Overflows of the upper fissure 8 lava channel this morning sent small flows of lava down the levee walls. These overflows did not extend far from the channel, so they posed no immediate threat to nearby areas. Channel overflows, like the ones shown here, add layers of lava to the channel levees, increasing their height and thickness. Photo taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
A closer view of the fissure 8 lava channel with the cinder quarry more clearly visible in the foreground (bottom of photo). During this morning’s overflight, HVO geologists observed no new breakouts of lava near this quarry. Photo taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
Fissure 8 continues to erupt vigorously, with lava streaming through a channel that reaches the ocean at Kapoho Bay. The width of the active part of the lava channel varies along its length, but ranges from about 100 to 300 meters (yards) wide. A clear view of the cinder-and-spatter cone that’s building around the vent from ongoing lava fountains can be seen here. Photo taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
Distant view of KÄ«lauea Volcano’s fissure 8 lava channel from HVO’s early morning overflight on June 10, looking to the southeast. Bryson’s cinder quarry is the brown patch just to the north of the channel. Photo taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
A closer aerial view of the lava delta forming at the Kapoho Bay ocean entry, where fissure 8 lava continued enter the ocean as of this morning. Laze (lava haze), an acidic white plume laced with tiny particles of volcanic glass, is produced by the ocean entry and creates an ongoing hazard that should be avoided. Photo taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
The fissure 8 lava flow reaches the ocean at Kapoho Bay, where a lava delta has formed and continues to grow as lava enters the sea. The largest white laze plume marks the main point where lava is entering the sea, but smaller active entry points persist along the entire leading margin of the flow. Photo taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
This image is from a temporary research camera positioned near Kapoho looking southwest. From left to right, one can see the eruptive fissures, with Fissure 15 on the far left, and Fissure 8 near the center. Webcam image taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
Another explosion occurred at Halema‘uma‘u at 12:51 a.m. HST today, releasing energy equivalent to a magnitude-5.3 earthquake. Following the explosion, summit activity consisted mostly of passive degassing at Halema‘uma‘u, similar to what is shown in this image taken mid-morning. Seismicity at the summit decreased after the explosion, but has been increasing throughout the day. Photo taken Sunday, June 10, 2018 courtesy of U.S. Geological Survey
A photogrammetry survey of KÄ«lauea’s summit by the U.S. Department of Interior Unmanned Aircraft Systems’ (UAS) KÄ«lauea response team show the topography of Halema‘uma‘u as of June 8. Cracks through the former overlook parking lot (bottom of image) wrap around the east margin of Halema‘uma‘u; the once-popular overlook viewing area (closed since 2008 due to volcanic hazards associated with the former summit lava lake) has collapsed into the crater. New faulting and slumping are obvious on the crater’s west side (left). The depth of the crater has increased by roughly 250 meters (820 feet) since early May. Limited UAS flights into the summit area are conducted with permission and in coordination with Hawai‘i Volcanoes National Park to collect quantitative and qualitative data needed for updated hazard assessments, all of which are shared with emergency managers. Image courtesy of the U.S. Geological Survey and Office of Aviation Services, Department of the Interior, with support from the Hawaiian Volcano Observatory and Hawai‘i Volcanoes National Park.
Map as of 12:00 p.m. (noon) HST, June 10, 2018. Given the dynamic nature of KÄ«lauea’s lower East Rift Zone eruption, with changing vent locations, fissures starting and stopping, and varying rates of lava effusion, map details shown here are accurate as of the date/time noted. Shaded purple areas indicate lava flows erupted in 1840, 1955, 1960, and 2014-2015.
This thermal map shows the fissure system and lava flows as of 6:45 am on Sunday, June 10. The flow from Fissure 8 remains active, with the flow entering the ocean at Kapoho. The black and white area is the extent of the thermal map. Temperature in the thermal image is displayed as gray-scale values, with the brightest pixels indicating the hottest areas. The thermal map was constructed by stitching many overlapping oblique thermal images collected by a handheld thermal camera during a helicopter overflight of the flow field. The base is a copyrighted color satellite image (used with permission) provided by Digital Globe.
This is a Civil Defense Message for 6 p.m., Sunday, June 10, 2018.
Hawaiian Volcano Observatory reports that the eruption continues in the lower East Rift Zone. Fissure 8 continues to produce a large channelized flow entering the ocean at Kapoho. Volcanic gas emissions from fissure eruptions remain very high. The National Weather Service reports that trade winds are pushing volcanic emissions southwest though Pahala to Ocean View areas.
Due to the current volcanic activity, the following policies are in effect:
Government Beach Road, between Kahakai Boulevard and Cinder Road is open only to residents of Waa Waa and Papaya Farms Road with official credentials; there is no curfew.
Residents downwind, do reduce exposure to volcanic emissions by staying indoors and closing windows or leaving the immediate area. You can monitor sulfur dioxide and hydrogen sulfide on Hawaii Island by visiting the Civil Defense website.
Do heed warnings from Civil Defense officials and be prepared to evacuate with little notice.
The shelters at Pahoa Community Center and Keaau Armory are open and pet-friendly.
The Recovery Information and Assistance Center at the Pahoa Community Center is closed on Monday, June 11, in observance of King Kamehameha Day and will re-open Tuesday, June 12.
The Pahoa Post Office is open during normal business hours with temporary Sunday hours from 10 a.m. to 2 p.m. for mail and package distribution only for residents in the affected areas. No retail services on Sunday.
For your safety, heed warnings from Civil Defense officials and stay alert.
Due to the lava entry at the ocean, the following policies are in effect:
Access to the area is prohibited due to the laze hazard.
Stay away from any ocean plume since it can change direction without warning.
The U.S. Coast Guard is actively monitoring the ocean entry area and enforcing a 300-meter standoff zone. Only permitted tour boats are allowed in the area.
Health hazards of laze include lung, eye and skin irritation.
Be aware that the laze plume travels with the wind and can change direction without warning.
Get the latest Vog Predictions here: http://mkwc.ifa.hawaii.edu/vmap/
Sulfur Dioxide (SO2) and Vog
Click on image for full description of air quality levels.
Volcanic gas emissions remain elevated throughout the area downwind of the vents in lower Puna.
Severe conditions may exist such as choking and inability to breathe.
Sulfur Dioxide (SO2) gas from fissures are especially dangerous for elderly, children/babies and people with respiratory problems.
County, State, and Federal partners continue to monitor the situation. You will be informed of any conditions that affect your safety.
Monitor vog levels and forecasts: People on Hawaii Island outside the area of volcanic activity are also advised to monitor levels of vog at https://vog.ivhhn.org
The residents of Puna are going through a very difficult time. We ask for your help and understanding.
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