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Volcano Watch: Keeping up with Kilauea – West Hawaii Today

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Volcano Watch: Keeping up with Kilauea – West Hawaii Today


Kilauea began erupting from fissures southwest of Kaluapele (the summit caldera) just after midnight on June 3; the eruption ceased just nine hours later, though lava flows continued to slowly spread for several more hours. Prior to the brief eruption, the USGS Hawaiian Volcano Observatory (HVO) had been monitoring pulses of heightened seismic activity in the summit area for weeks.

How did these earthquakes give us insight into the features of the molten magma below and the eruption that was to come?

Earthquakes result from the breaking of cooler, brittle rock. As magma moves into an area, it forces the surrounding rock to bend and then break. This brittle rock “failure” is what seismologists at HVO see daily on live data streams as earthquakes. The locations of earthquakes can outline magma chambers, indicate fault movement, or show where magma is moving into new area. At Kilauea, earthquake swarms paired with changes in ground motion as seen on tiltmeters give HVO scientists an idea of the pressurization of magma chambers beneath the surface.

The proposed magma plumbing system at Kilauea is divided into three main chambers: the Halema‘uma‘u reservoir, the south caldera reservoir, and the Keanakako‘i reservoir. In the weeks leading up to Monday’s eruption, there were three distinct periods of heightened unrest. From April 27-May 3, May 6-9, and May 17-18, two distinct clusters of earthquakes occurred in the south caldera and the upper East Rift Zone (see box 3 in Figure 1).

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During these swarms, earthquake locations often switched between the south caldera cluster and the upper East Rift Zone cluster as magma pressure levels fluctuated within the different storage regions. The event counts at the south caldera cluster increase while the counts at the upper east rift cluster diminish as the system moved closer to eruption. Rates of ground tilt, measured by summit tiltmeters would also increase during the earthquake swarms, indicating an increased pulse of magma was accumulating beneath the surface.

Although the earthquakes occurred in distinct clusters, they could have happened in response to the stresses created by magma chambers located nearby. For this reason, there were several possibilities scenarios. First, magma accumulation could stop, and no eruption would occur. Magma accumulation could continue with an eruption in Kaluapele or magma could migrate to the southwest with either an intrusion (similar to last January) or eruption.

As we now know, magma did indeed migrate to the southwest and this time it erupted.

Just after noon on Sunday, June 2, earthquakes increased again beneath the south caldera region and intensified quickly, prompting HVO to raise the alert level and aviation color code for Kilauea at 5:30 p.m. HST.

For twelve hours, earthquakes of up to M4.1 shook the summit region until 12:30 a.m. Monday morning, when a fissure opened about 1 mile (2 km) southwest of the caldera. The eruption happened in the vicinity of ground cracks that formed in the late January intrusion.

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Past eruptions in this area — in 1971 and 1974 — have been brief, so it was no surprise when the fissure stopped erupting nine hours after the eruption began. Fortunately, the short-lived eruption occurred within a closed area of Hawai Volcanoes National Park; it did no damage to infrastructure. This was the first eruption in this area of Kilauea in 50 years, and the first eruption outside of Kaluapele since 2018. Only about 100 acres were covered with new lava, compared to over 500 during the September 2023 eruption within Kaluapele.

While lava has stopped moving on the surface of Kilauea, volcanic gas emissions remain elevated and activity beneath the surface remains dynamic. HVO scientists will continue to closely monitor for signs of change.

Volcano
activity updates

Kilauea is not erupting. Its USGS Volcano Alert level is ADVISORY.

Kilauea erupted briefly on Monday, June 3, southwest of Kaluapele (Kilauea caldera) within the closed area of Hawaii Volcanoes National Park. Tremor and incandescence associated with the fissure vents are still present but have decreased significantly since June 3. Sulfur dioxide emission rates remain elevated in the upper Southwest Rift Zone eruption area; an emission rate of 400 tonnes per day was measured today, June 6, for the combined areas of Kilauea summit and the recent eruption. Overall seismicity in the summit region including the eruption area remains low, although inflationary ground deformation of the summit continues. Additional pulses of seismicity and deformation could result in new eruptive episodes within the area or elsewhere on the Southwest Rift Zone.

