Subbaetic System: Difference between revisions

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{{Short description|Mountain range in the Iberian Peninsula}}

{{Infobox mountain range

| name=Subbaetic System

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| elevation_m=2027

| elevation_note=

|coordinates =

| lat_d=|lat_m=|lat_s=|lat_NS=N

| long_d=|long_m=|long_s=|long_EW=W

| coordinates_ref =

| parent = [[Baetic System]]

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| map_caption = Location in Spain

| geology= [[Limestone]]|period=[[Cenozoic]]| orogeny=[[Alpine orogeny]]

|range_coordinates = {{coord|37|33|0|N|3|22|0|W|type:mountain|format=dms|display=inline,title}}

| range_lat_d=37|range_lat_m=33|range_lat_s=0|range_lat_NS=N

| range_long_d=3|range_long_m=22|range_long_s=0|range_long_EW=W

| range_coordinates_note =

}}

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[[File:SierradeHuetor.jpg|thumb|[[Sierra de Huétor]], [[Alfacar]], [[Granada Province]]]]

The '''Subbaetic''' or '''Sub-Baetic System''' ({{lang-langx|es|Sistema Subbético}} or ''Cordillera Subbética''<ref>[http://www.chsegura.es/chs/cuenca/infraestructuras/embalses/embalsedelTaibilla/marcoterritorial.html Embalse del Taibilla]</ref>) is one of the three systems of mountain ranges of the [[Baetic System]] in the southern [[Iberian Peninsula]]. Highest point {{convert|2027|m|abbr=on}} 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]].<ref>Edited by W Gibbons & T Moreno, ''Geology of Spain'', 2002, {{ISBN |978-1-86239-110-9}}</ref> 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.<ref>[http://www.sociedadgeologica.es/archivos_pdf/g12triptico_jaen.pdf Las montañas que surgieron del mar: la Sierra Sur de Jaén]</ref> The materials that compose this 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>

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*[[Sierra del Aljibe]], includes the Alcornocales Natural Park

* [[Sierra de Grazalema]]

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

*[[Subbaetic Ranges of Córdoba]]

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

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==External links==

*[httphttps://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]

*[http://www.granadanatural.com/blog.php?mes=9&anio=2009 Granada Natural - Las Zonas Externas]

*[http://www.sociedadgeologica.es/archivos/geogacetas/Geo33/Art16.pdf Relleno sedimentario y destrucción de una pequeña cuenca fluvio-lacustre en la Sierra Sur de Jaén (Cordilleras Béticas)]