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Nature LIÉBANA |
It is a closed territory which can only be accessed, from the north, through the Hermida gorge. This is, along a scenic road which follows the river Deva and runs parallel to it, boxed by rugged and almost vertical limestone walls, some of them more than 600 m high. This is a region of a surprising climatic variety, where a properly Mediterranean micro-climate contrasts with the rigours of the alpine meteorology in the highest areas. A natural reserve where some autochthonous tree species still remain like: evergreen and cork oaks, Pyrenean oaks and beech trees, which form intricate and beautiful woods in which a few protected species survive, like the brown bear, the road deer or the cappercaille. |
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| SITUATION AND ACCES |
On the north, the Picos de Europa massif, declared National Park, with the peacks of Santa Ana (2,.596 m) and the Tesorero (2,570 m); on the west, Peña Remoña (2,247 m) and the Coriscao (2,234 m); on the south, the highland passes of Pineda (1,738 m); San Glorio pass (1,609 m), Sierras Albas (1,306 m) and Piedras Luengas pass (1,373 m); and, finally, on the east, Peña Sagra (2,042 m) and Taruey pass, conform the main heights. Liébana is located inside this knot of mountains, defined by their municipalities: Camaleño and Cillorigo, crossed by the Deva river; Vega de Liébana or Cereceda, where the waters of the Quiviesa river flow through; Pesaguero and Cabezón de Liébana, crossed by the Bullón river, and, in the center, the village of Potes. To Liébana you can arrive by means of three important communication roads; the San Glorio pass (1,609 m), from León; the Piedras Luengas pass (1,313 m), from Palencia, and following the coast, through Unquera and Panes, crossing the impressive gorge of La Hermida. |
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| RIVERS |
The Bullón river, with its source in Peña Labra, descends through the municipalities of Pesaguero and Cabezón de Liébana until it joins the Deva in Ojedo. Finally, the Quiviesa river, born in San Glorio´s pass, flows down through the municipality of Vega de Liébana and joins the Deva river in the village of Potes. |
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| GEOLOGY |
Limiting with Palencia the slate and sandstone appear, belonging these to the Silurian, Devonian and Carboniferous periods and are, without doubt, the eldest rocky formations in Cantabria. The red brownish sandstones from the Triassic, and the compact conglomerates from the Carboniferous are in the north-eastern area of the region. Also, one can contemplate a series of material deposits of glacial and fluvial origin, mainly in Fuente Dé, Aliva, Peña Vieja and the Hermida gorge. |
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| CLIMATE, VEGETATION AND FAUNA |
During the months from November to January frosts are usual, although under this conditions there is less snow. Finally we should make special mention to the autumnal season, with dry weather and soft temperatures, and when nature in the region acquires a very special beauty, which shows mainly in its wood colours, with a variety of worthy to mention tones.
Beech woods are the most numerous in Liébana, located on shady hillsides from 600 to even 1,700 meters. Birch is found in small groves, in the top limit of some beech woods and the chestnut tree shows up in mixed forests or as isolated and centenarian individuals; cork oaks or (sufras) are generally located on sun exposed hillsides, from 400 to 800 meters.
The region has a rich and important variety of fauna, standing out some species in danger of extinction like the brown bear, cappercaille, golden eagle and the sporadic presence of wolf individuals. Roe deer, red deer and, the Chamoi in the peacks, are also very abundant, the same as wild boar, which is hunted in a regulated way in all the different valleys. In the rivers, the trout, the eel and the salmon, are very appreciated species. |
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| RESOURCES |
Liébana´s underground is very rich and there has been an important succession of mining exploitations, mainly in Picos de Europa, highlighted by the presence of the caramel blende (zinc sulfurate), and some locations of calamine (zinc carbonate) and galena (lead sulfurate). The last exploitation was the mine of Aliva, closed up some years ago. The surface area in Liébana is 57,483 hectares, distributed the following way: working lands, 566 hectares; grasslands, 12,294 hectares; forest land, 37,768 hectares; barren, 253 hectares; unproductive, 5,929 hectares and, other surfaces, 673 hectares.
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| PRODUCTS AND GASTRONOMY |
The artisan cold meat selection is excellent: "chorizos" (spicy sausages), pork loin, black and local black pudding, bacon, etc., as well as other exquisite meats, since livestock is bred in green and rich pasture lands.
The "Quesucos de Liébana" are also smaller cheeses with a mixture of different milks, using cow, sheep and goat´s, which can also come smoked or without kippering. They have a cylindrical or discoidal shape, are quite fatty, and have a firm and compact paste. When the "quesuco" is kippered it acquires a colour, scent and characteristic flavour.
Traditional cooking in Liébana is of extremely good quality, due to the fact that its raw materials are of unquestionable prestige. Full of flavour meats, exquisite to visitors; vegetables from the market gardens; trout and salmon from the rivers; legumes from the land; seasonal mushrooms; delicious lebaniego stew; home-made desserts, elaborated through generations; a variety of superior quality cheeses, and the mountain tea with "orujo", make the arriving visitor enjoy traditional cooking with first quality products. Traditional cooking is always present at the great variety of hostelry establishments distributed through the different municipalities in the district of Liébana. |
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| Towns | Nature | History | Monuments | Routes | Leisure |
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