Fernandina volcano erupts, lava flow reaching the ocean, Galapagos

Fernandina volcano erupts, lava flow reaching the ocean, Galapagos

A new eruption started at Fernandina volcano (Cerro la Cumbre) in Ecuador around 15:00 UTC on June 16, 2018, IGEPN reports. This large shield volcano is a part of Galapagos volcanic archipelago. Its last eruption occurred in September 2017.

The eruption is taking place on the north-northeast flank of the volcano and is so far characterized by the emission of lava flows and a gas column rising up to 3 km (1.8 miles) and drifting southwest.

According to the personnel of the Galapagos National Park, the lava flow has already reached the ocean.

The eruption of Fernandina volcano on June 16, 2018. Credit: Sabina Estupiñan, Marcelo Izquierdo and Daniel Muñoz

There are no human settlements in the area of the eruption and until IGEPN's latest report on June 16, there was no evidence of ash emission.

The agency is advising residents and tourists to stay away from the area in eruption and in particular from the area where lava flows are entering the ocean due to possible explosions and a large amount of toxic gas.

The eruption was preceded by a swarm of earthquakes, with the first one at 12:37 UTC on June 16.

Geological summary

Fernandina, the most active of Galápagos volcanoes and the one closest to the Galápagos mantle plume, is a basaltic shield volcano with a deep 5 x 6.5 km (3.1 to 4 miles) summit caldera. The volcano displays the classic "overturned soup bowl" profile of Galápagos shield volcanoes.

Its caldera is elongated in a NW-SE direction and formed during several episodes of collapse. Circumferential fissures surround the caldera and were instrumental in the growth of the volcano. Reporting has been poor in this uninhabited western end of the archipelago, and even a 1981 eruption was not witnessed at the time.

In 1968 the caldera floor dropped 350 m (1 148 feet) following a major explosive eruption. Subsequent eruptions, mostly from vents located on or near the caldera boundary faults, have produced lava flows inside the caldera as well as those in 1995 that reached the coast from a SW-flank vent.

The collapse of a nearly 1 km3 (0.24 mi3) section of the east caldera wall during an eruption in 1988 produced a debris-avalanche deposit that covered much of the caldera floor and absorbed the caldera lake. (GVP)

Featured image: The eruption of Fernandina volcano on June 16, 2018. Credit: Sabina Estupiñan, Marcelo Izquierdo  and  Daniel Muñoz


Producing content you read on this website takes a lot of time, effort, and hard work. If you value what we do here, please consider becoming a supporter.



Dave 3 years ago

I was on the my Daphnesailing towards fernandina just afer the eruption started at around 1230. At a distance we thought it was a fire but as we approached we realised that it was an eruption. We stayed near to the shoreline unit the lava hit the sea and caused the huge steam cloud.
We returned after dark to see spectacular scenes of rivers and spouts of lava spewing from fissures. Truly remarkable!

Teo Blašković (@Dave) 3 years ago

Thanks for reporting.

Post a comment

Your name: *

Your email address: *

Comment text: *

The image that appears on your comment is your Gravatar