Terevaka

Mauga Terevaka
Highest point
Elevation	507.41 m (1,664.7 ft)
Coordinates	27°5′4″S 109°22′46″W / 27.08444°S 109.37944°WCoordinates: 27°5′4″S 109°22′46″W / 27.08444°S 109.37944°W
Geography
Location	Easter Island
Geology
Mountain type	Shield volcano
Last eruption	Pleistocene

Ma′unga Terevaka is the largest, tallest (507.41 m (1,664.73 ft)) 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.

Map of Rapa Nui showing Terevaka, Poike and Rano Kau

Terevaka from space with Hanga Roa above and Rano Kau at top - a west up photo from Nasa

While Terevaka forms the bulk of Easter Island, the island has two older volcanic peaks; Poike which forms the eastern headland and Rano Kau the southern. Terevaka last erupted in the Pleistocene 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 an easy walk up on a trail that starts next to the moai at Ahu Akivi, by foot or horse. It is often very windy at the top.

See also

• List of volcanoes in Chile

References

• Haase, Karsten M.; Peter Stoffers; C. Dieter Garbe-Schönberg (October 1997). "The Petrogenetic Evolution of Lavas from Easter Island and Neighbouring Seamounts, Near-ridge Hotspot Volcanoes in the SE Pacific". Journal of Petrology 38 (06): 785–813. doi:10.1093/petrology/38.6.785. Retrieved 2010-03-16.
• Kaneoka I, Katsui Y, 1985. K-Ar ages of volcanic rocks from Easter Island. Bull Volc Soc Japan, 30: 33-36.
• Vezzoli L, Acocella V, 2009. Easter Island, SE Pacific: an end-member type of hotspot volcanism. Geol Soc Amer Bull, 121: 869-886.

External links

• Guide to Easter Island from the Easter Island Foundation
• Old photos of Rano Aroi (upper right)