Izalco

Geography & Climate

Izalco is located in El Salvador, within the Central America Volcanic Arc of the broader Middle America-Caribbean Volcanic Regions. Situated at 13.81° N, 89.63° W in the Northern Hemisphere, the volcano lies within a tropical climate zone. With a summit elevation of 1,950 meters above sea level, Izalco is a moderately sized peak that remains accessible to hikers and researchers for much of the year. The volcanic landform is characterized as a composite, which describes the physical shape and structure of the volcanic edifice as observed from the surface.

Geological Context

Izalco sits in a subduction zone, where one tectonic plate dives beneath another, creating intense heat and pressure that generates magma. Subduction zones are responsible for many of the world's most explosive volcanoes and deadliest eruptions. For communities in El Salvador near Izalco, this tectonic setting means the volcano is capable of producing powerful explosive eruptions, pyroclastic flows, and lahars that can threaten populated areas within tens of kilometers of the summit. The dominant rock type is andesite / basaltic andesite, a dark, fine-grained volcanic rock that forms from rapidly cooling, low-viscosity lava. Basaltic eruptions tend to be less explosive and produce fluid lava flows that can travel long distances. While less immediately dangerous than explosive eruptions, basaltic lava flows can destroy structures and infrastructure in their path, and volcanic gases released during these eruptions can affect air quality over a wide area.

Eruption History Summary

Izalco has 20 recorded eruptions in the geological database, spanning from 1884 CE to 1966 CE. The most powerful recorded event was a severe eruption capable of regional ash fall and pyroclastic flows in 1948 CE, reaching VEI 3 on the Volcanic Explosivity Index. Notable eruptions include 1948 CE (VEI 3), 1925 CE (VEI 3). With an average interval of roughly 4 years between eruptions over a span of 82 years, this is one of the more frequently active volcanoes in the database. This persistent activity suggests a robust and well-supplied magma system beneath the volcano. The most recent eruption in 1966 CE places this volcano within the modern era of volcanological observation.

Significance

With a maximum recorded VEI of 3, Izalco has produced eruptions capable of generating pyroclastic flows and significant ash fall in the surrounding area. While not among the largest eruptions globally, VEI 3 events pose serious hazards to local populations and can disrupt regional air travel. Its 20 recorded eruptions make it one of the most prolific volcanoes in our database, reflecting a persistent and well-documented eruptive history that has provided volcanologists with extensive data for understanding eruption patterns and forecasting future activity. Given its recent activity, Izalco is closely monitored by geological survey organizations to provide early warning of future unrest.

GVP Reference Summary

Volcán de Izalco began growing in 1770 CE on the southern flank of Santa Ana volcano, eventually building a steep 650-m-high stratovolcano truncated by a 250-m-wide summit crater. Frequent Strombolian eruptions during the two centuries prior to the cessation of activity in 1966 provided a night-time beacon for ships, causing it to be known as El Faro, the "Lighthouse of the Pacific." The dominantly basaltic andesite tephra and lava flows are geochemically distinct from those of both Santa Ana and its fissure-controlled flank vents. Lava flows have primarily erupted from flank vents, traveling as far as about 7 km south down the slopes of Santa Ana.

— Smithsonian Institution, Global Volcanism Program