Tuvalu is an island country in the Polynesian subregion of Oceania in the Pacific Ocean. Its islands are situated about midway between Hawaii and Australia. They lie east-northeast of the Santa Cruz Islands, northeast of Vanuatu, southeast of Nauru, south of Kiribati, west of Tokelau, northwest of Samoa and Wallis and Futuna, and north of Fiji. Tuvalu is composed of three reef islands and six atolls. They are spread out between the latitude of 5° and 10° south and between the longitude of 176° and 180°. They lie west of the International Date Line. Tuvalu has a population of 10,507. The total land area of the islands of Tuvalu is 26 square kilometres (10 sq mi).
The Western Pacific nation of Tuvalu, formerly known as the Ellice Islands, is situated 4,000 kilometers (2,500 mi) northeast of Australia and is approximately halfway between Hawaii and Australia. It lies east-northeast of the Santa Cruz Islands, southeast of Nauru, south of Kiribati, west of Tokelau, northwest of Samoa and Wallis and Futuna and north of Fiji. It is a very small island country of 26 km2 (10 sq mi). Due to the spread out islands it has the 38th largest Exclusive Economic Zone of 749,790 km2 (289,500 sq mi).
The first inhabitants of Tuvalu were Polynesians, so the origins of the people of Tuvalu can be traced to the spread of humans out of Southeast Asia, from Taiwan, via Melanesia and across the Pacific islands of Polynesia.
Nanumea is the northwesternmost atoll in the Polynesian nation of Tuvalu, a group of nine coral atolls and islands spread over about 400 miles (640 km) of Pacific Ocean just south of the equator and west of the International Date Line. Nanumea is 4 km2 (1.5 sq mi) with a population of 512 people.
Nui is an atoll and one of nine districts of the Pacific Ocean state of Tuvalu. It has a land area of 3.37 km² and a population of 610.
Nukulaelae is an atoll that is part of the nation of Tuvalu, and it has a population of 300. The largest settlement is Pepesala on Fangaua islet with a population of 300 people. It has the form of an oval and consists of at least 15 islets. The inhabited islet is Fangaua, which is 1.5 kilometres (0.93 mi) long and 50 to 200 metres wide. The easternmost point of Tuvalu is Niuoko islet. The Nukulaelae Conservation Area covers the eastern end of the lagoon. A baseline survey of marine life in the conservation zone was conducted in 2010.
Nukufetau is an atoll that is part of the nation of Tuvalu. The atoll was claimed by the US under the Guano Islands Act some time in the 19th century and was ceded in a treaty of friendship concluded in 1979 and coming into force in 1983. It has a population of 597 who live on Savave islet. In 1951 the school that was located on Motumua islet was transferred to Savave and became the government primary school for Nukufetau. It was named the Tutasi Memorial School in honour of its predecessor.
Motupuakaka is an islet of Nui atoll in the Pacific Ocean state of Tuvalu.
Pakantou is an islet of Nui atoll in the Pacific Ocean state of Tuvalu.
Piliaieve is an islet in the Pacific Ocean located in the state of Nui, Tuvalu.
Pongalei is an islet of Nui atoll in the Pacific Ocean state of Tuvalu.
Talalolae is an islet located in Nui atoll in the Pacific Ocean state of Tuvalu.
Tokinivae is an islet of Nui atoll, in the Pacific Ocean state of Tuvalu.< Nui tradition is that Kolaka, a warrior from Nukufetau came on several raiding expeditions to Tokinivae, until he was killed and buried at Tararorae.
Unimai is an islet of Nui atoll in the Pacific Ocean state of Tuvalu.
Funafuti is an atoll and the capital of the island nation of Tuvalu. It has a population of 6,320 people, making it the country's most populous atoll, with 60.15 per cent of Tuvalu's population. It consists of a narrow sweep of land between 20 and 400 metres wide, encircling a large lagoon 18 km long and 14 km wide. The average depth of the Funafuti lagoon is about 20 fathoms. With a surface area of 275 square kilometres (106.2 sq mi), it is by far the largest lagoon in Tuvalu. The land area of the 33 islets around the atoll of Funafuti totals 2.4 square kilometres (0.9 sq mi); taken together, they constitute less than one per cent of the total area of the atoll. Cargo ships can enter Funafuti's lagoon and dock at the port facilities on Fongafale.
Tanrake is a village in Tuvalu. It is on Nui atoll, on Fenua Tapu islet. The location is 7.25°S 177.15°E.
Telikiai is an islet of Nui atoll in the Pacific Ocean state of Tuvalu. Meang means "west". The islet features in the legends of the Tekaunibiti family, whose members went to catch birds on the islet and found three teanti-ma-aomata and captured two.
This timeline of the history of Tuvalu chronologically lists important events occurring within the present political boundaries of the Pacific island state of Tuvalu. This time line is introduced by the theories as to the origins of the Polynesian people and the migration across the Pacific Ocean to create Polynesia, which includes the islands of Tuvalu.
Tuvaluan mythology tells stories of the creation of the islands of Tuvalu and of the founding ancestors of each island. While on some of the islands there are stories of spirits creating the islands, a creation story that is found on many of the islands is that te Pusi mo te Ali created the islands of Tuvalu; te Ali is believed to be the origin of the flat atolls of Tuvalu and te Pusi is the model for the coconut palms that are important in the lives of Tuvaluans. The strength of this belief has the consequence that Moray eel are tapu and are not eaten.
The coral reefs of Tuvalu consist of three reef islands and six atolls, containing approximately 710 km2 (270 sq mi) of reef platforms. The islands of the Tuvalu archipelago are spread out between the latitude of 5° to 10° south and longitude of 176° to 180°, west of the International Date Line. The islands of Tuvalu are volcanic in origin. On the atolls, an annular reef rim surrounds the lagoon, and may include natural reef channels. The reef islands have a different structure to the atolls, and are described as reef platforms as they are smaller tabular reef platforms that do not have a salt-water lagoon, although they may have a completely closed rim of dry land, with the remnants of a lagoon that has no direct connection to the open sea or that may be drying up.
Dutch map of the island, made in June 1825
View of the main island
View of the atoll
