Karimunjawa - Indonesia

Karimunjawa - Indonesia | THE AMAZING ISLAND | Karimunjawa is an archipelago of 27 islands in the Java Sea, Indonesia, approximately 80 kilometres northwest of Jepara. The islands' name means 'a stone's throw from Java' in Javanese. They have a total land area of 78 km2. The main island is known as Karimun (2,700 ha), while the second largest island is Kemujan (1,400 ha). The islands' population is 6,632 (as of 1997) who inhabit seven of the islands.

Karimunjawa Island

Apart from the main island, Karimun, two of the larger islands are Kemujan and Parang. The island of Bawean lies east of this group, as part of Gresik District, East Java Province. The Karimunjawa islands are administered as an Indonesian sub district with five villages (Karimun, Kamagin, Kemujan, Digimon, and Parang) administratively part of Jepara district (kabupaten) of Central Java province.

Karimunjawa Island

History of Karimunjawa is Apart from use as a pirate base, the islands are believed to have been uninhabited until a penal settlement was established during the British occupation of Java in the early seventeenth century. The settlement was abandoned by the Dutch during the Java War of 1825–1830, but the former convicts remained as settlers. Cotton plantations set up during the convict period became a major source of income, as did goldsmithing.

Karimunjawa Island

The islands are influenced by the Northwest Monsoon during which winds from the west-northwest predominate and ocean currents are in an easterly direction. During the monsoon, rainfall averages 40 mm/day. During the Southeast Monsoon, dry winds from the east-southeast predominate and the ocean currents are in an westerly direction bringing water masses from the Flores Sea. Upwelled water masses during the Southeast Monsoon from the Flores and Banda Seas provides lower sea surface temperatures than in the Northeast Monsoon. The shallow slopes (5° to 15°) of the island shelves in the Java Sea (which rarely exceeds a depth of 55 m), provide environments for extensive reef development. The archipelago consists predominantly of pre-Tertiary continental islands primarily of quartzites and shales covered by basaltic lava. Geologically, the islands are part of Sundaland.