Balearic Islands such as Es Conills, Es Vedrà, Sa Conillera, Dragonera, S'Espalmador, S'Espardell, Ses Bledes, Santa Eulària, Plana, Foradada, Tagomago, Na Redona, Colom, L'Aire, etc. The Balearic Front is a sea density regime north of the Balearic Islands on the shelf slope of the Balearic Islands, which is responsible for some of the surface-flow characteristics of the Balearic Sea. Located in the middle of the Mediterranean Sea, the Balearic Islands unsurprisingly have typical Mediterranean climates. The below-listed climatic data of the capital Palma are typical for the archipelago, with minor differences to other stations in Majorca, Ibiza, and Menorca. Little is recorded
Geology of the Iberian Peninsula This includes the Alboran Island halfway across the sea. During the Pliocene and Pleistocene volcanism continued. The Trans Alboran Shear Zone is a 35° (north east) trending fault zone extending from Alicante in Spain, along the coast of Murcia through the Betic range, across the Alboran Sea to the Tidiquin Mountains in Morocco. This zone shows itself with earthquakes. The south east side is moving north east, and the north west side is moving south west. The Balearic Islands are on a raised platform called the Balearic Promontory. Majorca: Minorca: The southern margin consists of a narrow shelf where carbonates