Question: Where did the original inhabitants of the place that contains Poike come from?

full_context: Document 1: Teide: If measured from the ocean floor, it is at 7,500 m (24,600 ft) the highest volcano in the world base - to - peak outside of the Hawaiian Islands, and is described by UNESCO and NASA as Earth's third - tallest volcanic structure. Teide's elevation makes Tenerife the tenth highest island in the world. Teide is an active volcano: its most recent eruption occurred in 1909 from the El Chinyero vent on the northwestern Santiago rift. The United Nations Committee for Disaster Mitigation designated Teide a Decade Volcano because of its history of destructive eruptions and its proximity to several large towns, of which the closest are Garachico, Icod de los Vinos and Puerto de la Cruz. Teide, Pico Viejo and Montaña Blanca form the Central Volcanic Complex of Tenerife.
Document 2: Teide: Mount Teide (Spanish: Pico del Teide, pronounced (ˈpiko ðel ˈtei̯ðe), ``Teide Peak '') is a volcano on Tenerife in the Canary Islands, Spain. Its 3,718 - metre (12,198 ft) summit is the highest point in Spain and the highest point above sea level in the islands of the Atlantic.
Document 3: Indigenous peoples of the Americas: According to the 2002 Census, 4.6% of the Chilean population, including the Rapanui (a Polynesian people) of Easter Island, was indigenous, although most show varying degrees of mixed heritage. Many are descendants of the Mapuche, and live in Santiago, Araucanía and the lake district. The Mapuche successfully fought off defeat in the first 300–350 years of Spanish rule during the Arauco War. Relations with the new Chilean Republic were good until the Chilean state decided to occupy their lands. During the Occupation of Araucanía the Mapuche surrendered to the country's army in the 1880s. Their land was opened to settlement by Chileans and Europeans. Conflict over Mapuche land rights continues to the present.
Document 4: Anakena: Anakena is unusual for Easter Island in that it is one of only two small sandy beaches in an otherwise rocky coastline.
Document 5: Marshall Islands: Micronesians settled the Marshall Islands in the 2nd millennium BC, but there are no historical or oral records of that period. Over time, the Marshall Island people learned to navigate over long ocean distances by canoe using traditional stick charts.
Document 6: Rano Raraku: Rano Raraku is a volcanic crater formed of consolidated volcanic ash, or tuff, and located on the lower slopes of Terevaka in the Rapa Nui National Park on Easter Island in Chile. It was a quarry for about 500 years until the early eighteenth century, and supplied the stone from which about 95% of the island's known monolithic sculptures (moai) were carved. Rano Raraku is a visual record of moai design vocabulary and technological innovation, where 887 moai remain. Rano Raraku is in the World Heritage Site of Rapa Nui National Park and gives its name to one of the seven sections of the park.
Document 7: Lōʻihi Seamount: Lōihi Seamount (also known as Lōʻihi) is an active submarine volcano about 35 km (22 mi) off the southeast coast of the island of Hawaii. The top of the seamount is about 975 m (3,000 ft) below sea level. This seamount is on the flank of Mauna Loa, the largest shield volcano on Earth. Lōihi, meaning ``long ''in Hawaiian, is the newest volcano in the Hawaiian - Emperor seamount chain, a string of volcanoes that stretches over 5,800 km (3,600 mi) northwest of Lōʻihi. Unlike most active volcanoes in the Pacific Ocean that make up the active plate margins on the Pacific Ring of Fire, Lōʻihi and the other volcanoes of the Hawaiian - Emperor seamount chain are hotspot volcanoes and formed well away from the nearest plate boundary. Volcanoes in the Hawaiian Islands arise from the Hawaii hotspot, and as the youngest volcano in the chain, Lōihi is the only Hawaiian volcano in the deep submarine preshield stage of development.
Document 8: Samoa: The Samoan islands have been produced by vulcanism, the source of which is the Samoa hotspot which is probably the result of a mantle plume. While all of the islands have volcanic origins, only Savai'i, the western most island in Samoa, is volcanically active with the most recent eruptions in Mt Matavanu (1905–1911), Mata o le Afi (1902) and Mauga Afi (1725). The highest point in Samoa is Mt Silisili, at 1858 m (6,096 ft). The Saleaula lava fields situated on the central north coast of Savai'i are the result of the Mt Matavanu eruptions which left 50 km² (20 sq mi) of solidified lava.
Document 9: Easter Island: Polynesian people most likely settled on Easter Island sometime between 700 and 1100 AD and created a thriving and industrious culture as evidenced by the island's numerous enormous stone moai and other artifacts. However, human activity, the introduction of the Polynesian rat and overpopulation led to gradual deforestation and extinction of natural resources which severely weakened the Rapa Nui civilization. By the time of European arrival in 1722, the island's population had dropped to 2,000 -- 3,000 from an estimated high of approximately 15,000 just a century earlier. European diseases and Peruvian slave raiding in the 1860s further reduced the Rapa Nui population, to a low of only 111 inhabitants in 1877.
Document 10: Jean-Baptiste Dutrou-Bornier: Jean-Baptiste Onésime Dutrou-Bornier (19 November 1834 – 6 August 1876) was a French mariner who settled on Easter Island in 1868, purchased much of the island, removed many of the Rapa Nui people and turned the island into a sheep ranch.
Document 11: Easter Island: 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 (5 April) in 1722, while searching for Davis or David's island. Roggeveen named it Paasch - Eyland (18th - century Dutch for`` Easter Island''). The island's official Spanish name, Isla de Pascua, also means ``Easter Island ''.
Document 12: Canary Islands: When the Europeans began to explore the islands in the late Middle Ages, they encountered several indigenous peoples living at a Neolithic level of technology. Although the prehistory of the settlement of the Canary Islands is still unclear, linguistic and genetic analyses seem to indicate that at least some of these inhabitants shared a common origin with the Berbers on the nearby North African coast. The precolonial inhabitants came to be known collectively as the Guanches, although "Guanches" had been the name for only the indigenous inhabitants of Tenerife. From the 14th century onward, numerous visits were made by sailors from Majorca, Portugal and Genoa. Lancelotto Malocello settled on Lanzarote in 1312. The Majorcans established a mission with a bishop in the islands that lasted from 1350 to 1400.
Document 13: History of Easter Island: The Austronesian Polynesians, who first settled the island, are likely to have arrived from the Marquesas Islands from the west. These settlers brought bananas, taro, sugarcane, and paper mulberry, as well as chickens and Polynesian rats. The island at one time supported a relatively advanced and complex civilization.
Document 14: Poike: Poike is one of three main extinct volcanoes that form Rapa Nui (Easter Island) (a Chilean island in the Pacific Ocean). At 370 metres, it is the island's second highest point after Terevaka.
Document 15: Bagana: Bagana is an active volcano located in the centre of the island of Bougainville, Papua New Guinea, the largest island of the Solomon group. It is the most active volcano in the country, occupying a remote portion of central Bougainville Island. It is one of Melanesia's youngest and most active volcanoes.
ground_truth: the Marquesas Islands from the west
sub_queries: Poike >> part of Answer: Easter Island
where did the original inhabitants of Easter Island come from Answer: the Marquesas Islands from the west