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Rongorongo (/ ˈ r ɒ ŋ ɡ oʊ ˈ r ɒ ŋ ɡ oʊ / [1] or / ˈ r ɒ ŋ oʊ ˈ r ɒ ŋ oʊ /; [2] Rapa Nui: roŋoroŋo [ˈɾoŋoˈɾoŋo]) is a system of glyphs discovered in the 19th century on Easter Island that has the appearance of writing or proto-writing.
Easter Island is a volcanic island, consisting mainly of three extinct coalesced volcanoes: Terevaka (altitude 507 metres) forms the bulk of the island, while two other volcanoes, Poike and Rano Kau, form the eastern and southern headlands and give the island its roughly triangular shape.
Starting around 1100 AD, the people of Easter Island would begin construction of nearly 900 moai (large stone statues). At about 1200 AD, the people of Pohnpei, a Micronesian island, would embark on another megalithic construction, building Nan Madol, a city of artificial islands and a system of canals. By 1500, the first European explorers ...
Rapa Nui National Park (Spanish: Parque nacional Rapa Nui) is a national park and UNESCO World Heritage Site located on Easter Island, Chile. Rapa Nui is the Polynesian name of Easter Island; its Spanish name is Isla de Pascua. The island is located in the southeastern Pacific Ocean, at the southeastern extremity of the Polynesian Triangle. The ...
In the late 19th century, within a few years to decades of the destruction of Easter Island society by slave raiding and introduced epidemics, two amateur investigators recorded readings and recitations of rongorongo tablets by Easter Islanders. Both accounts were compromised at best, and are often taken to be worthless, but they are the only ...
In 1935, the Ministry of Lands and Colonization declared Easter Island a National Park and a Historic Monument. In 1936, Cornejo and Atan conducted an archaeological inventory on Easter Island, further enriching the knowledge of the island's cultural history. In 1948, Father Sebastian Englert conducted archaeological studies on Easter Island.
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Typical landscape on Easter Island; rounded extinct volcanoes covered in low vegetation. Easter Island is a volcanic island, consisting mainly of three extinct coalesced volcanoes: Terevaka (altitude 507 metres) forms the bulk of the island, while two other volcanoes, Poike and Rano Kau, form the eastern and southern headlands and give the island its roughly triangular shape.