Espigüete facts for kids
Quick facts for kids Espigüete |
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| Highest point | |
| Elevation | 2,450 m (8,040 ft) |
| Prominence | 474 m (1,555 ft) |
| Geography | |
Location in the Province of Palencia.
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| Location |  Castile and León Province of León |
| Country |  Spain |
| Geology | |
| Mountain type | Limestone |
| Climbing | |
| First ascent | 1854 |
| Normal route | South, from Cardaño de Abajo |
The Espigüete Peak (Spanish: Pico Espigüete) (2450 m) is one of the highest elevations of the Montaña Palentina (Spain), in the foothills of the Cantabrian mountain range (Fuentes Carrionas massif) and, despite not being the highest, it is its most characteristic peak. It is located in the municipality of Velilla del Río Carrión.
Location
It is located next to the town of Cardaño de Abajo, in the municipality of Velilla del Río Carrión, within the Montaña Palentina Natural Park, 26 km from Guardo and 126 km from Palencia. Its western foothills belong to the town of Valverde de la Sierra (León).
Characteristics
Main information
It is a pyramidal limestone mass, visible from a distance due to its isolation from any other peak. The south face has smooth reliefs while the north face has vertical walls. Due to its composition, it suffers variations in its appearance depending on the season and lighting, being covered with snow most of the winter.
On 27 June 2000, the declaration of the Fuentes Carrionas y Fuente Cobre-Montaña Palentina Natural Park was published in the Boletín Oficial del Estado —revised on 28 May 2010— to which Espigüete belongs. It is one of the highest peaks of the natural park (2450 m), characterized by peaks such as Curavacas (2528) and by the valley bottoms, with a difference in altitude that can reach over 1000 meters.
Geomorphology
Its limits are established by morpho-structural features: to the north, the thrust fault that directs the waters of the Arroyo Mazobres; to the east, the synclinorium complex that sinks its roots in the Arroyo de las Lomas; to the west, it is drawn against the metamorphic slopes of Caladillos and Carrascal; and to the south, its margin is formed by the prolonged slate and sandstone spines of the Cervera Formation. Despite its appearance, the Espigüete has numerous hollows in its interior, where there are huge canyons with subway rivers and lakes, deep pits and caves that make it a real treasure for speleologists.
Climatology
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31
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45
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105
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85
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Imperial conversion
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Flora
It is a transition area in which taxa typical of central and northern Europe are mixed with others characteristic of the Mediterranean world. The climatic conditions make it lack vegetation, developing only some lichen and small plants characteristic of the high mountains. Among the latter it is necessary to highlight a variety of sempervivum that only occurs in this peak, discovered in 1935 by the eminent botanist Paul Leon Giuseppi, and named in his honor Sempervivum Giuseppii.
History
The geologist and naturalist Casiano de Prado is recorded as the first to climb it, in 1854, and so did Aymar de Saint-Saud in 1892, on one of his visits to Picos de Europa.
See also
In Spanish: Espigüete para niños
