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Additional Information on Today’s Puna Geothermal Trip

UPDATE: At 3 PM today Puna Geothermal reported a release of steam from one of its wells. The situation was contained and secured as of 3:45 PM. The Hawaii County Fire Department remains on scene and is continuously monitoring the air quality at the site, the perimeter, and the surrounding community.

Based on all available data, there is no threat to the public and no evacuation is necessary. Civil Defense is monitoring the situation and we will keep the public advised of any changes in the situation. If you have any questions, you may call 935-0031.
puna-geothermal-ventureAdditional information on today’s Puna Geothermal Steam Release:

• HFD HAZMAT reported at 3:10 PM today that initial readings from PGV monitors at the PGV facility were 15.7 PPB
• Since then, when HFD HAZMAT got on scene at 3:38 PM, arrived at front gate and got “0” readings there, they then proceeded up to the plant and continued monitoring. All readings were at “0” readings.
• HFD HAZMAT then proceeded to go around the outside perimeter of facility downwind, down Kapoho Rd to HInalo street, got all negative, or “0” readings, last reading was at 3:53 PM.
• Dispatch at 4:04 received 2 calls of people complaining of strong smell of sulfur near Hinalo street.
• At 4:10 PM HFD HAZMAT went back and checked, again, they got negative or 0 readings.
• HFD Engine Company on scene at 3:19 PM.
• Both HAZMAT and Engine Company remain on scene at this time.

Per PGV:
• Isolation of H2S occurred within 1 hour, isolation is complete at this time.
• The noise was loud, it was a release valve opening up. The level of sound was about 70 decibels at time of release.
• it is unknown what caused the trip, technicians are looking into it at this time.

Trouble at Puna Geothermal Plant

puna-geothermal-venture

From Hawaii County Civil Defense:

At 3:03 today PGV reports a possible partial trip offline for their power plant. Community calling in about a loud bang at the plant, asking for more information.

  • PGV troubleshooting, Civil Defense is waiting on more information from them at the plant.
  • A partial H2S release possible
  • majority of steam going into an abatement tank
  • perimeter air quality monitoring ongoing.
  • The trigger point for notification/action is 25 PPMillion. The trigger point for OSHA is 10 PPM. We are not at those levels at this time
  • Civil Defense is following protocols according to plan.
  • HFD HAZMAT is on scene

Though readings are not at the action/alert level, we would like to ask for your assistance with notifying as many people as possible just for information purposes. It would be better if through community associations as they may have phone trees already planned.

More information coming

New HVO Map Shows Location of New Lava Breakout

This map shows recent changes to Kīlauea’s East Rift Zone lava flow field.

hvo-map-91916The area of the active flow field as of September 1 is shown in pink, while widening and advancement of the active flow as mapped on September 12 is shown in red. Older Puʻu ʻŌʻō lava flows (1983–2016) are shown in gray.

Map of coastal flow field with thermal overlay

This map includes a georeferenced thermal image mosaic showing the distribution of active and recently active breakouts on the coastal flow field.

hvo-map-91916a The thermal mosaic was acquired during a helicopter overflight on September 12. The episode 61g flow field is outlined in yellow to show the extent of the flow.

THURSDAY: 6th Annual Kipimana Cup – Keaau vs. Kamehameha

The Keaau Cougars will host the 6th Annual Kipimana Cup challenging the Kamehameha Warriors Thursday, this time with a new head coach who happens to be a former coach for Kamehameha.

kipimana-cup
“We are excited to host the Kipimana Cup at our campus this year,” said Iris McGuire, Keaau High School’s athletic director. “We have a new coach and style of football at Keaau High School,” she noted, referring to Aurellio Abellera, who was the defense coach for the Warriors before opting to lead the Cougars.

Hosted by W.H. Shipman, Limited, which calls Keaau home, the Kipimana Cup is a goodwill football game between the public and private schools located within a few miles radius in Keaau.

“Every year it is encouraging to see the attitude of friendship tied to this particular competition,” said Bill Walter, president of W.H. Shipman, Limited. “Team leadership has been effective in instilling what we all hoped that attitude would be: we can play hard, we can compete to win a game and we can compete here in Keaau in a spirit of good will. Similarly, we encourage incoming businesses to recognize this as a special place to do business and to work together to create an environment where our customers want to come to do business.”

