Here's The Awesome Science Behind Kilauea's Beautiful, Violent Lava Fountains

Lava fountaining seen at Fissure 22. One reached a height of 45 meters (150 feet)! USGS via Facebook

Robin Andrews 22 May 2018, 18:21

What’s taking place right now on Hawaii’s Big Island is as multifaceted an eruption as you’re likely to get. Aside from the eye-catching explosive activity at Kilauea’s summit, you’ve also got nearly two dozen fissures that have opened up in the last few weeks in the East Rift Zone (ERZ). Along with the acidic laze created when their lava oozes fall into the sea, their propagation has destroyed property and triggered sudden evacuations.

As is clearly shown by that spectacular cover shot, courtesy of the United States Geological Survey’s (USGS) Hawaiian Volcano Observatory (HVO), you’ve also got lava fountaining. Although it’s a common feature of plenty of eruptions, including those taking place here, the imagery captured by experts this time around is so resplendent that it warrants an explainer of its own – so what is it, exactly?

In recent days, the volcanism in the ERZ has stepped up a gear; four fissures’ flows have merged into one, which has created an ominous, beautifully singular, anastomosing flow, replete with said fire fountains and heightened, hazardous sulfur dioxide emissions.


The USGS’s latest advisories often speak of spatter – the ejection of blebs of lava from the flows – which is generally triggered by small amounts of rapidly expanding volcanic gases. These gases, once dissolved in the magma, are exsolving under less restrictive atmospheric pressures; they turn into bubbles, which embiggen and fling small amounts of lava all over the place.

Lava fountaining is, crudely put, spattering’s big sister. It comes in a variety of forms, but the same process of rapidly expanding gas applies.


Sicily’s Stromboli – the Lighthouse of the Mediterranean – has a lava fountain-prone eruption style. As the magma here slowly rises through its conduit (its rocky esophagus), the confining pressure on the magma decreases, which allows bubbles to form. These often coalesce into a single, large slug.

When this slug gets to the vent, it “pops”, and this rapid depressurization event flings lava into the air. At night, it illuminates the tiny island, hence the nickname.

A thermal map of the current fissure system in the ERZ, as of May 21. USGS
Full Article

If you liked this story, you'll love these

This website uses cookies

This website uses cookies to improve user experience. By continuing to use our website you consent to all cookies in accordance with our cookie policy.