Oruanui eruption: Difference between revisions
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[[Image:Taupo 2.png|thumb|420 px|A climactic period of the Oruanui eruption as it may have appeared from space]] |
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The '''Oruanui eruption''' of [[New Zealand]]'s [[Lake Taupo|Taupo volcano]] was the world's largest known eruption in the past 70,000 years, with a [[Volcanic Explosivity Index]] of 8. It occurred around 26,500 [[Before Present]] in [[Late Pleistocene]] and generated approximately 430 km³ of [[pyroclastic fall]] deposits, 320 km³ of [[pyroclastic density current]] (PDC) deposits (mostly [[ignimbrite]]) and 420 km³ of primary intracaldera material, equivalent to 530 km³ of [[magma]]. The eruption is divided into 10 phases on the basis of nine mappable fall units and a tenth, poorly preserved but volumetrically dominant fall unit. |
The '''Oruanui eruption''' of [[New Zealand]]'s [[Lake Taupo|Taupo volcano]] was the world's largest known eruption in the past 70,000 years, with a [[Volcanic Explosivity Index]] of 8. It occurred around 26,500 [[Before Present]] in [[Late Pleistocene]] and generated approximately 430 km³ of [[pyroclastic fall]] deposits, 320 km³ of [[pyroclastic density current]] (PDC) deposits (mostly [[ignimbrite]]) and 420 km³ of primary intracaldera material, equivalent to 530 km³ of [[magma]]. The eruption is divided into 10 phases on the basis of nine mappable fall units and a tenth, poorly preserved but volumetrically dominant fall unit. |
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Revision as of 00:08, 26 March 2008
The Oruanui eruption of New Zealand's Taupo volcano was the world's largest known eruption in the past 70,000 years, with a Volcanic Explosivity Index of 8. It occurred around 26,500 Before Present in Late Pleistocene and generated approximately 430 km³ of pyroclastic fall deposits, 320 km³ of pyroclastic density current (PDC) deposits (mostly ignimbrite) and 420 km³ of primary intracaldera material, equivalent to 530 km³ of magma. The eruption is divided into 10 phases on the basis of nine mappable fall units and a tenth, poorly preserved but volumetrically dominant fall unit.
Modern Lake Taupo partly fills the caldera generated during this eruption; a 140 km² structural collapse area is concealed beneath the lake, while the lake outline reflects coeval peripheral and volcano-tectonic collapse. Early eruption phases saw shifting vent positions; development of the caldera to its maximum extent (indicated by lithic lag breccias) occurred during phase 10.
The Oruanui eruption shows many unusual features; its episodic nature, wide range of depositional conditions in fall deposits of very wide dispersal, and complex interplay of falls and pyroclastic flows.
Tephra from the eruption covered much of the central North Island with ignimbrite up to 200 metres deep. Most of New Zealand was affected by ashfall, with even an 18 cm ash layer left on the Chatham Islands, 1,000 km away. Later erosion and sedimentation had long-lasting effects on the landscape, and caused the Waikato River to shift from the Hauraki Plains to its current course through the Waikato to the Tasman Sea.
See also
References
- Wilson, Colin J. N. (2001). "The 26.5 ka Oruanui eruption, New Zealand: an introduction and overview". Journal of Volcanology and Geothermal Research. 112: 133–174. doi:10.1016/S0377-0273(01)00239-6.
- Manville, Vern & Wilson, Colin J. N. (2004). "The 26.5 ka Oruanui eruption, New Zealand: a review of the roles of volcanism and climate in the post-eruptive sedimentary response". New Zealand Journal of Geology & Geophysics. 47: 525–547.
{{cite journal}}: CS1 maint: multiple names: authors list (link) - Wilson, Colin J. N.; et al. (2006). "The 26.5 ka Oruanui Eruption, Taupo Volcano, New Zealand: Development, Characteristics and Evacuation of a Large Rhyolitic Magma Body". Journal of Petrology. 47 (1): 35–69. doi:10.1093/petrology/egi066.
{{cite journal}}: Explicit use of et al. in:|author=(help) - Richard Smith, David J. Lowe and Ian Wright. 'Volcanoes - Lake Taupo', Te Ara - the Encyclopedia of New Zealand, updated 16-Apr-2007.