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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.
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.
Scientists turn to ancient DNA to understand the history of Easter Island, ... “Their ancestors had spent at least 3000 years living in an Oceanic environment. They sailed eastwards across ...
Easter Island is one of the youngest inhabited territories on earth, and for most of the history of Easter Island it was the most isolated inhabited territory on Earth. Its inhabitants, the Rapa Nui, have endured famines, epidemics, civil war, slave raids, and colonialism; have seen their population crash on more than one occasion.
Other researchers suggest the exact opposite — that Easter Island is a tale of a how an isolated people created a sustainable system, allowing a small but stable population to thrive for ...
New archaeological research has disproved one of the world’s most famous historical narratives - the environmental cautionary tale that claimed that the ancient civilisation of Easter Island in ...
Jared Diamond's thesis that Easter Island society collapsed in isolation entirely due to environmental damage and cultural inflexibility is contested by some ethnographers and archaeologists, who argue that the introduction of diseases carried by European colonizers and slave raiding, [16] which devastated the population in the 19th century ...
Rano Kau is a 324 m (1,063 ft) tall extinct volcano that forms the southwestern headland of Easter Island, a Chilean island in the Pacific Ocean. It was formed of basaltic lava flows in the Pleistocene with its youngest rocks dated at between 150,000 and 210,000 years ago.