Terevaka

Main article: Easter Island § Geology

Ma′unga Terevaka
Highest point
Elevation	1,664 ft (507 m)
Coordinates	27°5′4″S 109°22′46″W
Geography
Location	Easter Island
Geology
Mountain type	Shield volcano
Last eruption	Pleistocene, less than 110,000 years ago

Ma′unga Terevaka is the largest, tallest (507.41 m (1,664.73 ft)) and youngest of three main extinct volcanoes that form Easter Island. 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 can be climbed via a trail that starts next to the moai at Ahu Akivi.

Terevaka is the 12th most topographically isolated summit on Earth.

See also

• List of volcanoes in Chile
• List of islands by highest point
• Topographic isolation

References

• Karsten M. Haase; 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 (6): 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

• Education-Conservation-Research Terevaka Archaeological Outreach (non-profit)
• Guide to Easter Island from the Easter Island Foundation
• Old photos of Rano Aroi (upper right)