Results 21 to 30 of about 109 (105)
A new consistent and high-precision earthquake catalogue for the Taupō Volcanic Zone, New Zealand
SeismicaThe Taupō Volcanic Zone is a ~300 km long, volcanically active region in the North Island of Aotearoa New Zealand. As well as hosting numerous active volcanoes, it is also one of the most seismically active parts of the country.
Finnigan Illsley-Kemp, Eleanor Mestel
doaj +1 more source
Frontiers in Earth Science, 2016 Crystal nucleation and growth are first order processes captured in volcanic rocks and record important information about the rates of magmatic processes and chemical evolution of magmas during their ascent and eruption.
Georg F. Zellmer +6 more
doaj +1 more source
Seismic Swarms Occurrence Rate and b-value Mapping at Taupo Volcanic Zone
SeismicaWe analyze the seismicity of the Taupō Volcanic Zone (TVZ) over a 17-year period (2007-2024) using a swarm-informed ETAS model and high-resolution b-value mapping.
Giuseppe Petrillo +3 more
doaj +1 more source
New Zealand Journal of Geology and Geophysics, Volume 69, Issue 4, December 2026.Igneous centres across the Taranaki Peninsula represent the southwestern limit of arc volcanism associated with the Tonga–Kermadec–Hikurangi subduction system. Taranaki Maunga, the youngest and largest of three andesitic stratovolcanoes, dominates the geomorphology of the Taranaki Peninsula along with the eroded remnants of the Kaitake and Pouakai ...
G. P. Thrasher +3 more
wiley +1 more source
Biological Flora of New Zealand 17: Kunzea ericoides (Myrtaceae), Kānuka
New Zealand Journal of Botany, Volume 64, Issue 4, December 2026.This review summarises the taxonomic status, morphology, physiology, ecology, plant communities, mycological, invertebrate and vertebrate interactions and human use of the New Zealand endemic tree Kunzea ericoides (A. Rich.) Joy Thomps. (kānuka) (Myrtaceae).
P. J. Bellingham +8 more
wiley +1 more source
Geothermal Energy, 2017 Supercritical geothermal systems are very high-temperature geothermal systems that are located at depths near or below the brittle–ductile transition zone in the crust where the reservoir fluid is assumed to be in the supercritical state, that is for ...
Thomas Reinsch +5 more
doaj +1 more source
Earthquake Spectra, Volume 42, Issue 4, November 2026.This study presents the computational components and workflow developed to conduct probabilistic seismic hazard analysis (PSHA) in New Zealand (NZ) using physics‐based ground‐motion simulations, referred to as “CyberShake NZ.” Semi‐automated procedures generate multiple realizations of kinematic rupture models, create rupture‐specific velocity models ...
Brendon A. Bradley +5 more
wiley +1 more source
Frontiers in Earth Science, 2019 CO2 flux measurements are often used to monitor volcanic systems, understand the cause of volcanic unrest, and map sub-surface structures. Currently, such measurements are incomplete at Tarawera (New Zealand), which erupted with little warning in 1886 ...
Ery C. Hughes +13 more
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Limnology and Oceanography Letters, Volume 11, Issue 5, September 2026.Abstract Zooplankton transfer substantial energy in aquatic food webs and are used as indicators of environmental change. Syntheses of zooplankton community dynamics globally require datasets that span a wide range of environmental gradients; however, these datasets are limited due to methodological differences across programs, taxonomic ...
Stephanie E. Figary +142 more
wiley +1 more source
Implications of Thermal Weakening and Magma Compressibility for Volcano Monitoring
Journal of Geophysical Research: Solid Earth, Volume 131, Issue 9, September 2026.Abstract Magmatic intrusion and volcanic deformation are traditionally approximated with an inflating cavity in an elastic halfspace. Various analytical models predict surface displacement as a function of pressure or volume change, depth, and elastic crustal properties.
A. Spang +4 more
wiley +1 more source