Dan Lyons, head football coach for the Kamehameha Schools Keaau campus, noted the Kipimana Cup is a way of “creating a competition” among the two schools and their athletes, “but also an acknowledgement of sportsmanship” that exists between the two schools. “I just think it’s a really good thing for the community, building community togetherness with both of us being in Keaau.”

He noted that W.H. Shipman, Limited is rooted in the history of both schools, with the land originally owned by the family owned company. As for Keaau’s new coach being one of his former staffers, Lyons thinks it’s “awesome.”

“’Leo’ is a really good guy and a really good catch,” Lyons said. Noting the Cougars have already won a couple of games, he said Abellera will bring “structure, organization, character, and integrity” to the Keaau team. “I mean, he’s a very good coach and great guy. It obviously leaves a void in our program, but it certainly helps Big Island football be better.”

“I coached with Dan for the last three years, and he helped me bring back the fun in coaching and football,” Abellera said. He has actually been a math teacher at Keaau High School for the last 16 years, and this is his second time coaching there. “My dad got sick and footballl didn’t seem fun anymore,” he said.

It was Lyons and the Kamehameha Warriors that got him back into coaching. With Kamehameha on solid ground, and the Cougars in need of help, Abellera returned to Keaau.

For the Kipimana Cup Thursday, Kamehameha will show up with four wins and one loss to Kealakehe, in their most recent game on Friday. Keaau, meanwhile, will face off with the Kamehameha Warriors with two wins and one loss, having defeated the Honokaa Dragons in their most recent game last week.

Thursday’s Kipimana Cup will be a league game for both teams. Kamehameha Schools and Keaau High School didn’t always play against each other, being in different divisions — Keaau being in Division 1 and Kamehameha being in Division 2.  The Big Island Interscholastic Federation League ultimately changed that, but not before W.H. Shipman, Ltd. first pitched the annual Kipimana Cup six years ago.

W.H. Shipman, Limited provides $500 to each of the school’s booster clubs following the game, and a trophy to the winning team.
The Kamehameha Warriors have won all five of the previous Kipimana Cups, but that may be a different story this year with Abellera leading the Keaau Cougars, Lyons acknowledged.

Kamehameha School’s Hawai‘i campus opened on former W.H. Shipman land in 2001 and has an enrollment of a little over 1,000 students, grades K-12, while Keaau High School has an enrollment of 880 children, grades 9-12.  The school first opened in 1998, also on Shipman property.

Kipimana is how Hawaiians historically referred to Shipman. W.H. Shipman, Limited staff came up with the idea for the Kipimana Cup six years ago.

Based in the Puna for the last 130 years, W.H. Shipman, Limited currently has 17,000 acres in and around Keaau, and is active in agriculture and commercial/ industrial development and leasing. Shipman holds a long-range view toward sustainability and planned development for balanced community use.

Thursday’s Kipimana Cup will be held at Keaau High School.  Kickoff for the varsity game is expected to start around 7:30 p.m., a half hour after the 5 p.m. junior varsity game ends. Expect to pay a nominal admission.

Contact Walter at 966-9325 for more details.

Police Investigating Possible Drowning in Puna

Hawaiʻi Island police are investigating a possible drowning that occurred in the Puna district.

pohoiki-boat-ramp

On Tuesday, (September 6), at 4:00 p.m., officers responded to a report of an unresponsive woman who had been snorkeling at Pohoiki Beach. Upon police arrival, Hawaiʻi Fire Department Rescue personnel and Hawaiʻi County Lifeguards were attempting cardio-pulmonary resuscitation. Attempts to resuscitate the victim at the scene were unsuccessful.

The identity of the victim is being withheld pending notification of her next of kin.

Police have initiated a coroner’s inquest investigation and have ordered an autopsy to determine the exact cause of death.

Avocado Thieves Caught Red Handed

Two men are being held on charges after being arrested for allegedly stealing avocados from an orchard in Puna.

