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| The first Bon Dance since COVID began will be held this Saturday, Sept. 16 at Pāhala Hongwanji, with outdoor dancing in the round, following a 4 p.m. service. Photo by Ron Johnson |
THIS ISLAND'S LAST BON DANCE OF THE SEASON WILL BE SATURDAY AT PĀHALA
HONGWANJI. The dancing around the tower will begin in the early evening, following a 4 p.m. Obon service. It celebrates the end of the harvest and honors ancestors with the presentation of fresh vegetables, fruits and other foods on the temple altar. The venue for the service is Pāhala Hongwanji temple. The dancing will be outside.
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| Myra Sumida will perform with Pāhala Taiko on Saturday at Bon Dance at Pāhala Hongwanji. Photo by Julia Neal |
The tradition is mostly lost in Japan but remains alive in the Hawaiian Islands, brought here generations ago by immigrants working in the sugar plantations. Some people from Japan come to Pāhala to see the bon dance each year.
Also to enjoy are traditional Japanese foods, including sushi. Participants are invited to make Hachimaki, stamping Japanese characters onto the cloth headbands to be worn by everyone during the celebration. There will be a performance by Pāhala Taiko drumming.
Pāhala Hongwaji President Wayne Kawachi said that everyone with or without traditional kimono, Happi Coats and other Japanese clothing is invited to circle the tower and to learn the dances, accompanied by singing, flutes, drums and other music. Bon dancers who go from Buddhist temple to temple around the island will come to Pāhala on Saturday.
Also scheduled are aikido demonstrations.
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| Aikido demonstrations will be part of the Bon Dance celebration at Pāhala Hongwanji on Saturday evening. Photo by Julia Neal |
Soto Michi Dojo will be open in the old Japanese schoolhouse on the temple grounds with short aikido demos between 6:30 p.m. and 8 p.m., and sensei will be available to talk story about aikido and classes. Dojo members have also volunteered to clean the grounds and direct parking for the event.
This is the first Bon Dance at Pāhala since the Covid pandemic began. The address is 96-1123 Pa‘au‘au Place, Pāhala.
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GOV. JOSH GREEN WILL BE AMONG WORLD LEADERS SPEAKING AT THE UNITED NATIONS, says a statement from his office. The statement released Friday says Gov. Josh Green will go to New York and the UN on Saturday and "will be among other world leaders, including the heads of state of Spain, Turkey, Egypt, Ghana, São Tomé and Principe, and mayors from The Gambia and Colombia."
The event is the United Nations Sustainable Development Goals Summit in New York. Also in attendance, says Green's statement, will be Hawai‘i County Mayor Mitch Roth.
The statement says that during this trip to the East Coast, Green "will be giving an address to the UN on Sunday, Sept. 17, about Hawai‘i's efforts to implement policies to achieve the UN's Sustainable Development Goals and the importance of local leadership to achieve the SDGs by 2030." Green and Hawai‘i contingent are scheduled to present from 6:05 a.m. to 6:25 a.m. Hawai‘i Time on Sunday. Video will be available via livestream on UN Web TV at https://media.un.org/en/asset/k1x/k1x8on96di.
The Governor's statement says the Sustainable Development Goals "seek to address the root causes of poverty and the universal need for sustainable development that works for all people, including issues like protecting the planet and ensuring that all people have opportunities to enjoy health, justice, and prosperity." See more on UN Sustainable Development Goals at https://sdgs.un.org/goals.
Green also will participate in a second event entitled American Leaders Advancing the SDGs at 2 a.m. HST on Sept. 18. This will be a fireside chat moderated by Tony Pipa from Brookings Institute. The panel will include Green, Hawaiʻi Green Growth CEO Celeste Connors, and Kamehameha Schools students, says the statement from the Governor.
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Activity Summary: The Kīlauea summit eruption that began on September 10th continues Friday morning. Eruptive activity is confined to the downdropped block and Halemaʻumaʻu crater within Kīlauea’s summit caldera. No unusual activity has been noted along Kīlauea’s East Rift Zone or Southwest Rift Zone.
Summit Eruption Observations: Several roughly east-west oriented vents continue to erupt on the western side of the down-dropped block within Kīlauea’s summit caldera and are generating lava flows
onto Halema‘uma‘u crater floor. Effusion rates continue to decrease, but remain significant.
Summit Eruption Observations: Several roughly east-west oriented vents continue to erupt on the western side of the down-dropped block within Kīlauea’s summit caldera and are generating lava flows
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| A row of scones in Halema‘uma‘u are actively ejecting spatter, which helps build the height of each structure. Cone heights of 20 meters (66 feet) have been measured by field teams. Of the line of vents spanning 0.8 miles (1.4 km) that were observed active during the initial phases of the eruption, only six remain active as of September 14, 2023. USGS photo by L. Gallant |
onto Halema‘uma‘u crater floor. Effusion rates continue to decrease, but remain significant.
- Vigorous spattering is restricted to the westernmost large spatter cone with fountains 10-15 meters. Minor spattering is occurring within the next cone to the east, but the fountains remain mostly below the rim of its cone. Lava continues to flow from these and potentially several of the other cones.
