Volcanic Unrest at Taupō Volcano in 2019: Causes, Mechanisms and Implications [PDF]
Geochemistry, Geophysics, Geosystems, 2021 Taupō volcano, New Zealand, is a large caldera volcano that has been highly active through the Holocene. It most recently erupted ∼1,800 years ago but there have been multiple periods of historic volcanic unrest.
Finnigan Illsley‐Kemp +9 more
doaj +2 more sources
Geochemistry, Geophysics, Geosystems, 2023 Oxygen isotopes are useful for tracing interactions between magmas, crustal rocks and surface‐derived waters. We use them here to consider links between voluminous silicic magmatism and large‐scale hydrothermal circulation in New Zealand's central Taupō ...
Shane M. Rooyakkers +6 more
doaj +2 more sources
Scenario-based modelling of waves generated by sublacustrine explosive eruptions at Lake Taupō, New Zealand [PDF]
Natural Hazards and Earth System Sciences, 2023 Volcanogenic tsunami and wave hazard remains less understood than that of other tsunami sources. Volcanoes can generate waves in a multitude of ways, including subaqueous explosions.
M. W. Hayward +5 more
doaj +2 more sources
Environmental Impact of Silicic Magmatism in Large Igneous Province Events
Geophysical Monograph Series, Page 133-151., 2021 Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Scott E. Bryan
wiley +1 more source
Development of a Bayesian event tree for short-term eruption onset forecasting at Taupō volcano [PDF]
, 2022 Taupō volcano, located within the Taupō Volcanic Zone (TVZ) in the central North Island of Aotearoa-New Zealand, is one of the world's most active silicic caldera systems.
Scott E +4 more
core +1 more source
The 2001 Taupō Fault Belt Seismicity as Evidence of Magma‐Tectonic Interaction at Taupō Volcano
Geochemistry, Geophysics, Geosystems, 2022 The Taupō Volcanic Zone (TVZ) is the southern extent of the Tonga‐Kermadec volcanic arc and encompasses the Taupō Rift, with the two structures accommodating extension through the central North Island of New Zealand via magmatic and tectonic processes,
R. F. D. McGregor +2 more
doaj +1 more source
Lake Levelling Data from Lake Taupō, 1979-2021
, 2021 This dataset contains lake levelling measurements from Lake Taupō covering the period 1979-2021. If you use this data please cite: Otway, P., Illsley-Kemp, F., Mestel, E.R.H. Review of lake levelling surveys at Lake Taupō, 1979-2021.
Mestel, Eleanor +2 more
core +1 more source
Paleomagnetic constraint of the age and duration of the Taupō Eruption, New Zealand
Earth, Planets and Space, 2023 We have carried out paleomagnetic analyses of tephras from the Taupō eruption, one of the most violent eruptions on Earth in the past 5000 years. Pyroclastic deposits were collected with 7 cm3 cubes pushed into each unit of the Taupō eruption sequence ...
Takeshi Hasegawa +9 more
doaj +1 more source
The 2001 Taupō Fault Belt Seismicity as Evidence of Magma-Tectonic Interaction at Taupō Volcano
, 2022 The Taupō Volcanic Zone (TVZ) is the southern extent of the Tonga-Kermadec volcanic arc and encompasses the Taupō Rift, with the two structures accommodating extension through the central North Island of New Zealand via magmatic and tectonic processes ...
Finnigan Illsley-Kemp (8511963) +2 more
core +1 more source
, 2022 Contains two supplementary figures: Supplementary Figure S1. Minimum resolvable inflating sphere volume at each station around Lake Taupō as a function of source depth and overpressure Supplementary Figure 2.
Finnigan Illsley-Kemp (8511963) +12 more
core +1 more source