to the iconic "Horsetail" waterfall, passing landmarks like the Gradas de Soaso cascades and Circo de Soaso glacial cirque.[13]
  • Faja de Pelay: A challenging 22 km loop offering cliffside views from the Senda de los Cazadores path.[9][13]
  • Góriz Refuge: A key basecamp for ascents of Monte Perdido and adjacent peaks.[9]

Visitor management includes shuttle buses from Torla to reduce traffic and trail erosion.[10][13]

References

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  1. ↑ a b Script error: No such module "citation/CS1".
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  5. ↑ Ninot, J.M., Ferré, A., Grau, O., Font, X., Pérez-Haase, A. & Carrillo, E. Environmental drivers and plant species diversity in the Catalan and Andorran Pyrenees. Lazaroa 34: 89-105 (2013).
  6. ↑ Script error: No such module "Citation/CS1".
  7. ↑ Script error: No such module "citation/CS1".
  8. ↑ Script error: No such module "citation/CS1".
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  10. ↑ a b Script error: No such module "citation/CS1".
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External links

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