Fall AGU Session: Arc Dynamics of Kamchatka (V30)

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From: Michael Ramsey <mramsey+@xxxxxxxx>
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For those of you who have an interest in the Kamchatka region of
Russia, we would
like to draw your attention (and encourage your abstract submissions) to the
following special session at this year's Fall AGU meeting.

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V30: Arc Dynamics of Kamchatka: Recent Volcanological, Geophysical,
and Petrologic Results

Michael Ramsey (University of Pittsburgh)
Adam Simon (University of Nevada Las Vegas)
Michael West (University of Alaska Fairbanks)


Kamchatka, Russia is one of the most seismically and volcanically
active regions on Earth, with one of the fastest subduction rates of
any arc.  The peninsula contains 29 active volcanoes, beginning in the
north at the terminus of the Aleutian arc and ending in the south at
the start of the Kurile Islands.  Many of these volcanoes are in a
near-constant state of eruption, threatening both the local
populations as well as the numerous daily trans-Pacific flights of
people and cargo.  The Kamchatka volcanoes have a wide range of
compositions, styles, and morphologies, which can range from
hydrothermal systems, to fissure-fed basaltic flows, to composite
volcanoes that produce lava domes, flows, and large ash columns.  This
diversity of volcanic activity and the openness of Russia in the past
decade have made Kamchatka an attractive location for numerous
scientific studies.  Investigators have initiated collaborative
research projects with Russian scientists ranging from NSF-sponsored
programs focused on specific volcanic systems to NASA-sponsored
programs such as the Asia-Pacific Natural Laboratory (APNL), which is
focused on regional-scale scientific questions.  We seek to bring
together investigators who have worked on volcanic arc processes in
Kamchatka recently using methods ranging from geophysics of the
subsurface to remote sensing of ongoing eruptions.  We would
particularly like to highlight larger-scale, longer time-line
collaborative studies that combine several fields of geoscience in
order to better understand the dynamics and volcanology of the
Kamchatka Arc, including comparison to other arcs.

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