USGS Volcano Notice - DOI-USGS-HVO-2025-01-10T20:11:29+00:00

SUMMARY  

The eruption that began within Halemaʻumaʻu at the summit of Kīlauea volcano on December 23, 2024, remains paused. Monitoring data show that Kīlauea summit is slowly inflating, indicating that new magma is accumulating below the surface of the summit region.  An overflight this morning, Friday, January 10, confirmed that lava is visible within both vents. This statement reviews recent observations and summarizes what could be expected next at Kīlauea.  

EPISODIC ERUPTIONS

The recent eruption of Kīlauea within Halemaʻumaʻu brought back an eruptive style not seen for many years. The eruption included 3 episodes of lava fountaining separated by pauses in eruptive activity. The third pause is ongoing, and USGS Hawaiian Volcano Observatory (HVO) scientists are reviewing patterns of past eruptions and current monitoring data to forecast what could happen next at Kīlauea.  

Episodes are marked by the onset of lava fountains and rapid deflation of the source magma chamber. Pauses between fountain episodes are usually accompanied by reinflation of the summit. A new episode begins when the system builds up enough pressure to force magma to the surface again. Fountaining is driven by rapid volume expansion of gas in fresh lava but is commonly preceded by periods of eruption of sluggish degassed flows. Dense degassed material is pushed out of the vent like a cork from a champagne bottle, allowing gas-rich magma to rise rapidly and fountain. 

Episodic eruptions have occurred before on Kīlauea at the start of the 1983 Puʻuʻōʻō and the 1969 Maunaulu eruptions (44 and 12 episodes each) on the middle East Rift Zone, and during the 1959 Kīlauea Iki summit eruption (17 episodes).  While the recent Kīlauea summit eruption is currently paused, persistent night glow from the vent and continued strong degassing indicate molten magma is probably within 150–300 feet (50–100 meters) of the surface within the vent.  

The main feature of episodic eruptions is their repeatability, which allows patterns to be identified. Inflation following episodes 1 and 2 of the recent eruption at the summit of Kīlauea resulted in 6 microradians of ground tilt a tiltmeter north of the caldera, near Uēkahuna bluff, indicating the pressure increase required at that time for the eruption to resume.   

WHAT IS LIKELY TO HAPPEN NEXT

It is not possible to forecast an exact outcome of this activity but we are in a window where it is likely another fountaining episode may occur.  

Sufficient pressure could push magma up to the surface to start another eruptive episode at Kīlauea summit. Following episode 3, Kīlauea has inflated and the 6 microradian level was reached about 4:30 p.m. HST Wednesday, January 8 afternoon (5 days after episode 3 paused on Friday, January 3 at 8:40 p.m. HST). That amount of inflation had been the minimum amount of pressure required previously for this eruption to restart.  However, the large deflation that accompanied the prolonged fountaining of episode 3 suggests the system might need more inflation as recorded on tiltmeters to reach the pressure necessary for eruptive activity to resume. 

HVO scientists on a monitoring overflight of Kīlaeua summit the morning of January 10 observed active lava within both vents that erupted recently in Halemʻamaʻu. The longer the vent sits without eruption on the surface, the more time molten material within the vent has to cool and it could reach a point that the eruption can’t restart. Assuming the vent remains open, indicated by continued glow and degassing, and inflation rate remains constant, it seems likely that a new episode could begin sometime between January 8 and January 13, when ground tilt at the Uēkahuna tiltmeter is expected to reach 12 microradians, about double prior post-fountain tilt increases. 

Defining windows of time where there is a higher probability or likelihood of an eruption restart differs from more precise forecasts of eruptive activity that require a more specific time for an event to occur. While we know that magma is near the surface, we do not know the exact amount of degassed magma in the vent that is temporarily capping the fresh, gas-rich magma below.  The rate of re-pressurization continues to vary as reflected by the changing rate of tilt recorded at Kīlauea's summit making it difficult to know when enough pressure has accumulated to start forcing degassed magma out of the vent and starting a new episode.  

SUMMARY OF RECENT ERUPTIVE ACTIVITY  

Tiltmeters and GPS stations showed that the Kīlauea summit region was inflating following the September 15–20, 2024, middle East Rift Zone eruption in and near Nāpau Crater. Inflation rates indicated that a summit eruption or intrusive event could be possible by the end of 2024.  At 2:20 a.m. HST on December 23, vents opened in the southwest part of Kaluapele within Hawaiʻi Volcanoes National Park, following approximately a half an hour of elevated earthquake activity. Lava fountains rapidly reaching heights up to nearly 300 feet (91 meters) and fed lava flows that covered the floor of Halemaʻumaʻu crater. Tephra (lava that travels through the air) and Pele’s Hair were deposited downwind of the erupting vents, on a closed portion of Crater Rim Drive. Sulfur dioxide (SO₂) emission rates reached up to 140,000 tonnes/day and these elevated volcanic gas emissions were transported downwind, contributing to vog.  

