Question: Where did the original inhabitants of the location where Rano Raraku is come from?

full_context: Document 1: 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 2: 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 3: Arthur's Seat: Like the rock on which Edinburgh Castle is built, it was formed by an extinct volcano system of Carboniferous age (lava samples have been dated at 341 to 335 million years old), which was eroded by a glacier moving from west to east during the Quaternary (approximately the last two million years), exposing rocky crags to the west and leaving a tail of material swept to the east. This is how the Salisbury Crags formed and became basalt cliffs between Arthur's Seat and the city centre. From some angles, Arthur's Seat resembles a lion couchant. Two of the several extinct vents make up the 'Lion's Head' and the 'Lion's Haunch'.
Document 4: Mons Rümker: Mons Rümker is an isolated volcanic formation that is located in the northwest part of the Moon's near side, at selenographic coordinates 40.8° N, 58.1° W and is the planned landing site of the Chang'e 5 mission. The feature forms a large, elevated mound in the northern part of the Oceanus Procellarum. The mound has a diameter of 70 kilometres, and climbs to a maximum elevation of about 1,100 metres above the surrounding plain. It was named after Karl L. C. Rümker.
Document 5: 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 6: 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 7: 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 8: 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 9: 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 10: Main Crater: Main Crater () is the topographic feature that rises to about and forms the primary summit crater of Mount Erebus on Ross Island, Antarctica. Inner Crater, which lies within Main Crater, contains an anorthoclase–phonolite lava lake.
Document 11: Hoa Hakananai'a: Hoa Hakananai'a is a "moai" (Easter Island statue) housed in the British Museum in London. It was taken from Orongo, Rapa Nui (Easter Island) in November 1868 by the crew of the British ship , and arrived in England in August 1869. Though relatively small, it is considered to be typical of the island’s statue form, but distinguished by carvings added to the back, associated with the island birdman cult. It has been described as a "masterpiece" and "without a doubt, the finest example of Easter Island sculpture".
Document 12: 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 13: Arenal Volcano: The eruptions of May 7, 1998 damaged two square kilometers and destroyed a 400 by 100 meter area of green forest in the vicinity of Arenal Volcano. A fissure, 500 meters long and 10 meters deep, was opened up in the wall of the crater and all the material slid down the side of the volcano.
Document 14: West Hawk Lake: West Hawk Lake is located in the Whiteshell Provincial Park in southeastern Manitoba, Western Canada. The central portion of the lake is formed by the West Hawk crater, caused by a meteor impact into an ancient rock bed composed of mostly granite. Granite cliffs surround parts of the lake. This area is also known as part of the Canadian Shield that was formed billions of years ago. Parts of the Whiteshell park have elaborate petroforms that were made by First Nation peoples, possibly over a thousand years ago. There are petroform shapes of turtles, snakes, humans and geometrical patterns, often found upon pink granite ridges that were shaped during the last ice age.
Document 15: 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.
ground_truth: the Marquesas Islands from the west
sub_queries: Rano Raraku >> part of Answer: Easter Island
where did the original inhabitants of Easter Island come from Answer: the Marquesas Islands from the west