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
South African constitutional litigation but rather with the definition of the class of beneficiaries of the rights in the Bill of Rights. It therefore does not bar a foreign litigant who has a protectable interest in this country from seeking to protect that interest before a South African court. Indirect application means that the Constitution and the Bill of Rights do not directly bind actors. Instead, the influence of the Bill of Rights is mediated through other law: statutory or common law. In principle, and where possible, a legal dispute should be decided in terms of the existing principles or rules of ordinary law,