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Aneto

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Parent: Pyrenees Hop 4
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Aneto
NameAneto
Photo captionAneto from the Portillón Superior
Elevation m3404
Prominence m2812
ListingUltra prominent peak, Highest point of the Pyrenees
LocationProvince of Huesca, Aragon, Spain
RangePyrenees, Maladeta massif
Coordinates42, 37, 56, N...
First ascent20 July 1842 by Platon de Tchihatcheff and party
Easiest routeGlacier climb/scramble

Aneto. It is the highest mountain in the Pyrenees, with an elevation of 3,404 metres, and dominates the Maladeta massif in the Province of Huesca, Aragon, Spain. The peak's summit is famously marked by a large cross and features the most extensive glacier in the range, which has been in significant retreat due to climate change. First ascended in the mid-19th century, it is now a major objective for mountaineers and trekkers from around the world, offering challenging routes and access to the stunning landscapes of the Posets-Maladeta Natural Park.

Geography and location

Aneto is situated in the heart of the Pyrenees, the mountain range that forms a natural border between France and Spain. It lies within the Spanish autonomous community of Aragon, specifically in the northern part of the Province of Huesca. The mountain is the central and highest feature of the Maladeta massif, a compact granite batholith that contains several other notable peaks like Pico Maldito and Pico del Medio. The massif is bounded by key valleys including the Valle de Benasque to the south and the Val d'Aran to the north, with major passes like the Port de la Picada and Portillón Superior providing access. The entire area is protected within the Posets-Maladeta Natural Park, a region renowned for its high-mountain ecosystems and glacial landscapes.

Geology and formation

The mountain is composed primarily of granite that formed during the Variscan orogeny, a major mountain-building event in the late Paleozoic era. This granite forms part of the Maladeta batholith, a large igneous intrusion that was later uplifted and exposed by the tectonic forces of the Alpine orogeny, which created the modern Pyrenees. The distinctive jagged ridges and spires, such as those on the Cresta de los Portillones, are the result of intense glacial erosion and periglacial processes during the Quaternary glaciation. The geology of the area is closely studied by institutions like the Instituto Geológico y Minero de España, and the retreating Aneto Glacier provides critical data on climate change impacts in southern Europe.

Climbing and routes

The first successful ascent was achieved on 20 July 1842 by a party led by the Russian explorer Platon de Tchihatcheff, accompanied by guides including Pierre Redonnet and Bernard Arrazau, and local hunters from Benasque. The standard route, known as the Normal Route, approaches from the Refugio de la Renclusa and involves crossing the Aneto Glacier and navigating the famous Pas de Mahoma, a narrow rock bridge, before the final summit ridge. More technical climbs exist on the mountain's formidable north face, with classic lines like the Cresta del Medio and routes on the Pared de Barrañs attracting experienced alpinists. The Federación Española de Deportes de Montaña y Escalada oversees safety and route information, and the ascent is often combined with traverses to neighboring peaks like Pico de Alba or integrated into long-distance treks such as the GR 11.

Flora and fauna

The lower slopes and valleys surrounding the mountain, such as the Valle de Eriste, are covered in extensive forests of black pine and Scots pine, giving way to alpine meadows at higher elevations. The alpine flora is diverse and includes several endemic Pyrenean species, many of which are protected within the Posets-Maladeta Natural Park. Notable fauna includes the Pyrenean chamois, the marmot, and significant bird species like the lammergeier and the golden eagle. The ibex has been successfully reintroduced to the area, and the streams flowing from glaciers like the Glaciar de la Maladeta are habitats for the Pyrenean brook salamander.

History and exploration

While long known to local shepherds and inhabitants of Benasque, the mountain was historically feared and referred to as the "Cursed Peak" (Maladeta) due to its glaciers and frequent accidents. Its scientific exploration began in the late 18th and early 19th centuries with expeditions by figures like the French geologist Louis-François Élisabeth Ramond de Carbonnières. The successful 1842 ascent by Platon de Tchihatcheff's team, which included the painter Federico de Madrazo, marked a pivotal moment in Pyrenean mountaineering. The area later became a focal point for glacial studies by pioneers like Franz Schrader of the Société de Géographie. In the 20th century, the construction of the Refugio de la Renclusa and its management by the Federación Aragonesa de Montañismo greatly facilitated access, solidifying Aneto's status as a premier mountaineering destination.