Geography of Nauru
|This article needs additional citations for verification. (February 2013) (Learn how and when to remove this template message)|
map of the island of Nauru
|Area||21 km2 (8.1 sq mi)|
|Highest elevation||61 m (200 ft)|
|Largest settlement||Yaren (pop. 1,100)|
|Pop. density||441.67 /km2 (1,143.92 /sq mi)|
|Ethnic groups||Nauruan people|
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 . Nauru is one of the three great phosphate rock islands in the Pacific Ocean — the others are Banaba (Ocean Island) in Kiribati and Makatea in French Polynesia.
Its land area is 21 km2 (8.1 sq mi), and it has a 30-kilometre coastline (19 mi). Maritime claims are a 200-nautical-mile (370 km) exclusive fishing zone, and a 12-nautical-mile (22 km) territorial sea.
A sandy beach rises to the fertile ring around raised coral reefs. The raised phosphate plateau ('Topside') takes up the central portion of the island. The highest point is 200 ft (61 m) above sea level, along the plateau rim.
Geology of Nauru
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 sealevel 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 sea water. 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.
Nauru is moving at 104 mm per year to the north west 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.
- Periodic droughts, limited natural fresh water 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.
This is a list of the extreme points of Nauru, the points that are farther north, south, east or west than any other location.
- Northernmost point – Cape Anna, Ewa District
- Easternmost point – Cape Ijuw, Ijuw District
- Southernmost point – unnamed headland south of the wireless station, Meneng District
- Westernmost point - the harbour, Aiwo District
- Highest point - Command Ridge (71 m, 233 ft)
- Lowest point - Pacific Ocean (sea level)
- CIA factbook. "Nauru Terrain - Geography". www.indexmundi.com. Retrieved 19 April 2016.
- Annual Report Part 1: Information on Fisheries, Research and Statistics: Republic of Nauru. Working Paper 17 of the 4th Scientific Committee of the Western and Central Pacific Fisheries Commission. WCPFC 2008.
- Republic of Nauru. 1999. Climate Change Response Under the United Nations Framework Convention on Climate Change URL Accessed 2006-05-03