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Geochemical modeling of iron and aluminum precipitation during mixing and neutralization of acid mine drainage Geochemical modeling of iron and aluminum precipitation during mixing and neutralization of acid mine drainage

Geochemical modeling of precipitation reactions in the complex matrix of acid mine drainage is fundamental to understanding natural attenuation, lime treatment, and treatment procedures that separate constituents for potential reuse or recycling. The three main dissolved constituents in acid mine drainage are iron, aluminum, and sulfate. During the neutralization of acid mine drainage...
Authors
D. Kirk Nordstrom

Cyclic shear zone cataclasis and sintering during lava dome extrusion: Insights from Chaos Crags, Lassen Volcanic Center (USA) Cyclic shear zone cataclasis and sintering during lava dome extrusion: Insights from Chaos Crags, Lassen Volcanic Center (USA)

The ascent and extrusion of crystal-rich magma is commonly facilitated by deformation partitioned within annular, conduit-parallel shear zones. The physical properties and textures of the shear zone materials, where exposed at surface, provide a record of ascent and eruption dynamics. We describe the shear zone developed in Dome C, part of Chaos Crags in the Lassen Volcanic Center...
Authors
Amy Ryan, Michael J. Heap, James K. Russell, Lori A. Kennedy, Michael A. Clynne

The prevalence and significance of offset magma reservoirs at arc volcanoes The prevalence and significance of offset magma reservoirs at arc volcanoes

Determining the spatial relations between volcanic edifices and their underlying magma storage zones is fundamental for characterizing long-term evolution and short-term unrest. We compile centroid locations of upper crustal magma reservoirs at 56 arc volcanoes inferred from seismic, magnetotelluric, and geodetic studies. We show that magma reservoirs are often horizontally offset from...
Authors
Allan H. Lerner, Daniel O'Hara, Leif Karlstrom, Susanna K. Ebmeier, Kyle R. Anderson, Shaul Hurwitz

Geology and eruptive history of Bogoslof volcano Geology and eruptive history of Bogoslof volcano

Bogoslof volcano is a shallow submarine/subaerial volcano in the southern Bering Sea about 100 km west of the community of Dutch Harbor, Alaska. The subaerial parts of the volcano consist of two small islands, Bogoslof Island and Fire Island, that together have a total area of about 1.6 km2. Bogoslof was first depicted on a Russian map in 1772 and since then has been observed and visited
Authors
Christopher F. Waythomas, Matthew Warren Loewen, Kristi L. Wallace, Cheryl E. Cameron, Jessica F. Larsen

Felsic melt and gas mobilisation during magma solidification: An experimental study at 1.1 kbar Felsic melt and gas mobilisation during magma solidification: An experimental study at 1.1 kbar

Melt and gas transfer processes are essential to the formation and growth of the Earth’s crust and for sustaining volcanic activity. These processes also play a major role in magma fractionation at shallow depths (
Authors
Mattia Pistone, Lukas Baumgartner, Florence Begue, Paul A. Jarvis, Elias Bloch, Martin Robyr, Othmar Muntener, Thomas W. Sisson, Jon D. Blundy

Observations on the structure of Surtsey Observations on the structure of Surtsey

Comparison of investigations of the 1979 and 2017 cored boreholes coupled with continued observations of the dynamic surface of Surtsey has modified our concepts of the subsurface structure of the volcano. A geometrical analysis of the 2017 vertical and inclined cores indicates that near-surface layering dips westerly, indicating that the boreholes are located inside the Surtur crater...
Authors
James G. Moore, Marie D. Jackson

Modeling groundwater inflow to the new crater lake at Kīlauea Volcano, Hawaiʻi Modeling groundwater inflow to the new crater lake at Kīlauea Volcano, Hawaiʻi

During the 2018 eruption of Kīlauea Volcano, Hawai'i, scientists relied heavily on a conceptual model of explosive eruptions triggered when lava‐lake levels drop below the water table. Numerical modeling of multiphase groundwater flow and heat transport revealed that, contrary to expectations, liquid water inflow to the drained magma conduit would likely be delayed by months to years...
Authors
Steven E. Ingebritsen, Ashton F. Flinders, James P. Kauahikaua, Paul A. Hsieh

Source model for Sabancaya volcano constrained by DInSAR and GNSS surface deformation observation Source model for Sabancaya volcano constrained by DInSAR and GNSS surface deformation observation

Sabancaya is the most active volcano of the Ampato-Sabancaya Volcanic Complex (ASVC) in southern Perú and has been erupting since 2016. The analysis of ascending and descending Sentinel-1 orbits (DInSAR) and Global Navigation Satellite System (GNSS) datasets from 2014 to 2019 imaged a radially symmetric inflating area, uplifting at a rate of 35 to 50 mm/yr and centered 5 km north of...
Authors
Gregorio Boixart, Luis Cruz, Rafael Miranda, Pablo Euillades, Leonardo Euillades, Maurizio Battaglia

The health hazards of volcanic and geothermal gases: A guide for the public The health hazards of volcanic and geothermal gases: A guide for the public

This guide has been prepared by the International Volcanic Health Hazard Network (IVHHN) to explain the potential adverse health effects of volcanic and geothermal gas and aerosol emissions. It provides general information on how to protect yourself and your family. The information is based on a range of evidence from academics and health and regulatory agencies. Contact your local...
Authors
Bernadette Longo, Tamar Elias, Claire J. Horwell

The 1951 eruption of Mount Lamington, Papua New Guinea: Devastating directed blast triggered by small-scale edifice failure The 1951 eruption of Mount Lamington, Papua New Guinea: Devastating directed blast triggered by small-scale edifice failure

The catastrophic explosion of Mount Lamington volcano, Papua New Guinea on January 21, 1951 produced a devastating pyroclastic density current (PDC) that knocked down dense tropical rainforest over an area of 230 km2 and killed approximately 3000 people. We present results of a field reinvestigation of the 1951 PDC deposit combined with an analysis of the available photographs and...
Authors
Alexander Belousov, Marina Belousova, Richard P. Hoblitt, Herman Patia

Major-oxide and trace-element geochemical data from rocks collected on Little Sitkin Island, from Little Sitkin Volcano, Alaska Major-oxide and trace-element geochemical data from rocks collected on Little Sitkin Island, from Little Sitkin Volcano, Alaska

During the 2005 summer field season, geologists Michelle Coombs, Christina Neal, and Jessica Larsen from the University of Alaska, Fairbanks and the U.S. Geological survey, Alaska Volcano Observatory (AVO) conducted fieldwork on Little Sitkin Island in the western Aleutians of Alaska. The primary purpose of the fieldwork was to install geophysical networks for volcano monitoring. As part...
Authors
Jessica Larsen, Christina A. Neal, Cheryl E. Cameron

Radiocarbon dating of silica sinter and postglacial hydrothermal activity in the El Tatio geyser field Radiocarbon dating of silica sinter and postglacial hydrothermal activity in the El Tatio geyser field

The El Tatio geothermal field in the Chilean Altiplano contains hydrothermal silica sinter deposits overlaying glacial and volcanic units, providing an opportunity to constrain the timing of deglaciation and volcanic activity in an area with sparse absolute chronologies. We obtained 51 new radiocarbon ages and δ13C values on the organic material trapped in these sinter deposits. Based on...
Authors
Carolina Munoz Saez, Michael Manga, Shaul Hurwitz, Silvina Salgter, Dakota Churchill, Martin Reich, David Damby, Diego Morata
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