USGS Volcano Notice - DOI-USGS-HVO-2025-06-10T17:39:56+00:00

Activity Summary:

Episode 25 precursory activity has begun in Halema‘uma‘u. Sustained lava fountaining is forecast to begin between tomorrow (Wednesday) and Thursday. However, there is a chance that activity could proceed to high fountaining today. Precursory activity started within Halemaʻumaʻu this morning, June 10. Glow and intermittent lava spattering in the north vent changed to more continuous spattering in the early morning hours. At about 5:54 AM HST, lava overflowed the north vent cone and is currently flowing onto the crater floor.  Current activity includes gas pistoning from the north vent and a lava flow onto the crater floor. Summit inflation continues since the end of episode 24 on June 5, 2025. 

Fountaining episodes have occurred approximately once per week since the start of the eruption on December 23, 2024. All eruptive activity remains within Hawaiʻi Volcanoes National Park. No significant activity has been noted along Kīlauea’s East Rift Zone or Southwest Rift Zone. Current hazards include volcanic gas emissions and windblown volcanic glass (Pele’s hair) and tephra that have impacted Hawaiʻi Volcanoes National Park and nearby communities.

Summit Observations:

Summit webcams showed glow and scattered spattering at the north vent through yesterday. This changed to more continuous spattering and gas pistoning in the early morning hours. At about 5:54 AM HST, lava overflowed the north vent cone. The north vent continues to generate a lava flow onto the crater floor during high stands of the gas pistoning events. 

Vigorous degassing is visible from both the north and south vents. The average sulfur dioxide (SO₂) emission rate during inter-episode pauses is typically around 1,200 tonnes per day (t/d). Once high fountaining begins, SO₂ emission rates are likely to increase to about 50,000 tonnes/day.  

Tiltmeter UWD, near Uēkahuna, has recovered about 13 microradians of inflationary tilt since the end of episode 24 and a tiltmeter near Sandhill (SDH) has recovered 9.5 microradians, since episode 24 ended on June 5.

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.

• 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 are available here: Kīlauea Volcano, Hawaii (West Halemaʻumaʻu crater) v1cam, Kīlauea Volcano, Hawaii (East Halemaʻumaʻu crater) v2cam, and Kīlauea volcano, Hawaii (South Halemaʻumaʻu crater) v3 cam
• Summit eruption webcams: https://www.usgs.gov/volcanoes/kilauea/summit-webcams 

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: 

Tiltmeter UWD, near Uēkahuna, has recovered about 13 microradians of inflationary tilt since the end of episode 24 and a tiltmeter near Sandhill (SDH) has recovered 9.5 microradians. As a result, the forecast window for episode 25 has again become slightly shorter and is currently between Wednesday, June 11 and Thursday, June 12. The window is subject to change depending on changes in the rate of inflationary tilt. There have been some past episodes where the precursory activity we are currently seeing was followed by high fountaining with 24 hours. As such, there is a chance that the activity could evolve to fountaining today.

The current eruption has been characterized by episodic fountaining not seen in any eruptions since the 1983–86 episodic fountains at the beginning of the Puʻuʻōʻō eruption. Fountains and lava 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 have been accompanied by strong deflation of the summit region. Pauses between the fountaining episodes have been marked by an immediate change from deflation to inflation as the magma chamber recharges and repressurizes. Lava fountaining episodes have occurred approximately once per week since the start of the eruption. 

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.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.

For discussion of Kīlauea hazards, please see: https://www.usgs.gov/observatories/hawaiian-volcano-observatory/hazards.