Picos de Europa oor Galisies

Picos de Europa

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Picos de Europa

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The Picos de Europa.
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Unlike the heights of the Picos de Europa further to the south, these valleys are green and pastoral.
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Some zones of Picos de Europa, over 2,500 metres high, have an alpine climate with snow persisting year round.
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Llanes lies to the north of the Picos de Europa, a mountain range whose geology is almost entirely of limestone karst.
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It is a cave in the Picos de Europa mountains, which gives its name to the parish of Covadonga in the municipality of Cangas de Onís.
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Only Liébana for its geographic position in Picos de Europa, Trasmiera and Campoo, in the Ebro basin are established are clearly defined comarcas in the region.
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The economy of the comarca of Liébana has shifted from the primary sector to the rural tourism boom, thanks to its landscapes and the appeal of the Picos de Europa National Park.
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The town of Potes is located at the confluence of four valleys, near where the River Quiviesa flows in the River Deva, the latter born at altitudes of the Picos de Europa.
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The great limestone masses of Picos de Europa also stand out in the southwest of the region: most of their summits exceed 2,500 m, and their topography is shaped by the former presence of glaciers.
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So, while in the bottom of the valley of Liébana a Mediterranean climate can be enjoyed, it shifts progressively as we ascend to a humid Atlantic climate until subalpine conditions are reached in the high peaks of Picos de Europa.
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The Urrieles Massif or the Central Massif is a mountainous massif in the north of Spain, one of the three massifs that make up the Picos de Europa, and in turn, one of the stretches of the Cantabrian Massif belonging to the Cantabrian Range.
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