- 1Instituto de Geofísica, UNAM, CDMX, Mexico (jose729@ciencias.unam.mx)
- 2Instituto de Geofísica, UNAM, CDMX, Mexico (jacome@igeofisica.unam.mx)
- 3Instituto de Geofísica, UNAM, CDMX, Mexico (robin@igeofisica.unam.mx)
- 4Instituto de Geofísica, UNAM, CDMX, Mexico (victoria@geofisica.unam.mx)
- 5Istituto Nazionale di Geofisica e Vulcanologia, Palermo, Italy (salvatore.inguaggiato@ingv.it)
El Chichón is an active volcano in Chiapas, Mexico, that features a hydrothermal system characterized by thermal springs, fumaroles and an acid crater lake. Many studies have focused on tracking the geochemical evolution of its fluids since its last eruption in 1982 and some have specifically aimed to evaluate the geothermal potential. This work assesses the evolution of the geothermal potential through time using published geochemical data (1983-2025). We use geochemical diagrams, temperatures estimated with geothermometers and water-rock interaction analysis to identify the main system changes that influence the geothermal potential estimations. Given that El Chichón has been considered a geothermal prospect since the 1980s, we discuss the possible uses of this resource in terms of its recent active seismicity, the risk scenarios and the local socio-cultural context.
How to cite: Salas Ferman, J. L., Jácome Paz, M. P., Campion, R., Armienta, M. A., and Inguaggiato, S.: Temporal evaluation of El Chichon´s geothermal potential in the period of 1983-2025. , EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-15407, https://doi.org/10.5194/egusphere-egu26-15407, 2026.