Subbaetic System: Difference between revisions

Revision as of 08:25, 28 September 2011

Revision as of 03:14, 6 January 2012

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The [[Prebaetic System]] is a subsystem of the Cordillera Subbética. The materials that compose the eastern sector were formed in a relatively shallow sea.<ref>[http://aguas.igme.es/igme/publica/libro103/pdf/lib103/capiII_04.pdf Morfología kárstica del sector oriental del Prebético andaluz]</ref>

==Main mountain ranges==

Some of the mountain ranges that make up the ''Subbético'' system are, from west to east:

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*[[Sierra Sur de Sevilla]], highest points Terril (1,132 m) and Peñón de Algámitas (1,128 m)

*[[Subbaetic Ranges of Córdoba]]

**[[Sierra de Rute]], highest point 1,326 m

**[[Sierra de la Horconera]], highest point Pico Tiñosa (1,570 m), highest point in [[Córdoba Province (Spain)|Córdoba Province]], and Pico Bermejo (1,476 m)

**[[Sierra de los Pollos]], close to [[Carcabuey]] and [[Priego de Córdoba]]

**[[Sierra de Gaena]]

**[[Sierra de Jarcas]]

**[[Sierra de los Lanchares]], includes interstinginteresting fromationsformations, like the Lapiaz de los Lanchares

**[[Sierra del Lobatejo]], highest point 1,217 m

**[[Sierra Alcaide]]

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==References==

{{reflist}}

==External links==

*[http://openlibrary.org/books/OL4030404M/Morfologi%CC%81a_karstica_del_sector_central_de_la_Cordillera_Subbe%CC%81tica Morfología karstica del sector central de la Cordillera Subbética]