USGS Volcano Notice - DOI-USGS-HVO-2025-07-09T18:27:16+00:00

Activity Summary:

Episode 28 of the ongoing Halemaʻumaʻu eruption began just after 4 a.m. HST today, July 9, 2025. High fountaining is continuing at this time, with maximum fountain heights reaching nearly 1200 feet (365 meters).  

All eruptive activity remains within Hawaiʻi Volcanoes National Park, and no significant activity has been noted along Kīlauea’s East Rift Zone or Southwest Rift Zone.

Current hazards include volcanic gas emissions, along with windblown volcanic glass (Pele’s hair) and tephra that may reach roadways and communities downwind (southwest) of the summit area.

Summit Observations:

Following days of low-level gas pistoning and occasionally visible spatter and flames, activity began to increase just after 4 a.m. HST with a larger lava overflow, continuous low-level fountaining, weak deflation, and an increase in seismic tremor. Around 5:15 a.m. HST today, fountaining increased in height and vigor; at the same time, tilt began to drop sharply. High fountaining with maximum heights reaching nearly 1200 feet (365 meters) continues at the time of this update. Activity thus far – from pre-episode gas pistoning through lava overflows to the current fountaining – has been restricted to the north vent. The south vent does not show renewed activity at this time.

At the time of the onset of Episode 28, the tiltmeter near Uēkahuna (UWD) had recorded about 14 microradians of inflationary tilt since the end of episode 27. At this time, the tiltmeter has shown approximately 7.5 microradians of deflation in association with the current fountaining.

Tremor and degassing are elevated during fountaining episodes. Typical sulfur dioxide (SO₂) emission rates during high fountaining are around 75,000 tonnes/day.

Strands of volcanic glass known as Pele’s hair are present throughout the summit area of Hawaiʻi Volcanoes National Park and surrounding communities and can be remobilized by wind. Trade winds are blowing the both volcanic gases and erupted particles (tephra, ash, and Pele’s hair) to the west and southwest of Kīlauea summit today.

• Eruption resources, including the most recent map and a timeline of eruption episodes since December 23, 2024: https://www.usgs.gov/volcanoes/kilauea/science/eruption-information
• Three Kīlauea summit livestream videos that show eruptive lava fountains are available here: https://www.youtube.com/@usgs/streams 
• Summit eruption webcams: https://www.usgs.gov/volcanoes/kilauea/summit-webcams
• Volcano Watch article on gas pistoning: https://www.usgs.gov/observatories/hvo/news/volcano-watch-so-what-earth-or-least-kilauea-a-gas-piston

Rift Zone Observations:

Rates of seismicity and ground deformation remain very low in the East Rift Zone and Southwest Rift Zone, with no significant earthquake activity in the past 24 hours. Sulfur dioxide (SO₂) emissions from the East Rift Zone remain below the detection limit.

Analysis: 

Recent eruptive episodes have generally last less than 12 hours. Accordingly, we expect the fountaining associated with Episode 28 to end sometime later today.

In the next few days, as post-episode data comes in, we will likely be able to begin to forecast a possible window for the next episode.

The current eruption has been characterized by episodic lava fountaining not seen in any eruptions since the 1983–86 episodic fountains at the beginning of the Puʻuʻōʻō eruption. Lava fountains and flows have erupted from two vents within Halema'um'a'u crater that we refer to as the north vent and south vent. Each of the previous fountaining episodes lasted from a few hours to over a week and was accompanied by strong deflation of the summit region. Pauses between the fountaining episodes have been marked by an immediate switch from deflation to inflation as the magma chamber recharges and repressurizes. Fountaining episodes have occurred approximately once per week since the start of the current eruption on December 23, 2024.

HVO continues to closely monitor Kīlauea and is in contact with Hawai‘i Volcanoes National Park and the Hawai‘i County Civil Defense Agency about eruptive hazards.

Please see the Hawaiʻi Volcanoes National Park website for visitor information: https://www.nps.gov/havo/index.htm.

Hazards: 

This episodic eruption is occurring within a closed area of Hawaiʻi Volcanoes National Park. High levels of volcanic gas—primarily water vapor (H₂O), carbon dioxide (CO₂), and sulfur dioxide (SO₂)—are the primary hazard of concern, as this hazard can have far-reaching effects downwind. As SO₂ is continuously released from the summit during an eruption, it will react in the atmosphere to create the visible haze known as vog (volcanic smog) downwind of Kīlauea. SO₂ and vog may cause respiratory and other problems at high concentrations. Further information on vog can be found at https://vog.ivhhn.org/

Additional hazards include Pele's hair and other volcanic fragments from lava fountains. Pele's hair is strands of volcanic glass often produced by lava fountaining activity. Volcanic fragments can fall on the ground within a few hundred yards (meters) of the eruptive vent(s), or downwind of the vent(s). Strong winds may waft light particles, including Pele's hair, to greater distances downwind. Once they are on the ground, Pele's hair can sometimes cluster and tangle together, giving it the appearance of a tumbleweed. The extent of Pele's hair deposition is dependent on lava fountaining activity and current wind conditions. Residents and visitors should minimize exposure to Pele's hair and other volcanic fragments, which can cause skin and eye irritation. More information about how Pele's hair forms, its hazards, and what to do is available here: https://www.usgs.gov/observatories/hvo/news/volcano-watch-recent-lava-fountains-highlight-peles-hair-hazards. A recently updated Frequently Asked Questions document that includes information about potential health effects of Pele's hair is available here: https://vog.ivhhn.org/sites/default/files/PelesHair_FAQs_v2.pdf

Hawaiian lava flows generally advance slowly downslope, and during this eruption flows have been confined to Halemaʻumaʻu crater and the southwest side of Kaluapele, Kīlauea's summit caldera.

Other significant hazards also remain around Kīlauea caldera from Halemaʻumaʻu crater wall instability, ground cracking, and rockfalls that can be enhanced by earthquakes within the area closed to the public. This underscores the extremely hazardous nature of Kīlauea's caldera rim surrounding Halemaʻumaʻu crater, an area that has been closed to the public since late 2007.