Three episodes of eruption have occurred since then, separated by pauses during which little or no lava effusion has occurred:  

• 2:20 a.m. HST to 4:00 p.m. HST December 23, 2024 (14 hours 20 minutes of lava eruption) 
• 8 a.m. HST December 24 to 11 a.m. HST December 25, 2024 (15 hours of lava eruption) 
• 8 a.m. HST December 26, 2024 – 8:30 p.m. HST January 3, 2025 (8 and a half days of lava eruption) 

Prior to each episode of eruption, Kīlauea summit tiltmeters showed increasing rates of inflation as pressure accumulated in the magma chambers beneath the surface. With each eruptive episode onset, Kīlauea summit tiltmeters switched to deflationary tilt as that pressure beneath the surface was relieved by lava erupted on the surface. Inflationary tilt returned after each eruptive episode ended, indicating that pressure was again building in the magma chambers beneath Kīlauea summit. In total, the UWD tiltmeter located near Uēkahuna bluff in Hawaiʻi Volcanoes National Park recorded nearly 28 microradians of deflation associated with all three eruptive episodes. 

Summit eruptions observed over the past 60 years have exhibited vigorous activity in the opening days which can episodically wax and wane, or drop over time to sustainable low effusion rates, or slowly diminish and end. 

Recent unrest has been restricted to Kīlauea’s summit region within Hawai’i Volcanoes National Park; earthquake activity remains low at the summit and no unusual activity has been noted in the East Rift Zone or in the Southwest Rift Zone at this time.  

A map showing eruptive activity at Kīlauea over the timeframe of December 23, 2024, to January 2, 2025, is available here: https://www.usgs.gov/maps/january-2-2025-kilauea-summit-eruption-reference-map.  

WHAT WE ARE DOING         

Kīlauea’s summit region is monitored with a dense network of instruments recording seismic activity, ground deformation, and volcanic gas emissions. 

• Several webcameras also provide views of this area within Hawai‘i Volcanoes National Park: https://www.usgs.gov/volcanoes/kilauea/summit-webcams  
• HVO staff reoriented the V1 cam to better view the December 23, 2024–January 3, 2025, eruptive vents: https://www.youtube.com/usgs/live  
• HVO staff deployed a new webcam to monitor the eruptive vents in the west part of Kaluapele: https://www.usgs.gov/observatories/hvo/s2cam-halemaumau-crater-summit-kilauea  
• HVO staff conduct aerial overflights of Kīlauea summit during eruptions to monitor eruptive activity and assess hazards.   
• HVO staff conduct measurements of SO₂ emission rate as often as possible. In trade wind conditions, this is generally daily, but during Kona wind conditions, measurements are often impossible. Accordingly, we have been unable to precisely constrain the SO₂ emission rate associated with the current pause. Other datastreams (e.g., webcams, seismicity) indicate that elevated degassing is ongoing, though diminished relative to during lava fountaining. 
• A webpage summarizing recent eruptive activity is available here: https://www.usgs.gov/volcanoes/kilauea/science/eruption-information  

HVO is in frequent communication with Hawai‘i Volcanoes National Park and Hawai‘i County Civil Defense to keep them apprised of Kīlauea activity.  

HVO continues to closely monitor Kīlauea, watching for any signs of unrest that may precede a new eruption. Should volcanic activity change significantly, a Volcanic Activity Notice will be issued.  

CONTINUING HAZARDS 

Recent eruptive activity occurred within a closed area of Hawai'i Volcanoes National Park, which means that lava flows were not a hazard to infrastructure or the public. High levels of volcanic gas were, and continue to be, the primary hazard of concern, as there can be far-reaching effects down-wind. Currently, elevated levels of degassing continue despite the pause in eruptive activity. Sulfur dioxide (SO₂) in particular reacts in the atmosphere to create the visible haze known as vog (volcanic smog) downwind of Kīlauea. Vog and SO₂ are respiratory irritants, and even at low levels may affect sensitive individuals. 

Different areas may be affected by vog depending on the local winds. During trade wind conditions, in which winds come from the northeast, SO₂ and other emissions are carried southwest, downwind of Hawaiʻi Volcanoes National Park. They wrap around the southern part of the Island of Hawaiʻi, along the Kona coast, where they can be trapped by daytime onshore and nighttime offshore sea breezes. During Kona wind conditions, in which winds come from the south, volcanic gas emissions can become concentrated on the eastern side of the Island of Hawaiʻi. During episodes with very high SO₂ emission rates, vog can be far-reaching and may affect the entire state and beyond. 

Additional information about, including forecasts and effects on health, can be found at the resources below: 

• https://vog.ivhhn.org/  
• http://weather.hawaii.edu/vmap/new/  
• https://pubs.usgs.gov/fs/2017/3017/fs20173017.pdf  
• https://vog.ivhhn.org/vog-fact-sheets