Currently the US volcano community is spread out over many academic institutions, includes several government agencies, is fragmented and would benefit from coordination. Often non-detection of initial volcanic unrest, and uncoordinated response to volcanic activity and eruptions leads to data of different types getting collected at different times and locations or not at all. This results in inefficient resource use and limited impact of the information obtained. 

The purpose of this Research Coordination Network is to enable, organize, and focus the collaboration of US academic researchers, the USGS, NASA, NCAR, NOAA, the Smithsonian (GVP) and foreign entities involved in volcano science. The goal of the enhanced collaboration is to advance our ability to adequately monitor the unrest and run-up to volcanic eruptions and once an eruption occurs, to adequately collect critical data and samples to develop next-generation physical/chemical models of volcanoes and through these understand processes of magma generation, transfer and eruption. 

This RCN is funded by NSF and resulted from recent community reports: ERUPT and SZ4D

We also collaborate with the SZ4D and MCS RCNs

August 25, 2020 Presentation of CONVERSE to NSF as part of RCN updates

Please see the community reports that provide information on the disciplinary workshops held in 2019

CONVERSE Infrasound Workshop Report_final

CONVERSE RCN_ Volcano Geodesy Workshop Report

Rock Workshop Report

Gas_RS meeting report

Eruption_Dynamics_Workshop_Groups_Notes

Report CONVERSE Steering Committee Skype meeting__Feb 21 2019

Below are some other reports from 2018 (and related earlier) community activities

Report 2018 COVE workshop Albuquerque 

Report 2018 CONVERSE Meeting Albuquerque

2014_US_Volcano_Seismology_white_paper

Volcanic eruptions are often preceded by geophysical or geochemical signals. Below are some examples of some detected eruption precursors.

Deformation precursors at Okmok Caldera (from ERUPT report modified from Lu and Dzurisin, 2014)
CO2/SO2 as measured in the volcanic plume shows increase prior to Turrialba eruption (from SZ4D report and modified from de Moor et al., 2016)
CO2/SO2 ratios frequently show increases prior to eruptions. Above is a compilation of detected pre-eruptive changes (from Werner et al., 2019 https://www.cambridge.org/core/books/deep-carbon/carbon-dioxide-emissions-from-subaerial-volcanic-regions/F8B4EFAE0DAF5306A8D397C23BF3F0D7/core-reader)