Formentera is made up of two Miocene table-like plateaus that rise up from the sea: La Mola in the southeast and the Cap de Barbaria - Pla del Rei in the southwest, joined by a thin strip of land that is 1.5 km. wide and 5 km. long, with an area of depression in the north where two lakes or "estanys" are located, S´Estany des Peix and S'Estany Pudent. The geological origin of the island is linked to that of all the Balearic islands and especially to Ibiza. Its geological history is short and simple as the only geological substratum's that have been located belong to the Miocene and Quaternary Eras. The Miocene materials are limited to the highest areas such as the cliffs of La Mola, the Cap de Barbaria, Punta Prima and Punta Pedrera. The rest of the island is formed by sediments and alluvial soil deposited during the Quaternary Era. Formentera is the smallest and most southerly island of the Balearic Islands group.