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GEOLOGÍA

Para la determinación de la Geología presente en Alborea, se ha utilizado el Mapa Geológico de España numero 744 de Casas Ibáñez y el 719 de Venta del Moro, a escala 1:50.000.

La zona se sitúa en la provincia de Albacete. Geológicamente la Hoja de Casas Ibáñez, a la cual pertenece el termino municipal de Alborea, constituye una planicie casi Horizontal, que sirve de precaria divisoria de aguas entre las cuencas del Cabriel v el Júcar. En dicha planicie, formada por depósitos neógenos, se observan suaves relieves constituidos por materiales triásicos y cretácicos dispuestos en alineaciones E-O.

Los sedimentos más antiguos que aparecen en este ámbito corresponden al Triásico Medio (Muschelkalk), siendo los mas modernos, aparte de los diferentes cuaternarios, los depósitos calco-detríticos pliocenos que se extienden por gran parte de la zona.

La Hoja de Casas Ibáñez esta atravesada por una fosa tectónica de dirección E-O, por donde discurre el río Júcar, v que individualiza dos muelas dentro de la mitad meridional de la Hoja 744 del IGME. Los materiales que afloran están afectados por una tectónica de edad Alpídica y presentan estructuras fuertemente ligadas con las del zócalo Hercínico.|

Como puntos mas altos del termino municipal destacan los tres Vértices Geodésicos de "El Cerro Gordo" (739 m), "Los Guijarrales" (735m) y "Pinar Borregas" (743m)

"Cerro Gordo"                                "Los Guijarrales"                                  "Pinar Borregas"

Por el contrario los puntos con menor altitud los encontramos al norte del termino municipal ya en el limite con e río Cabriel en el paraje de "La Ginesita" con alturas entre los 463 y 400 metros.

     LEYENDA:      

Rango de altitud en m

Mapa de rangos de altitud

Mapa de relieves

El desnivel del termino municipal esta en torno al 2 o al 3% a excepción de la zona norte, donde debido al valle del Cabriel el desnivel medio varía entre el 3 y el 12%

     LEYENDA:     

Desnivel en %

Mapa de desniveles

 


 


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