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
History of South African nationality History of South African nationality South African nationality has been influenced primarily by the racial dynamics that have structured South African society throughout its development. The country's colonial history led to the immigration (or importation) of different racial and ethnic groups into one shared area. Power dispersion and inter-group relations led to European dominance of the state, allowing it to directly shape nationality although not without internal division or influence from the less empowered races. South African nationality begins with its history as a European colony. In 1652, the Dutch East India Company (abbreviated V.O.C., in reference to the original