- Pāhoehoe lava flows continue to travel in north and west directions from the vents, around elevated ground from the 1982 eruption, and onto Halema‘uma‘u crater floor. Overnight on Thursday, webcam imagery shows that the area of active lava remains restricted to the western part of the downdropped block and the northeastern parts of Halema‘uma‘u. This area of active lava does not appear to have changed significantly in size over the past 24 hours. Numerous oozeouts of lava were visible over other parts of Halema‘uma‘u crater floor overnight.
- Field crews Thursday reported that lava fountain heights at the vents reached up to about 10-15 meters (32-50 feet) and the horseshoe-shaped spatter ramparts that have accumulated on the south/downwind side of the vents remain 20 meters (66 feet) high.
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| Much of the plume from Kīlauea’s current eruption is sulfur dioxide (SO2). HVO’s gas monitoring station HRSDH has measured up to 12 ppm of SO2 at its location, nearly 2 miles (3 km) southwest, downwind of the eruption. According to the International Volcanic Health Hazard Network (IVHHN), prolonged exposure to SO2 in these concentrations is toxic. Even brief exposure to concentrations less than that will cause a respiratory response (airway resistance) and eye irritation. Concentrations more than that cause paralysis or death with extended exposure. SO2 mixes with air as it moves away from the vent and is less of a hazard for people keeping a safe distance. While the trade winds transport plumes in a southwest direction most of the time, conditions can change rapidly, especially in areas closer to the vent that remain closed to the public. USGS photo by M. Patrick |
- The laser rangefinder is aimed at a western portion of Halema‘uma‘u, not near the new eruptive activity, and recorded about 10 meters (33 feet) of uplift to this locality since the eruption started. This demonstrates that a significant amount of lava has intruded beneath the pre-existing crust within Halema‘uma‘u.
- Volcanic gas emissions in the eruption area are elevated; winds yesterday, September 14, prevented measurements of a suflur dioxide (SO2) emission rate. The most recent SO2 emission rate of 20,000 tonnes per day was measured the afternoon of September 13. This is down significantly from the 190,000 tonnes per day measured just after the onset of the eruption on Sunday, September 10th.
- A live-stream video of the eruption is available (here).
- More eruption information is available (here).
Rift Zone Observations: No unusual activity has been noted along the East Rift Zone or Southwest
Rift Zone; steady rates of ground deformation and seismicity continue along both. Measurements from continuous gas monitoring stations downwind of Puʻuʻōʻō in the middle East Rift Zone—the site of 1983–2018 eruptive activity—remain below detection limits for SO2, indicating that SO2 emissions from Puʻuʻōʻō are negligible.
Hazard Analysis: Eruptive activity is occurring on the down-dropped block and Halemaʻumaʻu crater, within Kīlauea’s summit caldera and in the closed area of Hawaiʻi Volcanoes National Park. During Kīlauea summit eruptions, the high level of volcanic gases—primarily water vapor (H2O), carbon dioxide (CO2), and sulfur dioxide (SO2)— and fine volcanic particles are the primary hazards of concern, as these hazards can have far-reaching effects downwind.
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| View from the ground of one of the vents erupting in Kīlauea caldera on September 14, 2023. The lava fountain heights at the vents reached up to about 10-15 meters (32-50 feet) and the horseshoe-shaped spatter ramparts that have accumulated on the south/downwind side of the vents are 20 meters (66 feet) high. USGS photo by D. Downs |
As SO2 is released from the summit, it reacts in the atmosphere to create the visible haze known as vog (volcanic smog) that has been observed downwind of Kīlauea. Vog creates the potential for airborne health hazards to residents and visitors, damages agricultural crops and other plants, and affects livestock. For more information on gas hazards at the summit of Kīlauea, please see (this link). Vog information can be found (here).
Strong winds may waft fine rock particles to areas downwind of erupting vents. People should minimize their exposure to these fine volcanic particles, which can cause skin and eye irritation. Reports from Hawaiian Volcano Observatory field crews indicate that fine particles of Pele’s Hair and other tephra are being deposited in the area near the Keanakāko‘i Overlook, which is approximately half a mile (about 1 km) from the eruption site. Hawaiʻi Volcanoes National Park has closed the Keanakāko‘i Overlook to the public at this time.
Other significant hazards also remain around Kīlauea’s summit 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 the rim surrounding Halemaʻumaʻu crater, an area that has been closed to the public since early 2008.
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Strong winds may waft fine rock particles to areas downwind of erupting vents. People should minimize their exposure to these fine volcanic particles, which can cause skin and eye irritation. Reports from Hawaiian Volcano Observatory field crews indicate that fine particles of Pele’s Hair and other tephra are being deposited in the area near the Keanakāko‘i Overlook, which is approximately half a mile (about 1 km) from the eruption site. Hawaiʻi Volcanoes National Park has closed the Keanakāko‘i Overlook to the public at this time.
Other significant hazards also remain around Kīlauea’s summit 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 the rim surrounding Halemaʻumaʻu crater, an area that has been closed to the public since early 2008.
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