[{"@context":"http:\/\/schema.org\/","@type":"BlogPosting","@id":"https:\/\/wiki.edu.vn\/en\/wiki41\/geography-of-nauru-wikipedia\/#BlogPosting","mainEntityOfPage":"https:\/\/wiki.edu.vn\/en\/wiki41\/geography-of-nauru-wikipedia\/","headline":"Geography of Nauru – Wikipedia","name":"Geography of Nauru – Wikipedia","description":"before-content-x4 From Wikipedia, the free encyclopedia Enlargeable, detailed map of Nauru after-content-x4 Nauru is a tiny phosphate rock island nation","datePublished":"2017-11-28","dateModified":"2017-11-28","author":{"@type":"Person","@id":"https:\/\/wiki.edu.vn\/en\/wiki41\/author\/lordneo\/#Person","name":"lordneo","url":"https:\/\/wiki.edu.vn\/en\/wiki41\/author\/lordneo\/","image":{"@type":"ImageObject","@id":"https:\/\/secure.gravatar.com\/avatar\/c9645c498c9701c88b89b8537773dd7c?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/c9645c498c9701c88b89b8537773dd7c?s=96&d=mm&r=g","height":96,"width":96}},"publisher":{"@type":"Organization","name":"Enzyklop\u00e4die","logo":{"@type":"ImageObject","@id":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","url":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","width":600,"height":60}},"image":{"@type":"ImageObject","@id":"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/thumb\/c\/c0\/Nauru2021OSM.png\/220px-Nauru2021OSM.png","url":"https:\/\/upload.wikimedia.org\/wikipedia\/commons\/thumb\/c\/c0\/Nauru2021OSM.png\/220px-Nauru2021OSM.png","height":"210","width":"220"},"url":"https:\/\/wiki.edu.vn\/en\/wiki41\/geography-of-nauru-wikipedia\/","about":["Wiki"],"wordCount":2512,"articleBody":"     (adsbygoogle = window.adsbygoogle || []).push({});before-content-x4From Wikipedia, the free encyclopedia  Enlargeable, detailed map of Nauru       (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4Nauru 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\u00a0mi) south of the Equator at coordinates 0\u00b032\u2032S 166\u00b055\u2032E\ufeff \/ \ufeff0.533\u00b0S 166.917\u00b0E\ufeff \/ -0.533; 166.917. Nauru is one of the three great phosphate rock islands in the Pacific Ocean\u2014the others are Banaba (Ocean Island) in Kiribati and Makatea in French Polynesia.       (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4Its land area is 21\u00a0km2 (8.1\u00a0sq\u00a0mi), and it has a 30-kilometre coastline (19\u00a0mi). Maritime claims are an Exclusive Economic Zone of 308,480\u00a0km2 (119,100\u00a0sq\u00a0mi) with 200-nautical-miles (370\u00a0km), and a 12-nautical-mile (22\u00a0km) territorial sea.The climate is tropical with a monsoon rainy season from November to February.A sandy beach rises to the fertile ring around raised coral reefs.[1] The raised phosphate plateau (‘Topside’) takes up the central portion of the island. The highest point is 213\u00a0ft (65 m) above sea level, along the plateau rim.Nauru’s only economically significant natural resources are phosphates, formed from guano deposits by seabirds, and fisheries,[2] particularly for tuna.       (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4Due to being surrounded by corals and sandy beaches, the island houses no natural harbours, nor any rivers or substantial lakes.Nauru has a unique navigational system, which is only capable of being used on the island.Table of ContentsGeology of Nauru[edit]Environmental issues[edit]Climate[edit]Extreme points[edit]References[edit]See also[edit]Geology of Nauru[edit]  An aerial image of Nauru in 2002 from the U.S. Department of Energy’s Atmospheric Radiation Measurement Program. Regenerated vegetation covers 63% of land that was mined.