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Terevaka

Terevaka

Overview
Maunga Terevaka is the largest, tallest and youngest of three main extinct volcanoes that form Rapa Nui (Easter Island
Easter Island
Easter Island ; is a Polynesian island in the southeastern Pacific Ocean, at the southeastern most point of the Polynesian triangle. A special territory of Chile annexed in 1888, Easter Island is widely famous for its 887 extant monumental statues, called moai , created by the early Rapanui people...

) (a Chile
Chile
Chile, officially the Republic of Chile , is a country in South America occupying a long, narrow coastal strip between the Andes mountains to the east and the Pacific Ocean to the west. It borders Peru to the north, Bolivia to the northeast, Argentina to the east, and the Drake Passage in the far...

an island in the Pacific Ocean
Pacific Ocean
The Pacific Ocean is the largest of the Earth's oceanic divisions. Its name is derived from the Latin name Tepre Pacificum, "peaceful sea", bestowed upon it by the Portuguese explorer Ferdinand Magellan. It extends from the Arctic in the north to Antarctica in the south, bounded by Asia and...

). Several smaller volcanic cones and craters dot its slopes, including a crater hosting one of the island's three lakes, Rano Aroi.

thumb
While Terevaka forms the bulk of Easter Island, the island has two older volcanic peaks; Poike
Poike
Poike is one of three main extinct volcanoes that form Rapa Nui . At 370 metres, it is the island's second highest peak after Terevaka.right|275 px|thumb|[[Ahu Tongariki]] with Poike in the background...

 which forms the eastern headland and Rano Kau
Rano Kau
Rano Kau is a 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.- The crater :Rano Kau has a crater...

 the southern.
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Encyclopedia
Maunga Terevaka is the largest, tallest and youngest of three main extinct volcanoes that form Rapa Nui (Easter Island
Easter Island
Easter Island ; is a Polynesian island in the southeastern Pacific Ocean, at the southeastern most point of the Polynesian triangle. A special territory of Chile annexed in 1888, Easter Island is widely famous for its 887 extant monumental statues, called moai , created by the early Rapanui people...

) (a Chile
Chile
Chile, officially the Republic of Chile , is a country in South America occupying a long, narrow coastal strip between the Andes mountains to the east and the Pacific Ocean to the west. It borders Peru to the north, Bolivia to the northeast, Argentina to the east, and the Drake Passage in the far...

an island in the Pacific Ocean
Pacific Ocean
The Pacific Ocean is the largest of the Earth's oceanic divisions. Its name is derived from the Latin name Tepre Pacificum, "peaceful sea", bestowed upon it by the Portuguese explorer Ferdinand Magellan. It extends from the Arctic in the north to Antarctica in the south, bounded by Asia and...

). Several smaller volcanic cones and craters dot its slopes, including a crater hosting one of the island's three lakes, Rano Aroi.

thumb
While Terevaka forms the bulk of Easter Island, the island has two older volcanic peaks; Poike
Poike
Poike is one of three main extinct volcanoes that form Rapa Nui . At 370 metres, it is the island's second highest peak after Terevaka.right|275 px|thumb|[[Ahu Tongariki]] with Poike in the background...

 which forms the eastern headland and Rano Kau
Rano Kau
Rano Kau is a 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.- The crater :Rano Kau has a crater...

 the southern. Terevaka last erupted in the Pleistocene
Pleistocene
The Pleistocene is the epoch from 2.588 million to 12 000 years BP covering the world's recent period of repeated glaciations. The name pleistocene is derived from the Greek and ....

and is less than 400,000 years old. Its lava field at Roiho has been dated at between 110,000 and 150,000 years old. Terevaka is rather difficult to climb, and is only accessible by foot or horse. It is very windy at the top.

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