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Coordinates: 27°7′S 109°22′W  /  27.117°S 109.367°W  / -27.117; -109.367

Easter Island (Rapa Nui: Rapa Nui , Spanish: Isla de Pascua ) is a Polynesian island in the southeastern Pacific Ocean, at the southeastern most point of the Polynesian triangle. A special territory of Chile annexed in 1888, Easter Island is widely famous for its 887 extant monumental statues, called moai (pronounced /ˈmoʊ.аɪ/ ), created by the early Rapanui people. It is a World Heritage Site (as determined by UNESCO) with much of the island protected within the Rapa Nui National Park. In recent times the island has been used as a cautionary tale for the cultural and environmental dangers brought upon by the overexploitation of resources, however this theory is now being contested by ethnographers and archaeologists alike who argue that the introduction of diseases carried by European colonizers and slave raiding, which devastated the population in the 1800s, had a much greater social impact than environmental decline and that introduced animals, first rats and then sheep, were greatly responsible for the island's loss of native flora which came closest to deforestation as recently as 1930-1960.

Name

The name "Easter Island" was given by the island's first recorded European visitor, the Dutch explorer Jacob Roggeveen, who encountered it on Easter Sunday 1722, while searching for Davis or David's island and named it Paasch-Eyland (18th century Dutch for "Easter Island"). The island's official Spanish name, Isla de Pascua, also means "Easter Island".

The current Polynesian name of the island, "Rapa Nui" or "Big Rapa", was coined following the slave raids carried out in Rapa Nui in the early 1860s because of Easter Island's geographic resemblance to the island of Rapa in the Bass Islands of the Austral Islands group. However, Thor Heyerdahl has claimed that the naming would have been the opposite, Rapa being the original name of Easter Island, and Rapa Iti was named by its refugees.

There are several hypotheses about the "original" Polynesian name for Easter Island, including Te pito o te henua , meaning "The Navel of the land" or "The ends of the land". Pito means both navel and umbilical cord which was considered to be the link between the world of the living (kainga) and the spiritworld Po, lying in the depths of the ocean further East. Since Easter Island is the easternmost Polynesian island it's possible the name refers to it being the "ends" of the world of the living, however after Alphonse Pinart translated it as "the Navel of the World" in his Voyage a l'Ile de Paques published in 1877, this second meaning has been lost. Some oral traditions claim that the island was first named Te pito o te kainga a Hau Maka , or the "Little piece of land of Hau Maka". Another name, Mata-ki-Te-rangi, means "Eyes looking to the sky."

Location and physical geography

Easter Island is one of the world's most isolated inhabited islands. Its closest inhabited neighbor is Pitcairn Island, with fewer than a hundred inhabitants 2075 kms to the West. It has a latitude close to that of Caldera, Chile; lies 3,510 km (2,180 mi) west of continental Chile at its nearest point (between Lota and Lebu). ( Isla Salas y Gómez , 415 kilometres to the east, is closer but uninhabited).

The island is approx 24.6 km (15.3 mi) long by 12.3 km (7.6 mi) at its widest point — its overall shape has been described as a triangle. It has an area of 163.6 km² (63 sq mi), and a maximum altitude of 507 metres. There are three Rano (freshwater crater lakes), at Rano Kau, Rano Raraku and Rano Aroi, near the summit of Terevaka, but no permanent streams or rivers.

Climate and weather

See also: Climate of Chile

The climate of Easter Island is subtropical maritime. The lowest temperatures are registered in July and August (18 °C (64 °F) and the highest in February (maximum temperature 28 °C (82 °F)), the summer season in the southern hemisphere. Winters are relatively mild. The rainiest month is April, though the island experiences year-round rainfall. As an isolated island Easter Island is constantly exposed to winds which help to keep the temperature fairly cool. Precipitation averages 1,118 mm (44.02 in) per year. Occasionally, heavy rainfall and rainstorms strike the island. These occur mostly in the winter months (June-August). Since it is close to the Pacific High and outside the range of the ITCZ, cyclones and hurricanes do not occur around Easter island.

Geology

The underlying island geology is one of extinct volcanoes. Easter Island is a volcanic high island, consisting mainly of three extinct coalesced volcanoes: Terevaka (altitude 507 metres) forms the bulk of the island. Two other volcanoes, Poike and Rano Kau, form the eastern and southern headlands and give the island its roughly triangular shape. There are numerous lesser cones and other volcanic features, including the crater Rano Raraku, the cinder cone Puna Pau and many volcanic caves including lava tubes. Poike used to be an island until volcanic material from Terevaka united it to Easter Island. The island is dominated by hawaiite and basalt flows which are rich in iron and show affinity with igneous rocks found in Galapagos Islands.

Easter Island and surrounding islets such as Motu Nui, Motu Iti are the summit of a large volcanic mountain rising over two thousand metres from the sea bed. It is part of the Sala y Gómez Ridge, a (mostly submarine) mountain range with dozens of seamounts starting with Pukao and then Moai, two seamounts to the west of Easter Island, and extending 2,700 km (1,700 mi) east to the Nazca Ridge.

Pukao, Moai and Easter Island were formed in the last 750,000 years, with the most recent eruption a little over a hundred thousand years ago. They are the youngest mountains of the Sala y Gómez Ridge, which has been formed by the Nazca Plate floating over the Easter hotspot. Alternative explanation is the activity of the Easter Fracture Zone. Only at Easter Island, its surrounding islets and Sala y Gómez does the Sala y Gómez Ridge form dry land.

In the first half of the 20th century, steam purportedly came out of the Rano Kau crater wall. This was photographed by the island's manager, Mr Edmunds.. According to geologists the last volcanic activity on the island occurred 10,000 years ago.

History

Main article: History of Easter Island

The history of Easter Island is rich and controversial. Its inhabitants have endured famines, epidemics, civil war, slave raids and colonialism, and near deforestation; their population has declined precipitously more than once. They have left a cultural legacy that has brought them fame disproportionate to their population.

300–400 CE has been put forward as a date for initial settlement of Easter Island, which would coincide approximately to the arrival of the first settlers on Hawaii. However, rectifications in radiocarbon dating have changed almost all of the early settlement dates in Polynesia and Rapa Nui is now considered to have been settled between 700 to 1,100 CE. According to oral tradition the first settlement was located in Anakena. There is an ongoing study by archaeologists Terry Hunt and Carl Lipo that suggests: “Radiocarbon dates for the earliest stratigraphic layers at Anakena, Easter Island, and analysis of previous radiocarbon dates imply that the island was colonized late, about 1200 CE. Significant ecological impacts and major cultural investments in monumental architecture and statuary thus began soon after initial settlement.” Jared Diamond points out in "Collapse" that Caleta Anakena is the landing point which provides the best shelter from prevailing swells, together with a sandy beach for canoe landings and launchings, so it seems likely to have been an early place of settlement. All of this however, contradicts archeological data where the radiocarbon dating of other sites precedes Anakena by many years, especially that of the Tahai, which precedes Anakena's dates by several hundred years.

The island was most probably populated by Polynesians who navigated in canoes or catamarans from the Marquesas Islands (3200 km away), or the Gambier Islands (Mangareva, 2600 km away). When Captain Cook visited the island, one of his crew members, who was a Polynesian from Bora Bora, was able to communicate with the Rapa Nui. The language most similar to Rapa Nui is Mangarevan with an 80% of similarity in words. In 1999, a voyage with reconstructed Polynesian boats was carried out, reach

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