 | This article needs additional citations for
verification. (November 2019) |
| Pukao Seamount | |
|---|---|
| Summit depth | Below Sea level |
| Height | 2500+ m |
| Location | |
| Location | west of Easter Island |
| Geology | |
| Type | Submarine volcano |
| Volcanic arc/ chain | Sala Y Gomez ridge |
| Age of rock | 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
- ^ 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.
| Culture |
|  | ||||
|---|---|---|---|---|---|---|
| Geography and geology | ||||||
| Administration |
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26°55′56″S 110°14′56″W / 26.9323°S 110.2490°W
 | This article about a specific oceanic location or ocean current is a stub. You can help Wikipedia by expanding it. |
 | This Chile location article is a stub. You can help Wikipedia by expanding it. |
| This article needs additional citations for
verification. (November 2019) |
| Pukao Seamount | |
|---|---|
| Summit depth | Below Sea level |
| Height | 2500+ m |
| Location | |
| Location | west of Easter Island |
| Geology | |
| Type | Submarine volcano |
| Volcanic arc/ chain | Sala Y Gomez ridge |
| Age of rock | 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
- ^ 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.
| Culture |
| | ||||
|---|---|---|---|---|---|---|
| Geography and geology | ||||||
| Administration |
| |||||
26°55′56″S 110°14′56″W / 26.9323°S 110.2490°W
|
| This article about a specific oceanic location or ocean current is a stub. You can help Wikipedia by expanding it. |
|
| This Chile location article is a stub. You can help Wikipedia by expanding it. |