Gibraltar Arc Gibraltar Arc The Gibraltar Arc is a geological region corresponding to an arcuate orogen surrounding the Alboran Sea, between the Iberian Peninsula and Africa. It consists of the Betic Cordillera (south Spain), and the Rif (North Morocco). The Gibraltar Arc is located at the western end of the Mediterranean Alpine belt and formed during the Neogene due to convergence of the Eurasian and African plates. Maximum altitudes of the region are reached at the Mulhacén peak (3482 m) at the Cordillera Betica. Precipitation is collected mainly by the Guadalquivir (Betics) and Sebou (Rif) rivers, which have delivered most sedimentary infill
Lines of Contravallation of Gibraltar to the territory by land. The lines covered a distance of 950 toises () and were built 1,000 toises () from the Rock of Gibraltar, where the British defences began. This sparked a diplomatic dispute between Britain and Spain. During the negotiations that led to the Treaty of Utrecht of 1713, under which Spain ceded Gibraltar to Britain, the British government sought to compel the Spanish to cede "a convenient quantity of land round Gibraltar, viz., to the distance of two cannon shot ... which is absolutely necessary for preventing all occasions of dispute between the Garrison and the Country