Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador
Cayambe Volcano is an ice-capped, 5,790 m high, andesitic-dacitic volcanic complex, located on the equator in the Eastern Cordillera of the Ecuadorian Andes. An eruption at Cayambe would pose considerable hazards to surrounding communities and a nationally significant agricultural industry. Although...
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| Format: | Article |
| Language: | English |
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Frontiers Media S.A.
2021-06-01
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| Series: | Frontiers in Earth Science |
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| Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2021.680865/full |
| _version_ | 1818407194057506816 |
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| author | S. Butcher A. F. Bell S. Hernandez M. Ruiz |
| author_facet | S. Butcher A. F. Bell S. Hernandez M. Ruiz |
| author_sort | S. Butcher |
| collection | DOAJ |
| description | Cayambe Volcano is an ice-capped, 5,790 m high, andesitic-dacitic volcanic complex, located on the equator in the Eastern Cordillera of the Ecuadorian Andes. An eruption at Cayambe would pose considerable hazards to surrounding communities and a nationally significant agricultural industry. Although the only historically documented eruption was in 1785, it remains persistently restless and long-period (LP) seismicity has been consistently observed at the volcano for over 10 years. However, the sparse monitoring network, and complex interactions between the magmatic, hydrothermal, glacial, and tectonic systems, make unrest at Cayambe challenging to interpret. In June 2016 a seismic “crisis” began at Cayambe, as rates of high frequency volcano-tectonic (VT) earthquakes increased to hundreds of events per day, leading to speculation about the possibility of a forthcoming eruption. The crisis began 2 months after the Mw7.8 Pedernales earthquake, which occurred on the coast, 200 km from Cayambe. Here we show that the 2016 seismicity at Cayambe resulted from four distinct source processes. Cross correlation, template matching, and spectral analysis isolate two source regions for VT earthquakes–tectonic events from a regional fault system and more varied VTs from beneath the volcanic cone. The temporal evolution of the LP seismicity, and mean Q value of 9.9, indicate that these events are most likely generated by flow of hydrothermal fluids. These observations are consistent with a model where a new pulse of magma ascent initially stresses regional tectonic faults, and subsequently drives elevated VT seismicity in the edifice. We draw comparisons from models of volcano-tectonic interactions, and speculate that static stress changes from the Pedernales earthquake put Cayambe volcano in an area of dilation, providing a mechanism for magma ascent. Our findings provide a better understanding of “background” seismicity at Cayambe allowing faster characterization of future crises, and a benchmark to measure changes driven by rapid glacial retreat. |
| first_indexed | 2024-12-14T09:23:57Z |
| format | Article |
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| institution | Directory Open Access Journal |
| issn | 2296-6463 |
| language | English |
| last_indexed | 2024-12-14T09:23:57Z |
| publishDate | 2021-06-01 |
| publisher | Frontiers Media S.A. |
| record_format | Article |
| series | Frontiers in Earth Science |
| spelling | doaj.art-5fdb029cc1f04aacaf6a00b49e70caab2022-12-21T23:08:14ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-06-01910.3389/feart.2021.680865680865Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, EcuadorS. Butcher0A. F. Bell1S. Hernandez2M. Ruiz3School of Geosciences, University of Edinburgh, Edinburgh, United KingdomSchool of Geosciences, University of Edinburgh, Edinburgh, United KingdomInstituto Geofísico, Escuela Politécnica Nacional, Quito, EcuadorInstituto Geofísico, Escuela Politécnica Nacional, Quito, EcuadorCayambe Volcano is an ice-capped, 5,790 m high, andesitic-dacitic volcanic complex, located on the equator in the Eastern Cordillera of the Ecuadorian Andes. An eruption at Cayambe would pose considerable hazards to surrounding communities and a nationally significant agricultural industry. Although the only historically documented eruption was in 1785, it remains persistently restless and long-period (LP) seismicity has been consistently observed at the volcano for over 10 years. However, the sparse monitoring network, and complex interactions between the magmatic, hydrothermal, glacial, and tectonic systems, make unrest at Cayambe challenging to interpret. In June 2016 a seismic “crisis” began at Cayambe, as rates of high frequency volcano-tectonic (VT) earthquakes increased to hundreds of events per day, leading to speculation about the possibility of a forthcoming eruption. The crisis began 2 months after the Mw7.8 Pedernales earthquake, which occurred on the coast, 200 km from Cayambe. Here we show that the 2016 seismicity at Cayambe resulted from four distinct source processes. Cross correlation, template matching, and spectral analysis isolate two source regions for VT earthquakes–tectonic events from a regional fault system and more varied VTs from beneath the volcanic cone. The temporal evolution of the LP seismicity, and mean Q value of 9.9, indicate that these events are most likely generated by flow of hydrothermal fluids. These observations are consistent with a model where a new pulse of magma ascent initially stresses regional tectonic faults, and subsequently drives elevated VT seismicity in the edifice. We draw comparisons from models of volcano-tectonic interactions, and speculate that static stress changes from the Pedernales earthquake put Cayambe volcano in an area of dilation, providing a mechanism for magma ascent. Our findings provide a better understanding of “background” seismicity at Cayambe allowing faster characterization of future crises, and a benchmark to measure changes driven by rapid glacial retreat.https://www.frontiersin.org/articles/10.3389/feart.2021.680865/fulllong-period seismicityvolcano-seismic swarmsvolcano-glacier interactionsvolcanic monitoringvolcano-tectonic interactions |
| spellingShingle | S. Butcher A. F. Bell S. Hernandez M. Ruiz Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador Frontiers in Earth Science long-period seismicity volcano-seismic swarms volcano-glacier interactions volcanic monitoring volcano-tectonic interactions |
| title | Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador |
| title_full | Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador |
| title_fullStr | Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador |
| title_full_unstemmed | Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador |
| title_short | Evolution of Seismicity During a Stalled Episode of Reawakening at Cayambe Volcano, Ecuador |
| title_sort | evolution of seismicity during a stalled episode of reawakening at cayambe volcano ecuador |
| topic | long-period seismicity volcano-seismic swarms volcano-glacier interactions volcanic monitoring volcano-tectonic interactions |
| url | https://www.frontiersin.org/articles/10.3389/feart.2021.680865/full |
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