Maui News

Lowering of Lava Lake Raises Potential for Explosive Eruptions

May 9, 2018, 10:40 AM HST
* Updated May 9, 10:58 AM

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The Halemaʻumaʻu lava lake from the evening of May 7, 2018 shows the agitated lake surface caused by intemittent rock falls. Falling rocks are common since the lava lake level has dropped quickly, and exposed the walls. On Sunday, the lake level was about 220 m (240 yards) below the crater rim and it continues to drop. PC: US Geological Survey.

The steady lowering of the lava lake in “Overlook crater” within Halemaʻumaʻu at the summit of Kīlauea Volcano has raised the potential for explosive eruptions in the coming weeks.

Scientists with the Hawaiian Volcano Observatory say that if the lava column drops to the level of groundwater beneath Kīlauea Caldera, influx of water into the conduit could cause steam-driven explosions.

Debris expelled during such explosions could impact the area surrounding Halemaʻumaʻu and the Kīlauea summit.

“At this time, we cannot say with certainty that explosive activity will occur, how large the explosions could be, or how long such explosive activity could continue,” HVO geologists said in a volcanic activity notice issued this morning.

Residents of the Kīlauea summit area are advised to learn about the hazards of ashfall, stay informed of the status of the volcano and area closures, and review family and business emergency plans.


Resource on volcanic ash hazards:


Primary hazards of concern should this activity occur are ballistic projectiles and ashfall.

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Ash column. PC: US Geological Survey 5.9.18

Ash Column Rises from Overlook Crater (8:29 a.m. 5.9.18)

Ash column rises from the Overlook crater at the summit of Kīlauea Volcano. HVO’s interpretation is that the explosion was triggered by a rockfall from the steep walls of Overlook crater. The photograph was taken at 8:29 a.m. HST from the Jaggar Museum overlook. The explosion was short-lived. Geologists examining the ash deposits on the rim of Halema‘uma‘u crater found fresh lava fragments hurled from the lava lake. This explosion was not caused by the interaction of the lava lake with the water table. When the ash cleared from the crater about an hour after the explosion, geologists were able to observe the lava lake surface, which is still above the water table.



During steam-driven explosions, ballistic blocks up to 2 m (yards) across could be thrown in all directions to a distance of 1 km (0.6 miles) or more. These blocks could weigh a few kilograms (pounds) to several tons.

Smaller (pebble-size) rocks could be sent several kilometers (miles) from Halemaʻumaʻu, mostly in a downwind direction.


Presently, during the drawdown of the lava column, rockfalls from the steep enclosing walls of the Overlook crater vent impact the lake and produce small ash clouds. These clouds are very dilute and result in dustings of ash (particles smaller than 2 mm) downwind.

Should steam-driven explosions begin, ash clouds will rise to greater elevations above ground. Minor ashfall could occur over much wider areas, even up to several tens of miles from Halemaʻumaʻu. In 1924, ash may have reached as high as 20,000 feet above sea level. Small amounts of fine ash from these explosions fell over a wide area as far north as North Hilo (Hakalau), in lower Puna, and as far south as Waiohinu.

Gas emitted during steam-drive explosions will be mainly steam, but will include some sulfur dioxide (SO2) as well. Currently, SO2 emissions remain elevated.


Steam-driven explosions at volcanoes typically provide very little warning. Once the lava level reaches the groundwater elevation, onset of continuous ashy plumes or a sequence of violent steam-driven explosions may be the first sign that activity of concern has commenced.


Kīlauea’s lava lake began to drop on May 2, 2018. From its peak on May 2 to the most recent measurement at 9 pm on May 6, the lava lake surface dropped a total of more than 200 m (656 ft). The subsidence was at a relatively constant rate of about 2 meters (yards) per hour.

Measurements of subsidence have not been possible since May 6 because of thick fume and the increasing depth to the lava surface. However, thermal images indicate continued lowering of the lake surface since that time, consistent with deflationary tilt recorded at Kīlauea’s summit. Therefore, we infer that the lake surface continues to drop at roughly the same rate. So, while HVO cannot report exact depths of the receding lava lake, we can monitor the overall trend.

USGS and HVO scientists are monitoring changes at the summit 24/7 and watching for signs that hazardous conditions have increased, or may increase. HVO is working closely with Hawai’i Volcanoes National Park and Hawai’i County Civil Defense to respond to this situation.


Updates on activity will be posted on the HVO website at

You can receive these updates by email through a free subscription service:

Hawai’i County Civil Defense will issue its own hazard notices should that become necessary:

Hawai’i Volcanoes National Park status is posted on their web page:

Resources on volcanic ash can be found at:

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