Reconstruction of the geology and structure of Lake Rotomahana and its hydrothermal systems from high-resolution multibeam mapping and seismic surveys: Effects of the 1886 Tarawera Rift eruption

de Ronde, C.E.J.; Walker, S.L.; LeBlanc, C.; Davy, B.W.; Fornari, D.J.; Tontini, F. Caratori; Scott, B.J.; Seebeck, H.; Stewart, T.J.; Mazot, A.; Nicol, A.; Tivey, M.A.

doi:10.1016/j.jvolgeores.2016.02.002

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The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles, guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the NOAA IR retains documents in their original published format to ensure public access to scientific information.

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Reconstruction of the geology and structure of Lake Rotomahana and its hydrothermal systems from high-resolution multibeam mapping and seismic surveys: Effects of the 1886 Tarawera Rift eruption

2016
By de Ronde, C.E.J. ; Walker, S.L. ; LeBlanc, C. ; ...
Source: Journal of Volcanology and Geothermal Research, 314, 57-83

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Journal Title:

Journal of Volcanology and Geothermal Research
Personal Author:

de Ronde, C.E.J. ; Walker, S.L. ; LeBlanc, C. ; Davy, B.W. ; Fornari, D.J. ; ... More +

de Ronde, C.E.J. ; Walker, S.L. ; LeBlanc, C. ; Davy, B.W. ; Fornari, D.J. ; Tontini, F. Caratori ; Scott, B.J. ; Seebeck, H. ; Stewart, T.J. ; Mazot, A. ; Nicol, A. ; Tivey, M.A. Less -
NOAA Program & Office:

OAR (Oceanic and Atmospheric Research) ; PMEL (Pacific Marine Environmental Laboratory)

OAR (Oceanic and Atmospheric Research) ; PMEL (Pacific Marine Environmental Laboratory) Less -
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Present-day Lake Rotomahana is one of the two focal points of the most destructive eruption in New Zealand's historical record, i.e., that of Mt. Tarawera on 10 June 1886, with devastating loss of life and presumed destruction of the iconic Pink and White Terraces that adorned the margins of the lake. Basaltic dikes are considered to have ascended near surface in the area, intruding into hydrothermally altered and water-saturated ground beneath the existing lake. The consequential hydrothermal and phreatomagmatic eruptions ejected 0.5325 km3 of material from the lakefloor and below, plastering the nearby landscape for several kilometers with mud and other debris. The eruption buried the natural outlet of the lake, with the bottom of the craters becoming filled by water within months and completely concealed from view within years; today Lake Rotomahana has depths up to 118 m.
Source:

Journal of Volcanology and Geothermal Research, 314, 57-83
DOI:

https://doi.org/10.1016/j.jvolgeores.2016.02.002
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0377-0273
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PDF
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Elsevier BV
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Journal Article
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Reconstruction of the geology and structure of Lake Rotomahana and its hydrothermal systems from high-resolution multibeam mapping and seismic surveys: Effects of the 1886 Tarawera Rift eruption

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