Anibare Bay is a large bay located in the Anibare District of eastern Nauru island.
It is bordered by capes to the north and south, in Ijuw and Meneng districts respectively.
Its Anibare Beach is in excess of two kilometers long. Anibare Bay was formed by the underwater collapse of the east side of the volcano that underlies Nauru. A large arc shaped block slid away from the side of Nauru and rotated out. This block extends to about 1100 m below sea level, with rough bulging landslide deposits down to 2000 m below sea level. [1]
While Anibare Bay is popular with tourists and naturalists, it can be at times dangerous owing to frequent heavy surf and the presence of rip currents.
The Anibare Bay escarpment is a line of wooded cliffs overlooking the bay. It ranges in gradient from vertical cliffs to gradually sloping areas, and contains the richest remaining native vegetation on the island. It forms a 35 ha site which has been recognised as an Important Bird Area (IBA) by BirdLife International because it is reported to hold the highest density of endemic Nauru reed warblers on the island, as well as supporting tree-nesting seabirds such as black noddies. Ity is likely to be a nesting site for Micronesian imperial pigeons, if any still remain. [2]
Noted industries include the government-owned Menen Hotel, and Anibare Harbour, an artificial commercial fishing area which was created in 2000. Anibare Beach resort tourism Development was proposed and approved on 24 Aug 2021.The project is meant to boost hospitality and tourism and income growth for Nauru.The planning is managed and supervised by GIP and led by CEO Troy Spenser.
Nauru is a tiny phosphate rock island nation located in the South Pacific Ocean south of the Marshall Islands in Oceania. It is only 53 kilometres (33 mi) south of the Equator at coordinates 0°32′S166°55′E. Nauru is one of the three great phosphate rock islands in the Pacific Ocean—the others are Banaba in Kiribati and Makatea in French Polynesia.
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Nauru is positioned in the Nauru Basin of the Pacific Ocean, on a part of the Pacific Plate that formed at a mid oceanic ridge at 132 Ma. From mid Eocene (35 Ma) to Oligocene times a submarine volcano built up over a hotspot, and formed a seamount composed of basalt. The seamount rises over 4300 m above the ocean floor. This hotspot developed simultaneously with a major Pacific Plate reorganisation.
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Coordinates: 0°32′01″S166°57′20″E / 0.53361°S 166.95556°E