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Enormous lava geysers once again erupt from Kīlauea summit as Episode 12 begins

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Screenshot from the livestream of the lava fountaining in Halema‘uma‘u Crater during Episode 12 of the ongoing eruption of Kīlauea volcano on the Big Island as of 6:55 p.m. Tuesday, March 4, 2025.

After a slow, sporadic start Tuesday morning, the 12th episode of the ongoing summit eruption of Kīlauea volcano on the Big Island was once again putting on a fantastic fountaining display similar to that of the prior episode that saw lava geysers of up to 600 feet high.

Hawaiian Volcano Observatory reports the most recent eruptive activity of the eruption in Kaluapele, the volcano’s summit caldera, that started Dec. 23, 2024, started at 7:30 a.m. Tuesday with sporadic small lava flows alternating between the south and north vents in the southwest portion of Halema‘uma‘u Crater.

A transition to fountaining began at 2 p.m.

Fountaining of about 20 to 30 feet started at the north vent and had reached 150 to 165 feet within 20 minutes. They were expected to grow.

Episode 12 started similarly to how the fourth episode of the eruption began, preceded by several hours of sluggish overflows of lava prior to the onset of fountaining.

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However, today’s overflows were of a more intermittent nature, differing slightly from Episode 4, but also related to degassed magma from the vent prior to fountaining.

  • View from 4:50 p.m. Tuesday, March 4, 2025, of Halemaʻumaʻu Crater at the summit of Kīlauea. Camera is positioned on the south rim and the view is to the west. (U.S. Geological Survey S2cam)
  • View from 4:52 p.m. Tuesday, March 4, 2025, of Halemaʻumaʻu Crater and the crater floor from the west rim of the Kīlauea summit caldera, looking east. (U.S. Geological Survey KWcam)
  • Episode 12 of the ongoing Halemaʻumaʻu eruption began a fountaining phase at 2 p.m. Tuesday, March 4, 2025. (Photo Courtsey: U.S. Geological Survey webcam image)
  • Coincident with a scheduled Hawaiian Volcano Observatory eruption monitoring overflight the morning of Tuesday, March 4, 2025, Kīlauea’s ongoing eruption in Halema‘uma‘u Crater started to show minor activity at both eruptive vents. This aerial view of the vents taken at 8:04 a.m. shows a small new lava flow that had flowed from the south vent (left) from 7:30 to 7:50 a.m. The north vent (right) had weak spattering. (Photo Courtesy: U.S. Geological Survey/K. Lynn)
  • A Hawaiian Volcano Observatory geologist collects of molten sample of lava in the eastern portion of Halema‘uma‘u Crater the morning of March 4, 2025. In this portion of the crater, far from the eruptive vents, lava has slowly oozed out during recent days as residue from earlier eruptive episodes. All samples are collected in coordination with and after receiving permission from Hawai‘i Volcanoes National Park. Analysis of the sample will provide information for ongoing eruption hazard assessment. (Photo Courtesy: U.S. Geological Survey/M. Patrick)

Interestingly, the fourth eruptive phase of the summit eruption — which is confined within Hawai’i Volcanoes National Park — was one of the more extended episodes. It lasted 3 days, from Jan. 15-18, before pausing.

Each of the 11 prior episodes continued for between somewhat less than 13 hours to up to 8 and a half days and they were separated by pauses lasting from less than 24 hours to 12 days.

Inflationary tilt at the summit reached just more than 10 microradians since the end of Episode 11; nearly balancing out the amount of deflation lost before the beginning of Episdoe 12.

Seismic tremor began increasing and tilt at Uēkahuna tiltmeter on the summit switched from inflation to deflation at 2 p.m., at the same time fountaining began.

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High levels of volcanic gas — primarily water vapor, carbon dioxide and especially sulfur dioxide — continue to be the primary hazard of concern, as this can have far-reaching effects downwind from the summit.

As sulfur dioxide is continuously released during an eruption, it reacts in the atmosphere to create vog, or volcanic smog, downwind.

View from 7:31 p.m. Monday, March 3, 2025, of the Kīlauea caldera, from the northwest rim. (U.S. Geological Survey V1cam)

Wind conditions and timing have prevented accurate measurements of sulfur dioxide emission rates since the beginning of Episode 10 of the current eruption.

Sulfur dioxide rates are estimated to be 10,000 tonnes per day or higher during eruptive episodes based on emissions measured during earlier phases.

Strands of volcanic glass known as Pele’s hair — which can sometimes cluster and tangle together on the ground and appear like tumbleweed — have also been reported on surfaces throughout the summit area and surrounding communities.

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The extent of Pele’s hair is dependent on lava fountaining activity and current wind conditions. Residents and visitors should minimize exposure to these volcanic particles, which can cause skin and eye irritation.

Additional hazards include other volcanic fragments from lava fountains that can fall on the ground downwind of the eruptive vents.

No changes have been detected in Kīlauea’s East Rift Zone or Southwest Rift Zone.

Kīlauea’s Volcano Alert Level and Aviation Color Code remain at Watch and Orange, respectively.

Hawaiian Volcano Observatory continues to closely monitor Kīlauea and will issue an eruption update Wednesday morning unless there are significant changes before then.

  • A Hawaiian Volcano Observatory geologist measures the chemistry of volcanic gases emitted during Episode 11 of the Kīlauea summit eruption Fe 26, 2025. (Photo Courtesy: U.S. Geological Survey/M. Patrick)
  • A Hawaiian Volcano Observatory geologist uses a laser rangefinder to measure the evolving height of cinder cones produced by recent lava fountaining at the summit of Kīlauea. The highest part of the tallest cone rim was about 160 feet above the crater floor as of Feb. 26, 2025. (Photo Courtesy: U.S. Geological Survey/M. Patrick)
  • The shapes and textures of clasts produced by recent lava fountaining at the summit of Kīlauea indicate their fluid nature as they traveled through the air. (Photo Courtesy: U.S. Geological Survey/M. Patrick)
  • The density of clasts produced by recent fountaining at the summit of Kīlauea is similar to that of a kitchen sponge because of abundant gas bubbles. These bubbles range in size from ones too small to see, up to larger ones about the size of golf balls. (Photo Courtesy: U.S. Geological Survey/M. Patrick)
  • Recent lava fountaining at the summit of Kīlauea produced large frothy clasts that landed on the western caldera rim in addition to many smaller clasts that produced a thick carpet of new tephra. (Photo Courtesy: U.S. Geological Survey/M. Patrick)

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