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HAWAIIAN VOLCANO OBSERVATORY DAILY UPDATE
U.S. Geological Survey
Saturday, August 8, 2026, 8:30 AM HST (Saturday, August 8, 2026, 18:30 UTC)


KILAUEA (VNUM #332010)
19°25'16" N 155°17'13" W, Summit Elevation 4091 ft (1247 m)
Current Volcano Alert Level: ADVISORY
Current Aviation Color Code: YELLOW

Summary: Kīlauea volcano is not erupting. Models indicate another episode is likely with the current forecast between August 10 and 13.

Overview:

The summit eruption of Kīlauea in Halemaʻumaʻu remains paused. Overnight, continuous weak to moderate glow was observed from the north vent. Glow from the south vent and recently opened crack upslope diminished significantly after 10:00 p.m. and 1:30 a.m. HST, respectively. Occasional flames and intensified glow associated with gas pistoning were observed primarily from the north vent and new crack, and less frequently from the south vent. Approximately 1.3 microradians of deflationary tilt has been recorded over the past day, with deflation continuing at this time. Current models indicate that the forecast window for episode 53 has shifted to August 10–13.

No significant activity has been noted along Kīlauea’s East Rift Zone or Southwest Rift Zone.

A summary of episode 52 is posted below.

NOTE: Significant changes in activity between Daily Updates are posted here: https://www.usgs.gov/observatories/hvo/observatory-messages

 

Summit Observations:

Overnight, continuous weak to moderate glow and occasional small flames were observed from the north vent. Glow from the south vent and recently opened crack upslope diminished significantly after 10:00 p.m. and 1:30 a.m. HST, respectively, although both continued to intermittently produce weak glow or flames throughout the night.

At approximately 10:20 p.m. HST, continuous tremor transitioned to irregular periods of gas pistoning, with individual gas piston spikes occurring approximately 10–20 minutes apart. Webcams showed occasional flames and intensified glow coincident with gas piston spikes. Large flames were occasionally observed from the recently opened crack, most notably at 10:22 p.m. HST, near the transition to gas pistoning, and at 4:18 a.m. HST. Small flames were occasionally observed from the north vent and rarely from the south vent. No spatter was associated with gas pistoning overnight.

No earthquakes have been detected beneath Halemaʻumaʻu caldera over the past 24 hours.

Since the end of episode 52, the Uēkahuna (UWD) tiltmeter has recorded 11.0 microradians of inflationary tilt after earlier reaching a maximum of 12.3 microradians on UWD. UWD tilt has lost about 1.3 microradians since 6:00 a.m. HST yesterday and continues to record deflationary tilt at this time. Similar variations between inflationary and deflationary tilt were recorded leading up to episodes 51 and 52. The total deflationary tilt measured at UWD during episode 52 was 14.4 microradians.

The sulfur dioxide (SO2) emission rate from the summit is likely now varying within a typical range of 1,000 to 5,000 tonnes per day. Winds are currently from the east-northeast, between 11-14 mph, with potential gusts as high as 20 mph. Degassing plumes from the new crack, north and south vents are currently being blown to the west-southwest. 

 

Rift Zone Observations:

Rates of seismicity and ground deformation remain low in the East Rift Zone and Southwest Rift Zone. SO2 emissions from the East Rift Zone remain below the detection limit.

 

Analysis:

The abrupt switch from summit deflation to inflation at the end of episode 52 along with glow from the vents indicates that episode 53 fountaining is likely. Inflationary tilt was interrupted by deflation from August 2 to 3. A second deflationary step began at 6:00 a.m. HST Friday morning and is continuing at this time.  Deflations prior to the start of episodes 51 and 52 lasted for roughly 2-3 days. If this deflation follows this trend, it would last until Sunday or Monday with the onset of episode 53 following in 1-2 days or between Monday and Wednesday of the coming week. This fits with current tilt-based models that have the forecast window for start of episode 53 fountains between Monday August 10 and Thursday August 13. Adjustments to the forecast may be necessary if the tilt pattern changes significantly.

Kīlauea has been erupting episodically since December 23, 2024, from two vents (north and south) in Halema‘uma‘u. Lava fountaining episodes, which generally last for less than 12 hours, are separated by pauses that can be longer than three weeks.

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

 

Summary of episode 52:

A detailed account of episode 52 is given in the HVO Status Report issued on July 29: https://volcanoes.usgs.gov/hans-public/notice/DOI-USGS-HVO-2026-07-29T13:10:51+00:00

  • Episode 52 of the ongoing Halemaʻumaʻu eruption began around 7:10 p.m. HST on July 28 and ended abruptly at 2:36 a.m. HST on July 29, 2026.
  • The maximum lava fountain height was approximately 500 feet (150 meters) above ground level from the north vent. The south vent never fountained during this episode but did emit flames at the end of the eruption. 
  • The maximum plume height was approximately 19,000 (5,800 meters) above mean sea level. 
  • Tephra fall was restricted mostly to the closed area of Hawaiʻi Volcanoes National Park to the southwest of the active Halemaʻumaʻu vents.  

     

Resources:

NOTE: HVO’s monitoring network is mostly recovered from recent power- and storm-related outages. Several summit stations, including the SDH tiltmeter, will remain offline until we are able to re-establish access across the deep tephra field southwest of the caldera.

The following links provide more information about the current eruption that began on December 23, 2024:

 

Hazards:

This episodic eruption is occurring within a closed area of Hawai'i Volcanoes National Park.

  • Volcanic Gas: high levels of volcanic gas—primarily water vapor (H2O), carbon dioxide (CO2), and sulfur dioxide (SO2)—are continually released during an eruption. Emissions can remain locally hazardous in the areas immediately downwind of the vents, even when the vents are not actively erupting. SO2 reacts in the atmosphere to create vog (volcanic air pollution) downwind. SO2 and vog may cause respiratory and other problems at high concentrations. Further information on vog can be found at https://vog.ivhhn.org/
  • Tephra: small glassy volcanic fragments—volcanic ash, pumice, scoria, Pele’s hair and reticulite—are created by the lava fountains. A combination of fountaining dynamics and wind conditions determines where tephra fall may occur for any given eruption episode. Larger particles fall near the vents while light particles may be wafted greater distances. These particles may be remobilized during windy conditions following recent eruptive episodes. Residents and visitors should minimize exposure to these fragments, which can cause skin, eye, and respiratory irritation. More information and guidance on tephra fall hazards is available at https://seagrant.soest.hawaii.edu/resource-and-guidance-for-volcanic-tephra-fall/
  • Lava flows: lava on the floor of Halemaʻumaʻu crater and the southwest side of Kaluapele, Kīlauea's summit caldera, remains hot and may slowly move in the days immediately following an eruptive episode.

Other significant hazards exist around Kīlauea caldera from Halemaʻumaʻu crater wall instability, ground cracking, and rockfalls that can be enhanced by earthquakes. Close to the eruptive vents, the tephra material on the crater rim is prone to cracking, slumping, and small landslides that sometimes expose hot and molten material within. 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.



More Information:



The Hawaiian Volcano Observatory is one of five volcano observatories within the U.S. Geological Survey and is responsible for monitoring volcanoes and earthquakes in Hawaiʻi and American Samoa.



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