In response to a 4:45 p.m. call Wednesday, Puna District officers learned that the owner of an orchard off Highway 132 in the Kapoho area had confronted two men and a woman in a pickup truck on his property after observing 80 pounds of avocados in the bed of the truck. The owner and a friend had blocked the truck and called the police.

Max Mattos

Max Mattos

The two men, 49-year-old Max Mattos of Keaʻau and 33-year-old Kawika Nobriga of Pāhoa, were arrested and charged with second-degree criminal trespass and second-degree theft. Their bail was set at $2,500 each.

Kawika Nobriga

Kawika Nobriga

The woman, 30-year-old Sabrina Jaeger of Pāhoa, was arrested on a bench warrant and charged with contempt of court. She was released after posting $300 bail.
Sabrina Jaeger
Mattos and Nobriga are being held at the Hilo police cellblock pending their initial court appearance scheduled for Thursday (August 25).

Aerial Video of Kīlauea Volcano’s Summit Lava Lake

This aerial video footage, filmed by USGS in late July 2016, features Kīlauea Volcano’s summit vent within Halemaʻumaʻu Crater.

lava lake 817

Hawaiʻi Volcanoes National Park’s Jaggar Museum, and the adjacent USGS Hawaiian Volcano Observatory, are perched on the rim of Kīlauea’s summit caldera (foreground of opening footage) just over a mile from the crater, offering spectacular viewing opportunities for Park visitors. Closer to Halemaʻumaʻu, black lava flows on both sides of the summit vent are clearly visible; these flows spilled onto the crater floor when the lava lake overflowed the vent rim in April–May 2015.

At the time this footage was captured, the lava lake level was 22–26 m (72–85 ft) below the vent rim; this morning, it was about 32 m (105 ft) below the vent rim. The summit vent, initially 35 m (115 ft) wide when it first opened in March 2008, has since been enlarged by numerous vent rim collapses and is now about 180 by 250 meters (590 by 820 feet) across.

New Lava Flow Map Shows Vicinity of Ocean Entries

This map shows recent changes to Kīlauea’s East Rift Zone lava flow field at the coast. The area of the active flow field as of August 2 is shown in pink, while widening and advancement of the active flow as mapped on August 12 is shown in red.

hvo map 81316

The base is a Digital Globe image from January 2016.

Police Investigating Human Remains and Missing Person Case – Jessica Urbina

Hawaiʻi Island police have initiated a coroner’s inquest case in connection with human remains found in Puna last month and a missing person case for a Canadian woman whose personal items were found nearby.

Jessica Urbina

Jessica Urbina

On July 18, Puna Patrol officers responded to a remote area of the Hawaiian Paradise Park subdivision for a report of partial human skeletal remains found by local hunters off Beach Road about half a mile on the Pāhoa side of Makuʻu Drive.

After the officers located those remains, detectives from the Area I Criminal Investigations Section responded and recovered them, as well as personal items in the area belonging to a Canadian woman named Jessica Urbina.

Investigation revealed that Urbina, from Montreal, Quebec, had come to Hawaiʻi on vacation in November 2000, when she was 21 years old, and that she had been reported missing to the Honolulu Police Department in 2001.

In addition to the coroner’s inquest investigation, Hawaiʻi Island police have initiated a missing person case for Urbina, who was 21 when she was last seen. She was described as 5-foot-1, 100 pounds with long black hair, brown eyes and fair skin.

Police have not yet identified the remains and do not know if there is a link between the remains and Jessica Urbina, who would be 37 years old now.

Police ask anyone who has any information about the human remains or Jessica Urbina to contact Lieutenant Gregory Esteban at 961-2252 or gregory.esteban@hawaiicounty.gov.

Tipsters who prefer to remain anonymous may call the islandwide Crime Stoppers number at 961-8300.

*EDITORS NOTE*

I guess this explains this:

“Hello Mr Tucker,

I’m a reporter from Montreal, Quebec for Le Journal de Montreal. My colleague Frederique Giguere and I are working on the missing of Jessica Urbina, from Quebec, who’s missing in Hawaii since 2001. 

I see that Stephanie P******* said in 2012 on your website that she’s her cousin http://damontucker.com/missing/ I’m trying to reach Stephanie, to talk about Jessica Urbina. Is there any way you help me with that ? 

