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Pukao (seamount)

Coordinates: 26°55′56″S 110°14′56″W / 26.9323°S 110.2490°W / -26.9323; -110.2490
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Pukao Seamount
Summit depthBelow Sea level
Height2500+ m
Location
Locationwest of Easter Island
Geology
TypeSubmarine volcano
Volcanic arc/chainSala Y Gomez ridge
Age of rockPleistocene
Last eruption>100,000 BCE

The Pukao Seamount is a submarine volcano, the most westerly in the Easter Seamount Chain or Sala y Gómez ridge. To the east are Moai (seamount) and then Easter Island. It rises over 2,500 metres from the ocean floor to within a few hundred metres of the sea surface.[1] The Pukao Seamount is fairly young, and believed to have developed in the last few hundred thousand years as the Nazca Plate floats over the Easter hotspot.

See also

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References

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  1. ^ Haase, Karsten M.; Peter Stoffers and 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.

26°55′56″S 110°14′56″W / 26.9323°S 110.2490°W / -26.9323; -110.2490