MESOZOIC SUCCESSIONS OF THE BETIC AND IBERIAN RANGES C H A P T E R 6 Castro, J.M. García, A. Gómez, J.J. Goy, A. Molina, J.M. Ruiz Ortiz, P.A. Sopeña, A. Above, slumped beds in the marly limestones and marls of the Carretero Formation (lower Cretaceous of the Sub- Betic) along the Jaén-Granada highway, km 70.4. The detachment surface is slightly oblique to the underlying bedding, which is parallel to the beds overlying the synsedimentary fold. Below, conglomerates and sandstones of the Triassic Buntsandstein facies at Barranco de la Hoz of the Gallo river (province of Guadalajara, Castillian Branch of the Iberian Range). Photo: L. Carcavilla