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Mainshock-aftershock clustering in volcanic regions Mainshock-aftershock clustering in volcanic regions

Earthquakes break their general Poissonean behavior through two types of seismic bursts: swarms and mainshock-aftershock sequences. The former is commonly thought to dominate in volcanic and geothermal regions, but aftershock production, including within swarms, is not well studied in volcanic regions. Here we compare mainshock-aftershock clustering in active volcanic regions in Japan to...
Authors
Ricardo Garza Giron, Emily E. Brodsky, Stephanie Prejean

Modeled inundation limits of potential lahars from Mount Adams in the White Salmon River Valley, Washington Modeled inundation limits of potential lahars from Mount Adams in the White Salmon River Valley, Washington

Lahars large enough to reach populated areas are a hazard at Mount Adams, a massive volcano in the southern Cascade Range of Washington State (fig. 1). It is considered to be still active and has the potential to erupt again. By definition, lahars are gravity-driven flows of water-saturated mixtures of mud and rock (plus or minus ice, wood, and other debris), which originate from...
Authors
Julia P. Griswold, Thomas C. Pierson, Joseph A. Bard

Lahar—River of volcanic mud and debris Lahar—River of volcanic mud and debris

Lahar, an Indonesian word for volcanic mudflow, is a mixture of water, mud, and volcanic rock flowing swiftly along a channel draining a volcano. Lahars can form during or after eruptions, or even during periods of inactivity. They are among the greatest threats volcanoes pose to people and property. Lahars can occur with little to no warning, and may travel great distances at high...
Authors
Jon J. Major, Thomas C. Pierson, James W. Vallance

Multi-year high-frequency hydrothermal monitoring of selected high-threat Cascade Range volcanoes Multi-year high-frequency hydrothermal monitoring of selected high-threat Cascade Range volcanoes

From 2009 to 2015 the U.S. Geological Survey (USGS) systematically monitored hydrothermal behavior at selected Cascade Range volcanoes in order to define baseline hydrothermal and geochemical conditions. Gas and water data were collected regularly at 25 sites on 10 of the highest-risk volcanoes in the Cascade Range. These sites include near-summit fumarole groups and springs/streams that...
Authors
I.M. Crankshaw, Stacey A. Archfield, A. C. Newman, Deborah Bergfeld, Laura E. Clor, Peter J. Kelly, William C. Evans, Kurt R. Spicer, Steven E. Ingebritsen

Joint 3-D tomographic imaging of Vp, Vs and Vp/Vs and hypocenter relocation at Sinabung volcano, Indonesia from November to December 2013 Joint 3-D tomographic imaging of Vp, Vs and Vp/Vs and hypocenter relocation at Sinabung volcano, Indonesia from November to December 2013

We conducted travel time tomography using P- and S-wave arrival times of volcanic-tectonic (VT) events that occurred between November and December 2013 to determine the three-dimensional (3D) seismic velocity structure (Vp, Vs, and Vp/Vs) beneath Sinabung volcano, Indonesia in order to delineate geological subsurface structure and to enhance our understanding of the volcanism itself...
Authors
Andri Dian Nugraha, Novianti Indrastuti, Ridwan Kusnandar, Hendra Gunawan, Wendy A. McCausland, Atin Nur Aulia, Ulvienin Harlianti

Natural hazards in Goma and the surrounding villages, East African Rift System Natural hazards in Goma and the surrounding villages, East African Rift System

The city of Goma and its surrounding villages (Democratic Republic of the Congo, DRC) are among the world’s most densely populated regions strongly affected by volcanic hazards. In 2002, Nyiragongo volcano erupted destroying 10–15% of Goma and forced a mass evacuation of the population. Hence, the ~ 1.5 million inhabitants of Goma and Gisenyi (Rwanda) continue to live with the threat of...
Authors
Charles M. Balagizi, Antoine Kies, Marcellin M. Kasereka, Dario Tedesco, Mathieu M. Yalire, Wendy A. McCausland

Imaging a crustal low-velocity layer using reflected seismic waves from the 2014 earthquake swarm at Long Valley Caldera, California: The magmatic system roof? Imaging a crustal low-velocity layer using reflected seismic waves from the 2014 earthquake swarm at Long Valley Caldera, California: The magmatic system roof?

The waveforms generated by the 2014 Long Valley Caldera earthquake swarm recorded at station MLH show clear reflected waves that are often stronger than direct P and S waves. With waveform analyses, we discover that these waves are reflected at the top of a low-velocity body, which may be residual magma from the ∼767 ka caldera-forming eruption. The polarity of the reflection compared to...
Authors
Nori Nakata, David R. Shelly

Origin of primitive tholeiitic and calc-alkaline basalts at Newberry Volcano, Oregon Origin of primitive tholeiitic and calc-alkaline basalts at Newberry Volcano, Oregon

Major and trace element and radiogenic isotopic characteristics of primitive mafic Pleistocene and Holocene lavas from Newberry Volcano, Oregon, define two groups. The first consists of dry tholeiitic high-alumina olivine basalts that are slightly enriched in highly incompatible elements. The second group consists of calc-alkaline basalts that contained 2–4 wt % H2O prior to eruption and...
Authors
Richard W. Carlson, Timothy L. Grove, Julie M. Donnelly-Nolan

Lava lake activity at the summit of Kīlauea Volcano in 2016 Lava lake activity at the summit of Kīlauea Volcano in 2016

The ongoing summit eruption at Kīlauea Volcano, Hawai‘i, began in March 2008 with the formation of the Overlook crater, within Halema‘uma‘u Crater. As of late 2016, the Overlook crater contained a large, persistently active lava lake (250 × 190 meters). The accessibility of the lake allows frequent direct observations, and a robust geophysical monitoring network closely tracks subtle...
Authors
Matthew R. Patrick, Tim R. Orr, Donald A. Swanson, Tamar Elias, Brian Shiro

Application of an updated atmospheric model to explore volcano infrasound propagation and detection in Alaska Application of an updated atmospheric model to explore volcano infrasound propagation and detection in Alaska

Winds and temperature gradients greatly affect the long-range propagation of infrasound. The spatio-temporal variability of these parameters must therefore be accurately characterized to correctly interpret recorded infrasound at long distances, specifically to differentiate between source and propagation effects. Here we present the first results of an open source reanalysis model...
Authors
Alexandra M. Iezzi, Hans Schwaiger, David Fee, Matthew M. Haney

Presentation of the Dana Medal of the Mineralogical Society of America for 2017 to Thomas W. Sisson Presentation of the Dana Medal of the Mineralogical Society of America for 2017 to Thomas W. Sisson

I have the pleasure of introducing Thomas W. Sisson, the Mineralogical Society of America Dana Medalist for 2017. Tom is known for his scientific rigor and landmark publications that have contributed to a diverse spectrum of fields closely tied to the mineralogical sciences. He is particularly recognized for his work on magma differentiation and the role of water in subduction-related...
Authors
Charles R. Bacon

New petrological, geochemical, and geochronological perspectives on andesite-dacite magma genesis at Ruapehu volcano, New Zealand New petrological, geochemical, and geochronological perspectives on andesite-dacite magma genesis at Ruapehu volcano, New Zealand

Time–composition relationships in eruptive sequences at composite volcanoes can show how the ongoing intrusion of magmas progressively affects the lithosphere at continental convergent margins. Here, new whole-rock and microanalytical major and trace element data from andesite-dacite lava flows are integrated with previous studies and existing isotopic data, and placed within the...
Authors
Chris E Conway, John A Gamble, Colin J.N. Wilson, Graham S. Leonard, Dougal B. Townsend, Andrew T. Calvert
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