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Mauna Loa is not erupting. Its USGS Volcano Alert Level is at NORMAL.

Webcams show no signs of activity on Mauna Loa. Summit seismicity has remained at low levels over the past month. Ground deformation indicates continuing slow inflation as magma replenishes the reservoir system following the 2022 eruption. SO2 emission rates are at background levels.

Nine earthquakes were reported felt in the Hawaiian Islands during the past week: a M3.5 earthquake 4 km (2 mi) S of Pahala at 30 km (18 mi) depth on June 5 at 4:18 a.m. HST, a M3.1 earthquake 3 km (1 mi) SSW of Pahala at 31 km (19 mi) depth on June 3 at 7:01 a.m. HST, a M4.1 earthquake 7 km (4 mi) SSW of Volcano at 0 km (0 mi) depth on June 2 at 9:12 p.m. HST, a M3.2 earthquake 7 km (4 mi) SW of Volcano at 1 km (1 mi) depth on June 2 at 7:38 p.m. HST, a M4.0 earthquake 7 km (4 mi) SSW of Volcano at 0 km (0 mi) depth on June 2 at 7:06 p.m. HST, a M3.1 earthquake 7 km (4 mi) SSW of Volcano at 0 km (0 mi) depth on June 2 at 6:15 p.m. HST, a M3.4 earthquake 7 km (4 mi) SW of Volcano at 1 km (1 mi) depth on June 2 at 5:15 p.m. HST, a M3.1 earthquake 8 km (4 mi) SW of Volcano at 1 km (0 mi) depth on June 2, 2024 at 4:58 p.m. HST, and a M3.4 earthquake 12 km (7 mi) S of Waikoloa at 35 km (22 mi) depth on June 1 at 7:16 p.m. HST.

HVO continues to closely monitor Kilauea and Mauna Loa.





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University of Hawaii study finds San Andreas Fault stress at 1,000-year high | Honolulu Star-Advertiser

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University of Hawaii study finds San Andreas Fault stress at 1,000-year high | Honolulu Star-Advertiser


LOS ANGELES >> Stress on the San Andreas Fault system has reached a 1,000-year high, according to new research from the University of Hawaii.

Higher stress on a fault means the pressure that causes earthquakes is building.

“Our results show that stress levels on multiple fault segments are now at or above the highest values seen in the past millennium and that the region may be capable of a large through-going rupture involving both fault systems,” said lead author Liliane Burkhard, research affiliate in the Hawai‘i Institute of Geophysics and Planetology at the UH-Manoa School of Ocean and Earth Science and Technology and a scientist at the University of Bern, Switzerland.

“We also found that Cajon Pass may act as an ‘earthquake gate:’ sometimes blocking large ruptures from crossing between the faults, and sometimes allowing them to pass through and involve both systems in a single event,” Burkhard said in a UH news release.

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Multi-fault ruptures, where earthquakes continue from one fault to another, have occurred in multiple recent earthquakes, including the 2011 Tohoku, Japan, earthquake and became a part of the U.S. Geological Survey’s earthquake forecasting model in 2015.

This type of quake would be possible if the Cajon Pass, which is between the San Bernardino and San Gabriel mountains in Southern California, allows an earthquake to pass through it, meaning rather than affecting the area along one fault line, a quake could continue along a second fault and affect a larger area.

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But Kate Scharer, a co-author of the study and a seismologist with the U.S. Geological Survey in Pasadena, said there’s no reason for California residents to be significantly more concerned than they were before hearing about the study.

While the stress has reached a milestone, the pressure was already high and the fault has been overdue for a large earthquake for some time, according to the study.

It has been over 100 years since a major tectonic rupture has affected the greater Los Angeles area, which means stress on the tectonic plates has been building, according to the study.

