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Subbaetic System
The Subbaetic or Sub-Baetic System ((スペイン語:Sistema Subbético) or ''Cordillera Subbética''〔(Embalse del Taibilla )〕) is one of the three systems of mountain ranges of the Baetic System in the southern Iberian Peninsula.Highest point high Peña de la Cruz in Sierra Arana. Its northern limit includes the valley of the Guadalquivir in its western part.
==Description==
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.〔Edited by W Gibbons & T Moreno, ''Geology of Spain'', 2002, ISBN 978-1-86239-110-9〕 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.〔(Las montañas que surgieron del mar: la Sierra Sur de Jaén )〕 The materials that compose this eastern sector were formed in a relatively shallow sea.〔(Morfología kárstica del sector oriental del Prebético andaluz )〕
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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