English: Composite from https://en.wiki.x.io/wiki/Taup%C5%8D_Volcano#/media/File:Lake_taupo_landsat.jpg and my own work based on Volcanic Unrest at Taupō Volcano in 2019: Causes, Mechanisms and Implications in Geochemistry Geophysics Geosystems June 2021 by Illsley-Kemp F. et al., volcanic vents updated as per Tapscott 2023
(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 Geophysics47 (3): 525. DOI:10.1080/00288306.2004.9515074.
(1 June 2021). "Volcanic Unrest at Taupō Volcano in 2019: Causes, Mechanisms and Implications". Geochemistry, Geophysics, Geosystems22 (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
The three unlabeled vents relating to 232 CE eruption and later Waitahanua Bank vent are according to the work of Tapscott 2023 are from south to north:
Y1 and Y3 phases of the 232 CE eruption
Horomatangi Reefs which is now Y2 and Y5 of the 232 CE eruption as well as post 232 CE vent
Waitahanui Bank, a post 232 CE vent
Y4 phase of the 232 CE eruption
Previous work (1980) had initially one vent for the 232 CE eruption, then several and suggested up to 5 recent vents. All locations and outlines are approximate in this figure.
This image is a derivative work of the following images:
This image is in the public domain because it is a screenshot from NASA’s globe software World Wind using a public domain layer, such as Blue Marble, MODIS, Landsat, SRTM, USGS or GLOBE.
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