Seismic monitoring of effusive-explosive activity and large lava dome collapses during 2013–2015 at Volcán de Colima, Mexico

• Published in: Journal of volcanology and geothermal research Vol. 351; pp. 75 - 88
• Main Authors: Arámbula-Mendoza, Raúl, Reyes-Dávila, Gabriel, Vargas-Bracamontes Dulce, M., González-Amezcua, Miguel, Navarro-Ochoa, Carlos, Martínez-Fierros, Alejandro, Ramírez-Vázquez, Ariel
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.02.2018
• ISSN: 0377-0273; 1872-6097
• DOI: 10.1016/j.jvolgeores.2017.12.017

Volcán de Colima, the most active volcano in Mexico, started a new eruptive cycle in January 2013. Since this date, the volcano has presented effusive and explosive activity. The beginning of the cycle was marked by a moderate Vulcanian explosion which had hyperbolical behavior in its precursory seismicity, possibly related to a shallow rupture process. Then, during the whole eruptive stage, the effusive activity was accompanied by low to moderate explosions. The explosions had energies mainly of 106joules and were located between 0 and 1600m below the crater, whereas the locations of tremor sources were found to be deeper, reaching up to 3800m beneath the crater. Very-long-period signals (VLPs) have been observed with Vulcanian explosions that produce pyroclastic flows. A few number of volcano-tectonic events (VTs) were recognized during the studied period (2013–2015), indicating that the volcano is an open system. This was particularly evidenced in July 2015, when a new batch of magma rose rapidly without large precursors, only an accelerated increase in the number of rockfalls and associated RSEM. This event generated two large lava dome collapses with several pulses of material and pyroclastic flows that travelled up to 10.3km from the summit. The seismic monitoring of Volcán de Colima is currently the only tool in real-time employed to assess the state of the volcanic activity. It is thus necessary to integrate new seismic methods as well as other geophysical monitoring techniques able to detect precursory signals of an impending hazardous event. •Automated classification of seismic events using HMMs, prove to be very useful for volcanic monitoring in real time.•A batch of magma rose rapidly without large seismic precursors, this event generated two large lava dome collapses.•Generation of VLPs during large Vulcanian explosions and with the lava dome collapses.•The explosions had energies mainly of 106 Joules and were located between 0 and 1600 m below the crater.