The Subbaetic or Sub-Baetic System (Spanish: Sistema Subbético or Cordillera Subbética[1]) is one of the three systems of mountain ranges of the Baetic System in the southern Iberian Peninsula. Highest point 2,027 m (6,650 ft) high Peña de la Cruz in Sierra Arana. Its northern limit includes the valley of the Guadalquivir in its western part.

Subbaetic System
Sistema Subbético
Peña de la Cruz, the highest peak in the Sierra Arana
Highest point
PeakPeña de la Cruz
Elevation2,027 m (6,650 ft)
Dimensions
Length510 km (320 mi) ENE/WSW
Width60 km (37 mi) NNW/SSE
Geography
Subbaetic System is located in Spain
Subbaetic System
Subbaetic System
Location in Spain
LocationAndalusia / Murcia
CountrySpain
Range coordinates37°33′0″N 3°22′0″W / 37.55000°N 3.36667°W / 37.55000; -3.36667
Parent rangeBaetic System
Geology
OrogenyAlpine orogeny
Rock ageCenozoic
Rock typeLimestone
Schematic representation of the Baetic System of mountain ranges
Sierra de Huétor, Alfacar, Granada Province

Description

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The Subbaetic System runs to the north of the Cordillera Penibética from Cape Trafalgar in Cádiz Province across Andalusia reaching into the Region of Murcia.[2] The highest peaks reach heights between 1,500m and well over 2,000 m.

Towards the east of the Sierra Sur de Jaén, east of Martos, another subsystem begins, the Prebaetic System, an offshoot of the Subbaetic System stretching further northeastwards.[3] The materials that compose this eastern sector were formed in a relatively shallow sea.[4]

Main mountain ranges

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Some of the mountain ranges that make up the Subbaetic System are, from west to east:

See also

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References

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  1. ^ Embalse del Taibilla
  2. ^ Edited by W Gibbons & T Moreno, Geology of Spain, 2002, ISBN 978-1-86239-110-9
  3. ^ Las montañas que surgieron del mar: la Sierra Sur de Jaén
  4. ^ Morfología kárstica del sector oriental del Prebético andaluz
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