Article Collection in Frontiers in Earth Science

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From: Thomas Giachetti <tgiachet@xxxxxxxxxxx>


Dear colleagues,

We invite you to contribute to an Article Collection in Frontiers in Earth
Science entitled "From Magma Break-Up to Deposit: the Eventful Journey of
Volcanic Pyroclastsâ??. A description of the article collection is available
below and more details are available at
https://urldefense.com/v3/__https://www.frontiersin.org/research-topics/23603/from-magma-break-up-to-deposit-the-eventful-journey-of-volcanic-pyroclasts__;!!IKRxdwAv5BmarQ!KpnZ_cVrY4ikzp-vlR-QkEB78Dwt8FoNQ10biT7FAlb9Ls4ilWcQvbWgHd6RjUE$
.
If interested, please use the 'Participate' button to register. The
manuscript deadline is 21 December 2021 (flexible). Deadline for optional
abstracts is September 29.

Sincerely,

Topic Editors: Thomas Giachetti, Mie Ichihara, Miguel
Alatorre-Ibarguengoitia, Bettina Scheu, Thomas Shea


Explosive volcanic eruptions result from the fragmentation of the magma
below Earthâ??s surface into pyroclasts that are then dispersed by volcanic
plumes and pyroclastic density currents. These eruptions may generate
destructive pyroclastic falls and flows that have been responsible for the
deaths of thousands of people. It is thus crucial to assess how magma
breaks up into fragments and what happens to these fragments until they are
deposited. Their size, shape, and density distributions as well as their
evolution with time and space ultimately control how they will be
transported, where they will be deposited, and the textural and geochemical
record they preserve. The subterraneous nature of processes leading up to
fragmentation and pyroclast dispersal as well as our current inability to
see through volcanic plumes and pyroclastic density currents constitute
important observational gaps.

Magma fragmentation creates a wide range of pyroclasts whose initial size,
shape, and texture distributions remain poorly constrained. These pristine
fragments of magma are however permanently exposed to changes until they
are deposited. Various processes such as collisions, expansion, outgassing,
agglomeration, sintering, healing, etc acting in the conduit, the plume,
and/or the pyroclastic density currents as well as during final deposition
alter the pyroclasts and transform their distribution. Moreover, if magma
fragmentation has for long been thought of as the eruptive process that
distinguishes explosive from effusive volcanic eruptions, recent studies
have shown that effusive volcanism may also comprise phases of magma
fragmentation.

We aim at collecting original papers focusing on magma fragmentation and
the morphological, textural, and compositional evolution, transport, and
deposition of newly formed pyroclasts, whether it is in the conduit, plume,
pyroclastic flows, and fall or flow deposits. Papers looking at processes
such as primary and secondary fragmentation, inter-particle collisions,
pyroclast expansion, post-fragmentation outgassing, pyroclast
agglomeration, sintering, and healing are encouraged, as well as studies
examining the transport and deposition of tephra. Contributions originating
from analysis of natural samples, experimental volcanology and petrology,
and theoretical and numerical modeling are all welcome. We strongly
encourage papers that emphasize links between processes and products.



1-1-1-1-1-1-1-1-1-1-1-1-1-1



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End of Volcano Digest - 27 Aug 2021 to 30 Aug 2021 (#2021-80)
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