Announcing the 2020 Kleinman Grants for Volcano Research

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From: "Dzurisin, Daniel" <dzurisin@xxxxxxxx>


*Announcing the 2020 Kleinman Grants for Volcano Research*



The Community Foundation for Southwest Washington announces the following
students have been awarded 2020 Kleinman Grants for Volcano Research. Jack
Kleinman was a USGS employee at the David A. Johnston Cascades Volcano
Observatory (CVO) who died in a kayaking accident in 1994. By supporting
field-oriented research projects in volcanology, the Kleinman Grants
memorialize Jackâ??s exuberance for fieldwork, volcanoes, and the natural
world. During the past 25 years, the program has helped more than 100
aspiring volcanologists who seek to learn more about volcanoes, how they
work, and how to mitigate the associated hazards.



*Emma Burkett *is an M.S. student at the University of New Hampshire (Julia
Bryce, adviser). Her research project â??Assessing Magma Storage Extent
within Crust at Augustine Volcanoâ?? is aimed at better understanding the
dynamics of Augustineâ??s magmatic system. She plans to combine information
gleaned from field observations and trace-element diffusion modeling
of plagioclase
and pyroxene crystals to: 1) evaluate the pacing of magma accumulation, 2)
compare timeline reconstructions with monitoring data with the goal of
relating above-ground indications of volcanic activity to magmatic
processes below, and 3) assess the vertical extent of the magma
storage-and-transport system beneath the volcano. Ultimately, the goal is
to learn how magmatic systems evolve, under what conditions volcanoes
erupt, and how eruptions and volcano hazards develop. The project will be
carried in collaboration with Dr. Jessica Larsen at the University of
Alaska Fairbanks.



*Annika Dechert* is a graduate student at the University of Oregon (Josef
Dufek, adviser). Her project â??Numerical Modeling of Zircons at the Three
Sisters, ORâ?? will provide more detailed information on the eruptive history
of South Sister volcano by determining zircon ages for a broad suite of
samples that represent a temporal span through the late Pleistocene and
Holocene. To interpret the zircon age populations in terms of magma
reservoir-scale dynamics and evolution, Annika will use a 3D multiphase
model that connects the growth of zircon crystals to the chemical, thermal,
and physical timeline of the magma system. Her work promises new insight
into the state of South Sisterâ??s magma system through time, including
volume; longevity; proportion of solids, melt, and fluid; chemical
composition; and temperature. The research is a collaborative effort with
Nathan Andersen (USGS) and Hélène Le Mével (Carnegie Institution).



*Marie Takach* is a Ph.D. candidate at Oregon State University (Frank
Tepley, adviser). The ultimate goal of her project â??Explosive Mixed Tephra
Deposits Reveal their Pre-Eruptive Origins (El Misti Volcano, Peru)â?? is to
determine the root cause of eruption triggers at El Misti, a historically
active, explosive volcano that threatens Arequipa, Peru, a city with one
million inhabitants. Marie plans to; 1) Use geochemical analyses of glasses
and minerals to document end-member magma compositions; 2) Apply various
geothermobarometers to describe pre-eruptive magma storage conditions each
known eruption; 3) Assess for the presence and degree of magma
mixing/mingling; 4) Test timeframes between episodes of magma
mixing/mingling and eruption by modeling plagioclase trace element
diffusion; and 5) Quantify the time elapsed between explosive eruptions and
evaluate the magma storage timescales using U-series and 40Ar-39Ar
geochronology. Field work and research will be done in collaboration with
Christopher Harpel (USGS, VDAP).



*Joshua Wiejaczka* is a Ph.D. candidate at the University of Oregon,
working under the supervision of Thomas Giachetti (adviser). With his
project â??Plinian to effusive to caldera-forming: eruptive intensity
transitions of the 7.7 ka Cleetwood and Climactic eruption of Crater Lake,
Oregon, USAâ??, Josh hopes to link shifts in eruption dynamics that occurred
during the end of the Cleetwood eruption with the initiation of the
subsequent caldera-forming eruption of Mount Mazama/Crater Lake. He
proposes to accomplish that goal by analyzing stratigraphic changes in
particle size distribution, shape, texture, porosity, and componentry that
occur throughout the products of both eruptions. In addition, Josh plans to
analyze porosity, permeability, and bubble size distribution of pumices
with a helium pycnometer, capillary flow porometer, and SEM, respectively.
Ultimately, the goal of his research is to understand why the Cleetwood
eruption was followed very quickly by caldera collapse to form modern-day
Crater Lake, whereas other Plinian eruptions of comparable size elsewhere
were not. Josh has been coordinating his plans with Charlie Bacon (USGS).


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