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
Ottoman invasion of the Balearic Islands (1558) Ottoman invasion of the Balearic Islands (1558) An Ottoman raid of the Balearic islands was accomplished by the Ottoman Empire in 1558, against the Spanish Habsburg territory of the Balearic islands. The Ottomans had already attacked the Balearic Islands many times previously, as in the 1501 Ottoman raid on the Balearic islands. Then followed the sacks of Pollença (in 1531 and 1550), the Sack of Mahon in 1535, Alcúdia (1551), Valldemossa (1552), Andratx (1553), and Sóller (1561). Ottoman attacks only decreased after the Battle of Lepanto in 1571, although they continued until the 17th century. On 30 December 1557, Henry