The 1857 Fort Tejon earthquake was the most recent “big one” to affect Southern California, while the San Jacinto Fault saw moderate earthquakes in 1918, 1968 and 1987, according to the study. A long period without seismic activity “raised concern that the next slip event in this region could be both large and complex,” the study says.

As more time passes, an earthquake becomes more likely because built-up energy needs to be released.

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“We know for the southern San Andreas and the San Jacinto fault that they were just a little bit over the average (time between earthquakes) from looking at the geologic record,” Scharer said.

Those two faults are at highest risk for an earthquake because they are the fastest moving, she said.

The study looked at a geologic record of earthquake activity across the past 1,000 years, giving a new perspective on the total stress the San Andreas and San Jacinto fault systems are under. Tectonic plates are always moving and accumulating stress, save for those few seconds where an earthquake is happening.

When an earthquake releases built-up stress from hundreds to thousands of years of an interseismic period, energy is felt in the form of an earthquake, Scharer said.

Earthquake forecast models from the U.S. Geological Survey are “a reminder that damaging earthquakes are inevitable for California,” and the new study highlights just how much stress the fault systems are under as Californians prepare for the “big one,” according to the USGS.

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The study’s importance is with the calculations of stress the researchers did. After a geologic record, which looks at prehistoric earthquakes and is assembled by digging trenches across faults and looking at layers that have been offset in the past, is created, the researchers were able to determine that the stress on the San Andreas fault is at a 1,000-year high.

The stress level could influence if the Cajon Pass facilitates an earthquake spreading from one fault to another, or if it stops an earthquake from doing so. When the stress levels on both faults are similar, both faults appear to rupture jointly, according to the study.

Using a physics-based computer model, the researchers found that that the stress that would normally be released in large earthquakes has continued to accumulate and is at unprecedented levels.

The Cajon Pass, the study suggests, could facilitate a joint rupture of both the San Andreas and San Jacinto faults simultaneously, which could be “significantly more damaging than a single-fault event,” affecting densely populated areas including Los Angeles, San Bernardino, Riverside and the Coachella Valley, according to the UH news release.

“This is not a prediction of when an earthquake will happen,” Burkhard said. “However, studies like this are important contributions to national and global earthquake hazard research in that we are using rigorous, quantitative science to better understand the risk facing millions of people. What we can say is that the system is critically stressed, and that physics-based models like this one give us a clearer picture of the range of scenarios we should be prepared for. That information matters for hazard assessments, infrastructure planning, and emergency preparedness.”

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Honolulu Star-Advertiser staff contributed to this report.




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Police recover 19 gaming machines, $7K in Kakaako gambling bust

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Police recover 19 gaming machines, K in Kakaako gambling bust


HONOLULU (HawaiiNewsNow) – The Honolulu Police Department shut down an illegal gambling operation in Kakaako.

On Thursday, officers with the Narcotics/Vice Gambling detail, along with the District 1 Crime Reduction Unit, Forfeiture Detail and Specialized Services Division, executed a search on a property on Kawaiahao Street.

HPD said they recovered 19 gaming machines and more than $7,000 in cash.

Police shut down the gambling operation in Kakaako Thursday.(Honolulu Police Department)

The department said they remain committed to addressing illegal gambling operations.

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“The June 25, 2026, operation is the 19th illegal gambling search warrant executed so far in 2026 and the third in the month of June,” said HPD Maj. Jerome Pacarro. “Enforcing the law against these illegal operations helps prevent related criminal activity from taking root and strengthens the safety of our communities.”

To report illegal gambling, call the Narcotics/Vice 24-hour hotline at (808) 723-3933 or use the online form here.

Copyright 2026 Hawaii News Now. All rights reserved.



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Hilo Pride parade and festival on Saturday – Hawaii Tribune-Herald

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Hilo Pride parade and festival on Saturday – Hawaii Tribune-Herald






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