10.

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9.

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8. 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. 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 397 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.

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7. Poike (370 m)

Poike is one of three main extinct volcanoes that form Rapa Nui (Easter Island) (a Chilean island in the Pacific Ocean). At 370 m, it is the island's second highest peak after Terevaka.

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6. Maunga Terevaka (507 m)

Maunga Terevaka is the largest, tallest (507.41 m) and youngest of three main extinct volcanoes that form Rapa Nui (Easter Island) (a Chilean island in the Pacific Ocean). Several smaller volcanic cones and craters dot its slopes, including a crater hosting one of the island's three lakes, Rano Aroi.

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5. Lake Pehoé

Lake Pehoé (Spanish pronunciation: [peoˈe]) is a surface water body located in Torres del Paine National Park, in the Magallanes Region of southern Chile. The lake is fed mainly by Paine River through the Nordenskjöld Lake, but it also receives the waters of the outlet of Skottsberg Lake.

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4. Rano Kau (324 m)

Rano Kau is a 324 m 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. Rano Kau has a crater lake which is one of the island's only three natural bodies of fresh water. Most of the volcano is on the coast and has been eroded back to form high sea cliffs which at one point have started to bite into the crater wall. On its northern side, the volcano slopes down to Mataveri International Airport.

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3. Parinacota (6348 m)

Parinacota is a massive potentially active stratovolcano on the border of Chile and Bolivia. It is part of the Nevados de Payachata volcanic group. The other major edifice in that group is the Pleistocene peak of Pomerape. Parinacota's last eruptive phase has been dated using the helium surface exposure technique, which ties the eruption to 290AD ± 300 years.

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2. Cordillera del Paine (2884 m)

The Cordillera del Paine is a small mountain group in Torres del Paine National Park in Chilean Patagonia. It is located 280 km (170 mi) north of Punta Arenas, and about 1,960 km south of the Chilean capital Santiago. It belongs to the Commune of Torres del Paine in Última Esperanza Province of Magallanes and Antártica Chilena Region.

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1. Easter Island

Easter Island is a Polynesian island in the southeastern Pacific Ocean, at the southeastern point of the Polynesian Triangle. A special territory of Chile that was annexed in 1888, Easter Island is famous for its 887 extant monumental statues, called moai, created by the early Rapanui people. It is a UNESCO World Heritage Site, with much of the island protected within Rapa Nui National Park.

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