Biak Numfor RegencyBiak Numfor Regency is one of the regencies (kabupaten) in Papua Province of Western New Guinea in northeastern Indonesia. GeographyThe regency consists two of the three largest members of the Biak Islandsarchipelago at the northern entrance into Cenderawasih Bay.
Papua (province)Papua, formerly known as West Irian and Irian Jaya, is a province of Indonesia, comprising the northern coast of Western New Guinea together with island groups in Cenderawasih Bay to the west. It roughly follows the borders of the Papuan customary region of Mamta – Saireri and is divided into eight regencies (kabupaten) and one city (kota), the latter being the provincial capital of Jayapura.
Cenderawasih BayCenderawasih Bay (Indonesian: Teluk Cenderawasih, "Bird of Paradise Bay"), also known as Sarera Bay (Indonesian: Teluk Sarera) and formerly Geelvink Bay (Dutch: Geelvinkbaai), is a large bay in northern Province of Papua, Central Papua and West Papua, New Guinea, Indonesia.
JayapuraJayapura (formerly Hollandia (1910–1962), Kota Baru (1962–1963), Soekarnopura (1963–1968)) is the capital and largest city of the Indonesian province of Papua on the island of New Guinea. It is situated on the northern coast of the island and covers an area of 835.48 km2 (322.58 sq mi). The city borders the Pacific Ocean and Yos Sudarso Bay to the north, the country of Papua New Guinea to the east, Keerom Regency to the south, and Jayapura Regency to the west.
Biak ArchipelagoThe Biak Islands (Indonesian: Kepulauan Biak, also Schouten Islands or Geelvink Islands) are an island group of Papua province, eastern Indonesia in the Cenderawasih Bay (or Geelvink Bay) 50 km off the north-western coast of the island of New Guinea. The group consists of the main islands of Biak, Supiori and Numfor, and numerous smaller islands, mostly covered in rain forest. The population of the archipelago is about 130,000.
IndonesiaIndonesia, officially the Republic of Indonesia, is a country in Southeast Asia and Oceania, between the Indian and Pacific oceans. Comprising between 13,000 and 17,000 islands, including Sumatra, Java, Sulawesi, and parts of Borneo and New Guinea, it is the world's largest archipelagic state and the 14th-largest country by area. Indonesia has extensive tropical forests and marine ecosystems that support one of the world's highest levels of biodiversity.
New GuineaNew Guinea (Tok Pisin: Niugini; Hiri Motu: Niu Gini; Indonesian: Papua, fossilized Nugini, also known as Papua or historically Irian) is the world's second-largest island, with an area of 785,753 km2 (303,381 sq mi). It has the third-largest remaining rainforest globally, and the highest plant biodiversity of any island.
IslandAn island or isle ( ) is a piece of land, distinct from a continent, completely surrounded by water. There are continental islands, which were formed by being split from a continent by plate tectonics, and oceanic islands, which have never been part of a continent. Oceanic islands can be formed from volcanic activity, grow into atolls from coral reefs, and form from sediment along shorelines, creating barrier islands.
AtollAn atoll () is a ring-shaped island, including a coral rim that encircles a lagoon. There may be coral islands or cays on the rim. Atolls are located in warm tropical or subtropical parts of the oceans and seas where corals can develop. Most of the approximately 440 atolls in the world are in the Pacific Ocean. Two different, well-cited models, the subsidence model and the antecedent karst model, have been used to explain the development of atolls.
CoralCorals are colonial marine invertebrates within the subphylum Anthozoa of the phylum Cnidaria. They typically form compact colonies of many identical individual polyps. Coral species include the important reef builders that inhabit tropical oceans and secrete calcium carbonate to form a hard skeleton. A coral "group" is a colony of very many genetically identical polyps.
ReefA reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic (non-living) processes such as deposition of sand or wave erosion planing down rock outcrops. However, reefs such as the coral reefs of tropical waters are formed by biotic (living) processes, dominated by corals and coralline algae.*As an Amazon Associate I earn from qualifying purchases.