Do you have her email, by example? 

Thank you very much for your help.”

Urbina

Kamokuna Lava Ocean Entry Continues – Delta Forming

The Kamokuna ocean entry continues, and is approximately 250 m (820 ft) wide. Pāhoehoe activity on the coastal plain continues to widen the flow upslope of the emergency access road.

Click to enlarge

Click to enlarge

Photo comparison of the emergency access road from July 25, the day the lava first crossed (left), and today August 5 (right).

Click to enlarge

Click to enlarge

The flow is now approximately 200 m (650 ft) wide on the road and has inflated to a few meters tall (HVO geologist for scale).

USGS is warning about a Delta forming:

As the loose debris builds a foundation forward and upward, small lava flows spread atop the debris to form a lava delta above sea level that may extend tens to hundreds of meters beyond the old shoreline.

Sketch by J. Johnson, 2000

Sketch by J. Johnson, 2000

At the same time, the entire delta can slowly sink as the submarine debris pile shifts under the weight of the overlying lava flows; recent studies of several growing lava deltas showed that they subsided several centimeters per month. This new land is extremely unstable!

More on Deltas here:  http://hvo.wr.usgs.gov/hazards/oceanentry/deltacollapse/

New Map Released of Lava Flow

This map shows recent changes to Kīlauea’s East Rift Zone lava flow field. The area of the active flow field as of July 26 is shown in pink, while widening and advancement of the active flow as mapped on August 2 is shown in red. Lava reached the ocean on the morning of July 26. Older Puʻu ʻŌʻō lava flows (1983–2016) are shown in gray.

Click to enlarge

Click to enlarge

The blue lines over the Puʻu ʻŌʻō flow field are steepest-descent paths calculated from a 2013 digital elevation model (DEM), while the blue lines on the rest of the map are steepest-descent paths calculated from a 1983 DEM (for calculation details, see http://pubs.usgs.gov/of/2007/1264/). Steepest-descent path analysis is based on the assumption that the DEM perfectly represents the earth’s surface. DEMs, however, are not perfect, so the blue lines on this map can be used to infer only approximate flow paths. The base map is a partly transparent 1:24,000-scale USGS digital topographic map draped over the 1983 10-m digital elevation model (DEM).

Thermal Image of Lava Flow Shows Ocean Entry

This image shows a thermal map of the flow on the pali and coastal plain, created from airborne thermal images. White pixels are hot, and show areas of active surface breakouts. The background image is a satellite image collected before the current lava flow was active.

hvo 731 thermal

The thermal map shows scattered pāhoehoe breakouts on the coastal plain, with a narrow lobe of lava crossing the gravel road and extending to the ocean. The ocean entry has widened since it first formed on Tuesday, July 26, and now spans about 240 m (260 yards) of the coastline.

61G Lava Flow Continues to Stream Into Ocean

The 61g lava flow continues to stream into the ocean, with two entry points observed today: the original one, where lava first entered the ocean on July 26…

Lava Beachand a smaller one to the west.
lava beach 2
The ocean entries are adding lava to the rubble at the bottom of the sea cliff.

Click to enlarge

Click to enlarge

Black sand—formed by the interaction of hot lava and cool seawater, as well as by wave erosion of the rocky cliff—is also accumulating along the coastline.

A close-up view of the main ocean entry, showing the accumulation of lava and black sand at the base of the sea cliff.

Click to enlarge

Click to enlarge

Today, HVO’s geology field crew gathered data near the 61g lava flow vent on the eastern flank of Puʻu ʻŌʻō.

Click to see full screen

Click to see full screen

All You Can Eat Tacos, Chips & Salsa Fundraiser for Madie TOMORROW!

For the safety and concern of her community due to Tropical Storm Darby, 4th District County Council Candidate Madie Greene postponed her taco fundraiser that was going to be held last weekend and has moved it to TOMORROW!

A suggested donation of $15.00 is a steal when you can eat all-the-tacos you want provided by Luquins Restaurant.

Tacos with Madie

Aloha Friends and Community Members,

We cordially invite you to attend a Mahalo Event for Madie Greene this coming Saturday at the Akebono Theater, next to Luquins, 6 pm with awesome entertainment and taco buffet.

