몬테호 데 라 시에라 최고의 러닝 경로

A beautiful Black Village in La Sierra Poble in Madrid. Clean, well-kept, with good hospitality services, it is the beginning and end of multiple routes, but it also has a very extensive exhibition of outdoor statues of all types nearby.

Puebla de la Sierra is one of the black towns of Madrid, in the border area with Guadalajara. Black towns are so called because of their slate-built houses. This town is especially picturesque and its location on the mountainside, in a privileged setting, makes it an unforgettable visit.

a beautiful and well-kept town in the Sierra Norte

Meira's giant chair is a metal sculpture by an anonymous author from the Galician town of Meira, in Pontevedra, and is part of the outdoor art gallery of Puebla de la sierra.

The path with the yellow markings surrounds the summit of Peña Hierro to the left of the cliffs and reaches the geodesic vertex of Porrejón (1,823 m), one of the main peaks of the Sierra del Rincón. In another secondary summit there is a large stone milestone and good views of the western sector of the Central System. Attention when leaving the summit, especially in fog. The trail goes down from the summit in a southwesterly direction to go around the head of a valley and then there are milestones and clear traces of the path that goes down to the port of Puebla.

La Puebla, a port with two slopes, has a rough start but before the second kilometer it softens.

The waterfall is also known by the names of Chorro de Somosierra or Cascada de los Litueros. It is a wonderful waterfall several meters high that offers amazing postcards. The path is technical in some sections, go carefully and step firmly to enjoy the surroundings.

The summit of Pico Porrejón is a curious exhibition of the geological components that give uniqueness to the reliefs of the Sierra del Rincón Biosphere Reserve, a compact block of metamorphic rocks of gneiss and micacite with a strong projection of quartzite and slate subjected to the Consequences of gelivation, which is a form of periglacial erosion on the rocky scree, the water enters the cracks and, due to the effect of ice-thaw, creates the striking blades, ridges and stone passageways that abound in the Ayllón massifs.