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| Pukao Seamount | |
|---|---|
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| Summit depth | Below Sea level |
| Height | 2500+ m |
| Location | |
| Location | west ofEaster Island |
| Geology | |
| Type | Submarine volcano |
| Volcanicarc/chain | Sala Y Gomez ridge |
| Age of rock | Pleistocene |
| Last eruption | >100,000BCE |
ThePukao Seamount is asubmarine volcano, the most westerly in theEaster Seamount Chain orSala y Gómez ridge. To the east areMoai (seamount) and thenEaster 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 theNazca Plate floats over theEaster hotspot.
26°55′56″S110°14′56″W / 26.9323°S 110.2490°W /-26.9323; -110.2490
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