All are welcome, so please share with your friends and neighbors.

We hope to see you all there….

Friends of Madie Greene, Candidate for County Council District 4.

As Lava Meets the Ocean, New Dangers Persist

The 61G lava flow extending southeast of Puʻu ʻŌʻō towards the coastal plain on Kīlauea’s south flank remains active. The 61G lava flow extending southeast of Puʻu ʻŌʻō entered the ocean, as of as of 1:12 a.m. HST, last night. Areas of incandescence remain visible in overnight webcam views of the active lava flow field, marking lava tube skylights and areas of active lava on the pali and along the flow as it extends towards the coast.

Last night Senator Kahele walked out to the flow.

Last night Senator Kahele walked out to the flow.  That would make “Lava Meets Kai” a reality… LOL!

As a strong caution to visitors viewing the new ocean entry (location where lava meets the sea) for Flow 61G, there are additional significant hazards besides walking on uneven surfaces and around unstable, extremely steep sea cliffs. Venturing too close to an ocean entry exposes you to flying debris created by the explosive interaction between lava and water.

Also, the new land created is unstable because it is built on unconsolidated lava fragments and sand. This loose material can easily be eroded away by surf causing the new land to become unsupported and slide into the sea. Finally, the interaction of lava with the ocean creates an acidic plume laden with fine volcanic particles that can irritate the skin, eyes, and lungs.

Lava Flow Crosses Emergency Road and Flows Into Ocean

Flow 61G reached the emergency access road inside Hawai’i Volcanoes National Park on July 25 at 3:20 pm and crossed the road in about 30 minutes. At 4:00 pm, the flow front was approximately 110 m (0.07 miles) from the ocean.

hvo 726aThe active lava flow on Kīlauea Volcano’s south flank crossed the emergency access road in Hawaiʻi Volcanoes National Park this afternoon around 3:20 p.m., HST, providing wonderful lava-viewing experiences for Park visitors.

. A section of the road can be seen here, with fume from the active lava tube in the far distance behind it, and the active flow front in the foreground.

A section of the road can be seen here, with fume from the active lava tube in the far distance behind it, and the active flow front in the foreground.

The flow front continued to advance, and was less than 100 meters (yards) from the ocean a few hours later (when this photo was taken).

The lava flow reached the ocean about 01:15 a.m. on  July 26.

The lava flow reached the ocean about 01:15 a.m. on July 26.

Lava Now 0.2 Miles from Ocean

Activity Summary: Eruptive activity continues at Kīlauea Volcano’s summit and East Rift Zone. The 61G lava flow extending southeast of Puʻu ʻŌʻō towards the ocean remains active but poses no threat to nearby communities. As of yesterday, the flow tip was about ~370 m (0.2 miles) from the ocean. The lava lake at Halemaʻumaʻu Crater continues to circulate and intermittently spatter. Seismicity and deformation rates throughout the volcano remain at background levels.
hvo 725 g61
Summit Observations: The lava lake within the Halemaʻumaʻu Overlook crater remains active. The depth to the lake was estimated at 26 m (85 ft) below the crater rim, measured on Sunday. Tiltmeters at Kīlauea’s summit recorded a slight inflationary tilt. Seismicity is within normal, background rates with tremor fluctuations associated with lava lake spattering. The summit sulfur dioxide emission rate ranged from 3,700 to 7,300 metric tons/day.

Puʻu ʻŌʻō Observations: Webcam images over the past 24 hours show persistent glow at long-term sources within the crater. There were no significant changes in seismicity over the past 24 hours. The tilt still recovering due to heavy rainfall over the weekend. The sulfur dioxide emission rate from all East Rift Zone vents on July 22 was about 500 metric tons/day.

Lava Flow Observations: The 61G lava flow extending southeast of Puʻu ʻŌʻō towards the coastal plain on Kīlauea’s south flank remains active. On Sunday, the flow tip was active and breakouts were active within a few hundred meters (yards) upslope. The flow was approximately ~240 m (0.15 miles) from the coastal emergency road and 370 m (0.2 miles) from the ocean; based on National Park personnel observations. Areas of incandescence remain visible in overnight webcam views of the active lava flow field, marking lava tube skylights and areas of active lava on the pali and along the flow as it extends towards the coast.

