Results 61 to 70 of about 392 (152)
Implications of Thermal Weakening and Magma Compressibility for Volcano Monitoring
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
Over the past decade several “seismometers in schools” programmes have been developed in Aotearoa New Zealand by a range of organisations, for a variety of reasons and aiming to achieve a range of educational outcomes.
Graham Leonard (2855981) +12 more
core +1 more source
Abstract Porosity and permeability in crystalline shield basement are commonly assumed to be low, yet some fault zones sustain fluid circulation over kilometer scales. Here we quantify multiscale fault‐zone connectivity at Kivetty, central Finland, by integrating legacy deep‐borehole data, including packer tests, downhole logs, and a long‐term multi ...
Daniel Carbajal‐Martínez +8 more
wiley +1 more source
Abstract Although geothermal energy is a low‐carbon resource, some powerplants can coproduce and release CO2 ${\text{CO}}_{2}$, which is then subject to emissions monitoring and sometimes financial penalty. Accurate attribution of these emissions is difficult because exploitation of the reservoir alters hydrological flows that in turn modify surface ...
David Dempsey
wiley +1 more source
Two caldera forming ignimbrite eruptions of Taupō volcano (New Zealand) are among the most violent, powerful, and complex known Late Quaternary volcanic eruptions on Earth. The >530 km3 (dense rock equivalent [DRE]) ~25.5 ka Ōruanui, and 35 km3 (DRE) 232
Stephen Piva (8513037)
core +1 more source
Conspecific Negative Distance‐Dependence and New Zealand Podocarp Forest Dynamics
ABSTRACT The Janzen‐Connell hypothesis proposed that conspecific negative density or distance dependence (CNDDD) helps maintain the species richness of tropical rainforests through the action of specialist natural enemies that suppress conspecific recruitment beneath canopy trees.
Christopher H. Lusk +2 more
wiley +1 more source
Seismic Anisotropy And Time-Frequency Analyses During Taupō's 2019 Unrest
The currently active Taupō volcano (with its most recent eruptive event at ∼ 1.8 ka) was responsible for Earth’s youngest supereruption at 25.5 ka. In the past 141 years, 21 unrest events have been observed in records of seismicity, crustal deformation ...
Bakkar Hindeleh, Henriette (14104113)
core +1 more source
A Microphysical Model for Predicting Magma Fragmentation
Abstract Explosive volcanic eruptions occur when coherent bubbly magma breaks apart in a process called “fragmentation.” Accurate conceptual and numerical models of fragmentation are a pre‐requisite for prediction of eruption explosivity. However, existing models, which neglect bubble‐scale magma physics, agree poorly with new experimental evidence ...
Jérémie Vasseur +6 more
wiley +1 more source
A Dendrogeochemical Study of Kauri & The 232 Ce Taupō Eruption
Full Text is available to authenticated members of The University of Auckland only.The exact date of the devastating Late Holocene Taupō eruption has been debated for decades with the currently accepted date set at 232 +/- 10 years Common Era (CE). This
Caffin, Michael John
core
Implications of a Supervolcano’s Seismicity
Last year’s rumblings beneath New Zealand’s Taupō supervolcano, the site of Earth’s most recent supereruption, lend new urgency to research and outreach efforts in the ...
Simon Barker (277881) +3 more
core +1 more source

