Pukao (seamount) explained

Pukao Seamount
Depth:Below Sea level
Height:2500+ m
Location:west of Easter Island
Volcanic Group:Sala Y Gomez ridge
Age:Pleistocene
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

References

-26.9323°N -110.249°W

Notes and References

  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 . 10.1093/petrology/38.6.785. free .