[3]Nauru is a raised coral atoll 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 (35mya) to Oligocene times, a submarine volcano built up over a hotspot and formed a seamount    composed of basalt. The seamount is over 4300 metres high. This hotspot was simultaneous with a major Pacific Plate reorganisation. The volcano was eroded to sea level and a coral atoll grew on top to a thickness of about 500 metres. Coral near the surface has been dated from 5 Mya to 0.3 Mya. The original limestone has been dolomitised by magnesium from seawater. The coral was raised above sea level about 30 metres and is now a dolomite limestone outcrop which was eroded in classic karst style into pinnacles up to 20 metres high. To at least a depth of 55 metres below sea level, the limestone has been dissolved forming cavities, sinkholes, and caves. Holes on the topside of the island were filled up by a phosphate layer up to several metres thick.Anibare Bay was formed by the underwater collapse of the east side of the volcano.Buada Lagoon was formed by solution of the limestone when the sea level was lower, followed by collapse.Nauru is moving at 104\u00a0mm (4.1\u00a0in) per year to the northwest along with the Pacific Plate.Freshwater can be found in Buada lagoon, and also in some brackish ponds at the escarpment base in Ijuw and Anabar in the northeast. There is an underground lake in Moqua Cave in the southeast of the island. Since there are no streams or rivers on Nauru, water must be gathered from roof catchment systems. Water is also brought to Nauru as ballast on ships returning for loads of phosphate.[4]Environmental issues[edit]Periodic droughts, limited natural freshwater resources (roof storage tanks collect rainwater, but mostly dependent on a single, aging desalination plant)Extreme soil conditions are caused by high alkalinity, high phosphate levels, and low potassium. Iron, manganese, copper, molybdenum, and zinc are rendered unavailable to plants. Combined with thin or damaged soils this causes low fertility.Intensive phosphate mining during the past 90 years has left the central 80% of Nauru a wasteland and threatens limited remaining land resources.Nauru is a party to the international environmental agreements on biodiversity, climate change, desertification, the law of the sea and marine dumping.Climate[edit]  Temperature change in Nauru since 1909 in the context of global warmingNauru’s climate is hot and very humid year-round because of its proximity to the equator and the ocean. Nauru is hit by monsoon rains between November and February, but rarely has cyclones. Annual rainfall is highly variable and is influenced by the El Ni\u00f1o\u2013Southern Oscillation, with several significant recorded droughts.[5][6] The temperature on Nauru ranges between 30 and 35\u00a0\u00b0C (86 and 95\u00a0\u00b0F) during the day and is quite stable at around 25\u00a0\u00b0C (77\u00a0\u00b0F) at night.[7]Climate data for Yaren District, NauruMonthJanFebMarAprMayJunJulAugSepOctNovDecYearRecord high \u00b0C (\u00b0F)34(93)37(99)35(95)35(95)32(90)32(90)35(95)33(91)35(95)34(93)36(97)35(95)37(99)Average high \u00b0C (\u00b0F)30(86)30(86)30(86)30(86)30(86)30(86)30(86)30(86)30(86)31(88)31(88)31(88)30(87)Average low \u00b0C (\u00b0F)25(77)25(77)25(77)25(77)25(77)25(77)25(77)25(77)25(77)25(77)25(77)25(77)25(77)Record low \u00b0C (\u00b0F)21(70)21(70)21(70)21(70)20(68)21(70)20(68)21(70)20(68)21(70)21(70)21(70)20(68)Average precipitation mm (inches)280(11.0)250(9.8)190(7.5)190(7.5)120(4.7)110(4.3)150(5.9)130(5.1)120(4.7)100(3.9)120(4.7)280(11.0)2,080(81.9)Average precipitation days1614131199121411101315152Source: WeatherbaseExtreme points[edit]This is a list of the extreme points of Nauru, the points that are farther north, south, east or west or higher than any other location.References[edit]See also[edit]     (adsbygoogle = window.adsbygoogle || []).push({});after-content-x4"},{"@context":"http:\/\/schema.org\/","@type":"BreadcrumbList","itemListElement":[{"@type":"ListItem","position":1,"item":{"@id":"https:\/\/wiki.edu.vn\/en\/wiki41\/#breadcrumbitem","name":"Enzyklop\u00e4die"}},{"@type":"ListItem","position":2,"item":{"@id":"https:\/\/wiki.edu.vn\/en\/wiki41\/geography-of-nauru-wikipedia\/#breadcrumbitem","name":"Geography of Nauru – Wikipedia"}}]}]