Results 61 to 70 of about 765 (157)

Magma Ascent and Accumulation Drives Surface Deformation and Ring Fault Seismicity Preceding the 2024 Eruption of Fernandina Volcano, Galápagos Islands

open access: yesJournal of Geophysical Research: Solid Earth, Volume 130, Issue 12, December 2025.
Abstract At caldera volcanoes, ring faults can play a key role in controlling the dynamics of unrest and patterns of associated surface deformation and seismicity. Here we show that the March 2024 eruption of Fernandina volcano was preceded by a 2.5‐year episode of magma accumulation, driving surface uplift and asymmetric seismicity on a ring fault ...
Andrew F. Bell   +7 more
wiley   +1 more source

Nakhlite Emplacement as Constrained by X‐Ray Computed Tomography and 3D Quantitative Textural and Petrofabric Analyses

open access: yesJournal of Geophysical Research: Planets, Volume 130, Issue 12, December 2025.
Abstract Nakhlites, clinopyroxene‐rich rocks, are the largest single‐origin suite of samples from Mars. Despite extensive study to discern their petrogenetic histories, nakhlite emplacement mechanisms and environments are not well‐constrained, and it is unknown whether they represent intrusive or extrusive igneous rocks, or a combination.
Sierra R. Ramsey   +5 more
wiley   +1 more source

Distribution and Transport of Thermal Energy within Magma–Hydrothermal Systems

open access: yesGeosciences, 2020
Proximity to magma bodies is generally acknowledged as providing the energy source for hot hydrothermal reservoirs. Hence, it is appropriate to think of a “magma–hydrothermal system” as an entity, rather than as separate systems.
John Eichelberger
doaj   +1 more source

The communication of volcano information in New Zealand – a narrative review

open access: yesNew Zealand Journal of Geology and Geophysics, Volume 68, Issue 4, Page 591-608, December 2025.
ABSTRACT Communication of volcano information is critical for effective volcanic risk management. A variety of information is communicated to inform decisions and guide actions for planning, preparedness, and response. Such information needs to be reliable, and fit‐for‐purpose across different stages of volcanic activity (quiescence, unrest, short or ...
Manomita Das   +15 more
wiley   +1 more source

Static stress implications for Kīlauea volcano activity after the 2018 Hawai'i earthquake

open access: yesGeodesy and Geodynamics
The MW6.9 thrust-faulting earthquake in Hawai'i on May 4, 2018, occurred near the Kīlauea shield volcano. We use 57-day-long continuous Global Positioning System (cGPS) data and 6-day-long semi-continuous GPS data to develop a detailed coseismic slip ...
Lupeng Zhang, Su Tian
doaj   +1 more source

Rapid metal pollutant deposition from the volcanic plume of Kīlauea, Hawai’i [PDF]

open access: gold, 2021
Evgenia Ilyinskaya   +16 more
openalex   +1 more source

Products of Littoral Explosions and their Formation Conditions: A Case Study from Episode 58 of Puʻu ʻŌʻō, Kīlauea Volcano, HI [PDF]

open access: bronze, 2020
Rebecca deGraffenried   +11 more
openalex   +1 more source

Beyond Cumulative Sum Charting in Non-Stationarity Detection and Estimation

open access: yesIEEE Access, 2019
In computer science, stochastic processes, and industrial engineering, stationarity is often taken to imply a stable, predictable flow of events and non-stationarity, consequently, a departure from such a flow. Efficient detection and accurate estimation
Felix Zhan   +8 more
doaj   +1 more source

Sheet flow caves of Kilauea Caldera, Hawaii County, Hawaii [PDF]

open access: yesInternational Journal of Speleology, 1998
Terminal lobes of sheet flows of pahoehoe lava sometimes form three-dimensional nests, initially separated by partitions consisting of accreted ‘skins” of each lobe. Melting breaks down these partitions, forming a uniform flow unit. In Kilauea Caldera we
William R. Halliday
doaj  

Hollow volcanic tumulus caves of Kilauea Caldera, Hawaii County, Hawaii [PDF]

open access: yesInternational Journal of Speleology, 1998
In addition to lava tube caves with commonly noted features, sizable subcrustal spaces of several types exist on the floor of Kilauea Caldera. Most of these are formed by drainage of partially stabilized volcanic structures enlarged or formed by ...
William R. Halliday
doaj  

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