Easter Island Essay

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Rapa Nui, or Easter Island is a tiny speck of land secluded in the southeastern part of the Pacific Ocean. "Ancient voyaging from the central islands of eastern Polynesia would have normally gone against the prevailing trade winds, with the island forming only a small target, although westerly winds associated with periodic ENSO may have carried Polynesian colonists to the island (Anderson, Caveides and Walden, Finney)". Volcanoes constitute the three rims of Rapa Nui. In addition to the cones of three dominant volcanoes (Rano Kao, Poike, and Maunga Terevaka), Easter Island's landscape is also dotted with nearly 70 subsidiary cones. The most ancient stones are 500,000 year old alkali basalt/hawaiite lava flows constructing the Poike composite volcano at the island's eastern edge. Poike, which was formerly an island that eventually became joined to Terevaka by basalt flows emitted from Terevaka, has been seriously crumbled by the sea on each and every edge. The southwest flank of Rapa Nui was created by the Kao volcano. The Rano Kao lake inside the volcano's crater is one of Easter Island's only three pure chunks of crisp water. The water from the exceedingly submerged crater, which is approximately 3,000 feet in width, is carried to Easter Island's capital, Hanga Roa. The crater is roughly a mile in diameter and features a unique microclimate protected from winds. The lake has an abundance of climbing plants. The interior declivity was the spot of the most recent wild toromoro tree just before the species was felled for cordwood in 1960. The majority of Kao volcano is on the seacoast and has been abraded back to build towering sea escarpments which at one time have begun to cut into the caldera precipice. Kao is halfway between Poike and Terevaka in the level of its sea escarpment and soil growth. The Terevaka volcano dominates almost the entire mainland of Rapa Nui

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