Upper holocene tephro-chronostratigraphy of Irazú Volcano, Costa Rica

• Published in: Scientific reports Vol. 14; no. 1; p. 7100
• Main Authors: Campos-Durán, Daniela, Alvarado, Guillermo E., Martí, Joan
• Format: Journal Article
• Language: English
• Published: London Nature Publishing Group UK 26-03-2024; Nature Publishing Group; Nature Portfolio
• Subjects: 704/2151; 704/4111; Cinder cones; Eruptions; Explosions; Holocene; Humanities and Social Sciences; Irazú volcano; multidisciplinary; Radiometric dating; Risk management; Science; Science (multidisciplinary); Stratigraphy; Tephra deposits; Tephro-chronostatigraphy; Upper Holocene; Volcanic hazards; Volcanoes; Costa Rica; Tephro-chronostatigraphy; Eruptive recurrence; Irazú volcano; Upper Holocene; Volcanic hazards; Radiometric dating; Tephra deposits
• DOI: 10.1038/s41598-024-57962-7
• EISSN: 2045-2322

Irazú is one of the largest and most active volcanoes in Costa Rica. We present the tephro-chronostratigraphy of the last 2.6 ka of the Irazú volcano based on detailed field work and C
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radiometric dating, as well as a revision of the geological and historical records. In the stratigraphic record we identified at least 30 tephra units. Eight of them corresponding to the historical period (i.e., after 1700 A.D.), separated by repose periods of different durations. The distribution of the deposits, the volcanic morphologies (craters and pyroclastic cones) and the radiometric ages indicate that most of this recent eruptive activity has occurred from the summit of Irazú along an E–W fissure (~ 4 km long). Toward the west of the summit, near the Sapper hill may be the source of the oldest eruptions at 200 A.D., while the La Laguna cone, located to the east of the summit, could have formed around 1540 A.D., and Main Crater to the west could have formed around sixteenth–seventeenth century. Since then, the historical eruptions (i.e., 1723–1724, 1917–1921, 1924, 1928, 1930, 1933, 1939–1940 and 1963–1965) have been sourced from this crater, but not all of them are registered in the stratigraphy. The eruption frequency of Irazú during this period ranges from 23 to 100 years, with a major event about every 80 years. Irazu’s eruptions have been mainly phreatomagmatic and Strombolian, including some phreatic explosions. We present a detailed tephro-chronostratigraphy that will help to building temporal analysis for hazard assessment and risk management plans to face future eruptions at Irazú.