Elevation 1,332 m (4,370 ft) Width 6.5 km (4.0 mi) NE/SW Orogeny Variscan orogeny Peak Bañuela Period Paleozoic Types of rock Schist, Slate, Quartzite | Length 33 km (21 mi) NW/SE Parent range Sierra Morena Province Province of Ciudad Real Country Spain Age of rock Paleozoic | |
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Location Castile-La Mancha and Andalusia, Spain Similar Bañuela, Penibaetic System, Despeñaperros, La Garganta, Baetic Depression | ||
Ruta por sierra madrona el cuentakil metros
Sierra Madrona is a mountain range of the Sierra Morena, Spain. It is located in Ciudad Real Province, in the region of Castile-La Mancha as well as the Córdoba and Jaén provincial limits, Andalusia.
Contents
- Ruta por sierra madrona el cuentakil metros
- Map of Sierra Madrona 13130 Ciudad Real Spain
- El valle de alcudia y sierra madrona
- Description
- Geology
- References
Map of Sierra Madrona, 13130, Ciudad Real, Spain
Its highest peak, 1,332 m high Bañuela, is the highest point of the whole Sierra Morena system. Other notable summits are Dormideros 1,328 m, Corral de Borros 1,312 m, Abulagoso 1,301 m and Rebollera 1,161 m.
El valle de alcudia y sierra madrona
Description
Sierra Madrona is a massif composed of a series of subranges including Sierra de Quintana, Sierra de Hornilleros, Sierra de Navalmanzano, Sierra de la Garganta nad Sierra del Nacedero. They are aligned in a NW-SE direction and are separated by narrow valleys. The range is bounded by the Robledillo river valley and Sierra de la Solana and Umbria de Alcudia in the North, the Montoro river valley in the East, by the smooth hills of Sierra de Andújar, Sierra Quiteria and Los Pedroches in the South, and by the Yeguas River valley in the West.
The range is mostly covered in shrubland and is named after the madroño or madroña, the Strawberry Tree (Arbutus unedo) which is abundant in the area. The easiest route to reach it is to drive from Andújar or Puertollano.
The cave paintings of Peña Escrita and La Batanera are located in caves within the range area.
Geology
Geologically the range is made up of Paleozoic schist, slate and quartzite, as well as greywacke and sandstone. Structurally the range comprises a succession of wide anticlines and synclines in a Hercynian WNW-ESE direction.