Summary

Improves on File:Lake taupo landsat & volcanic features.jpg but more complex with key.

Annotations based on:

• (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 and Geophysics 47 (3): 525. DOI:10.1080/00288306.2004.9515074.
• (2020). "Taupō: an overview of New Zealand's youngest supervolcano". New Zealand Journal of Geology and Geophysics. DOI:10.1080/00288306.2020.1792515.
• (1 June 2021). "Volcanic Unrest at Taupō Volcano in 2019: Causes, Mechanisms and Implications". Geochemistry, Geophysics, Geosystems 22 (6): 1–27. DOI:10.1029/2021GC009803.
• Re-establishing the beast: an investigation into the spatiotemporal evolution of the Y5 phase of the Taupō 232±10 CE eruption, New Zealand: a thesis submitted in partial fulfilment of a Philosophiae Doctor degree in Earth Science, Volcanic Risk Solutions, School of Agriculture and Environment (Thesis)^[1], Massey University, New Zealand, 2023
• (2021). "Shallow subaqueous to emergent intra-caldera silicic volcanism of the Motuoapa Peninsula, Taupo Volcanic Zone, New Zealand–New constraints from geologic mapping, sedimentology and zircon geochronology". Journal of Volcanology and Geothermal Research 411. DOI:10.1016/j.jvolgeores.2021.107180.

The three vents relating to 232 CE eruption and later Waitahanua Bank vent are according to the work of Tapscott 2023 are from south to north:

1. Y1 and Y3 phases of the 232 CE eruption
2. Horomatangi Reefs which is now Y2 and Y5 of the 232 CE eruption as well as post 232 CE vent
3. Waitahanui Bank, a post 232 CE vent
4. Y4 phase of the 232 CE eruption

Licensing

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• File:Satellite image of New Zealand in December 2002.jpg

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