
handle: 10045/637
A occidente del gran afloramiento triásico que divide la llanada cuaternaria de Villenase encontraba una amplia cuenca artesiana, ocupada por extensos sectores lacustres, que seprolongaba por los términos de Caudete y Sax. Hacia el interior de esta cuenca cerrada viertenlos caudales subterráneos de una serie de estructuras mesozoicas con áreas de alimentaciónconsiderables. Los mantos acuíferos, retenidos por el Keuper, y las formaciones arcillosabulosasdel Cuaternario, revisten excepcional importancia.
Propiedad de la tierra, Geography (General), Desamortización, G1-922, Laguna de Villena
Propiedad de la tierra, Geography (General), Desamortización, G1-922, Laguna de Villena
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