Hawaii Electric Light Restores Power to 900 Customers After Tropical Storm Darby

Overnight, Hawaii Electric Light restored electric service to 900 customers in various parts of Hamakua, upper Puna, and Kona that were impacted by high winds from Tropical Storm Darby. About 100 customers in Hawaiian Paradise Park, Leilani Estates, Kapoho, Orchidland Estates, Honokaa, and Kailua-Kona remain without power.

 Hawaii Electric Light crews work to restore electric service in Hawaiian Paradise Park.


Hawaii Electric Light crews work to restore electric service in Hawaiian Paradise Park.

Crews worked through the night to repair damage to utility poles and power lines that was caused primarily by fallen trees, tree branches, and tree bark contacting power lines.

“Many of our employees have been working around the clock since Friday to prepare for the storm and to then safely restore electric service as quickly as possible,” said Rhea Lee-Moku, public information officer. “We know how difficult it is to be without electricity for a long period of time, and we thank our customers for their patience and understanding.”

Hawaii Electric Light expects to restore service to the remaining 100 customers tonight. However, it cautions that although the eye of the storm has passed over Hawaii Island, the weather forecast reports thunderstorms and heavy rain approaching the east side of the island. Lightning and moisture-soaked trees can make work conditions unsafe for crews. This may delay restoration efforts in areas impacted by the thunderstorms. Crews will continue to work to restore power to customers unless weather conditions become hazardous and unsafe.

The company also reminds the community that high winds and heavy rains may have partially-uprooted trees and cracked tree branches that can easily topple or break. Do not approach or touch a downed line as it can be energized and dangerous.

To report an outage, a low-hanging or downed power line, please call 969-6666. Hawaii Electric Light continues to proactively post outage notifications, including power restoration updates, on its Twitter account @HIElectricLight with the hashtag #BigIslandOutage.

New Thermal Image Map Shows Where Lava is Active

This image shows a thermal map of the flow on the pali and coastal plain, created from airborne thermal images. White pixels are hot, and show areas of active surface breakouts. The background image is a satellite image collected before the current lava flow was active.

Click to enlarge

Click to enlarge

The thermal map shows minimal activity on the upper pali, with a channelized ʻaʻā flow at the base of the pali. The flow front area had scattered pāhoehoe breakouts, with a narrow lobe of active lava forming the leading tip of the flow. The leading tip of the flow was 730 m (0.45 miles) from the ocean.

Sluggish Lava Breakouts Advance Slowly on Coastal Plain

The flow front remains active and consists of slowly advancing pāhoehoe. There are scattered breakouts along the margins of the flow on the coastal plain and base of the pali.

hvo 723a

During the overflight yesterday, the flow front was 730 m (0.45 miles) from the ocean.

A faint double rainbow provided a beautiful backdrop for sluggish pāhoehoe lava oozing out from near the flow front this morning.  Pictures were taken as part of a site visit to the G61 flow front on July 22, 2016.   The flow was about 615m from the road and 760 m from the ocean. (Click to enlarge)

A faint double rainbow provided a beautiful backdrop for sluggish pāhoehoe lava oozing out from near the flow front this morning. Pictures were taken as part of a site visit to the G61 flow front on July 22, 2016.
The flow was about 615m from the road and 760 m from the ocean. (Click to enlarge)

During early morning field observations, a large breakout of lava near the base of Pūlama Pali (steep fault scarp in background) was visible through fumes from the lava tube and heat shimmer from lava on the coastal plain.

The approximate location of the lava tube feeding Kīlauea's active lava flow is visible as degassing sources (white fume) on the pali. (Click to enlarge)

The approximate location of the lava tube feeding Kīlauea’s active lava flow is visible as degassing sources (white fume) on the pali. (Click to enlarge)

A breakout at the base of the pali viewed by a field crew this morning has formed a channelized ʻaʻā flow on the steeper portion of the coastal plain.

hvo 723d

A close up view of the ʻaʻā channel.

hvo 723e