This small-scale map shows Kīlauea’s active East Rift Zone lava flow in relation to lower Puna. The area of the flow on June 30 is shown in pink, while widening and advancement of the flow as of July 7 is shown in red.
Click to enlarge
The blue lines show steepest-descent paths calculated from a 1983 digital elevation model (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. Puʻu ʻŌʻō lava flows erupted prior to June 27, 2014, are shown in gray.
Statement from Henry Yang, Chair of the TMT International Observatory Board:
“After more than two months of consultation, education, and dialogue with many stakeholders, we humbly announce that the TMT International Observatory Board has decided to move ahead to restart the construction of the Thirty Meter Telescope on the morning of Wednesday, June 24. Our period of inactivity has made us a better organization in the long run. We are now comfortable that we can be better stewards and better neighbors during our temporary and limited use of this precious land, which will allow us to explore the heavens and broaden the boundaries of science in the interest of humanity.
“We look forward to a positive relationship with all Hawaiians, while we understand that the majority of Hawaii’s people are supporting the TMT project. We deeply respect and are mindful of those who have concerns, and yet, we hope they will permit us to proceed with this important task while reserving their right to peaceful protest.
“As done at any construction site, we plan to first investigate and assess any possible oil leakage and ensure we can provide proper maintenance of machines and equipment so they operate safely and correctly – in order to protect Maunakea and preserve the sensitive environment. We will then begin to repair and install fencing in the interest of public safety.
“As we proceed, TMT is open and willing to allow cultural practitioners in the area of the construction site to continue customary and traditional practices. Allowing this practice to continue to occur will require further dialogue and mutual agreement to work out the details in order to establish a cooperative and harmonious environment for all parties.
“In an effort to be sensitive to and observant of the Native Hawaiian host culture, we will deepen our knowledge of the cultural, ecological, and spiritual aspects of the mountain and continue to learn how to better respect and appreciate Maunakea’s important cultural areas.
“On behalf of TMT, I want to express our sincere appreciation to the people in Hawaii for their understanding and support.”
Bishop Silva has done little or nothing to reach out and comfort the brave men and women who have come forward to say that they were sexually abused by Hawaii’s clerics. Instead of doing even the smallest thing to comfort the wounded, he salutes and honors those who may have caused horrible damage. Not only does this defy the way of Aloha, but Silva’s irresponsible actions deter other victims, witnesses and whistleblowers from speaking up. He’s also essentially encouraging other Catholic officials to behave in similarly hurtful ways in clergy sex abuse and cover up cases.
Statement by Joelle Casteix of Newport Beach, CA, SNAP Western Regional Director,
Hawaii Volcano Observatory Statement on current activities:
After a week of elevated activity, HVO would like to review recent observations and thoughts on what we may expect next at Kīlauea Volcano. LAVA FLOWS ON THE FLOOR OF HALEMAʻUMAʻU
Beginning at about 9:40 p.m., HST, last night and continuing into this morning, the Overlook crater lava lake overflowed its rim on several occasions, sending short, lobate sheets of pāhoehoe as far as 130 m (142 yds) across the floor of Halemaʻumaʻu Crater. These overflows were captured on USGS-HVO’s web cameras. Thus far, the flows have been brief and their forward motion ceased as the lava lake level fell and lava subsided into the Overlook crater. As yet, no change in lava spattering or surface circulation patterns on the lake in response to these overflows has been noted.
Given the sustained high, and slowly rising, levels of lava within the vent during the past week, these overflows were expected and they are likely to continue intermittently. During similar lava lake activity at Halemaʻumaʻu in the 1800s and early 1900s, lava lakes frequently produced overflows. Over time, overflows and intermittent spattering can build a collar of solidified lava that then contains the rising and circulating lava lake. This phenomenon is known as a ‘perched lava lake.’
ROCKFALLS, EXPLOSIONS, AND SPATTER ON THE HALEMA‘UMA‘U CRATER RIM; ASHFALL AT JAGGAR OVERLOOK AND BEYOND
Yesterday morning at about 10:20 a.m., HST, a rockfall from the southeast wall of Halemaʻumaʻu Crater above the lava lake initiated an explosion from the lake surface. Large clots of molten spatter up to 2 meters (2 yards) across showered the rim of Halemaʻumaʻu in the vicinity of the closed visitor overlook fence. The hot spatter formed a nearly continuous blanket for about 100 m (110 yards) along the crater rim and extended back from the rim about 50 m (55 yards). Small bits of crater-wall rock were embedded in the spatter clots. Additional explosions and showers of rock and spatter can be expected. They can occur suddenly and without warning and underscore the exceedingly hazardous nature of the Halema‘uma‘u Crater rim, an area that has been closed to the public since late 2007.
Visitors to the Hawai‘i Volcanoes National Park Jaggar Museum Overlook and other Park areas should also note that under southerly wind conditions, similar rockfalls and explosions can result in a dusting of powdery to gritty ash composed of volcanic glass and rock fragments. Several such ashfalls occurred last weekend and, although they represent a very minor hazard at this time, people should be aware that additional dustings of ash are likely at Jaggar Museum and other areas around the Kīlauea summit. For more information about volcanic ash hazards and precautions at Kīlauea, please see: http://hvo.wr.usgs.gov/hazards/FAQ_SO2-Vog-Ash/main.html
CONTINUED INFLATION AND EARTHQUAKE ACTIVITY IN THE KĪLAUEA SUMMIT AND UPPER EAST RIFT ZONE
For the past week or so, HVO monitoring networks have recorded steady inflation of the Kīlauea Volcano summit area. Shallow earthquake activity has also been elevated beneath the summit caldera, upper East Rift Zone, and upper Southwest Rift Zone. Of the hundreds of earthquakes that have occurred in the past week, most have been small, less than magnitude-2 (M2).However, this morning (April 29) a M3.0 earthquake occurred at the easternmost caldera boundary. It is the second M3+ earthquake in this region during this sequence.
During this period of elevated summit activity, there has been no obvious change in the eruption rate of lava from Puʻu ʻŌʻō. Rates of gas emission from both the summit and Puʻu ʻŌʻō remain largely unchanged. Short-lived increases in sulfur dioxide from the summit lava lake have been noted during rockfall-triggered explosive events, such as the one that occurred yesterday morning.
Video by Mick Kalber:
WHAT WE CAN EXPECT
The current activity is best explained by an increase in magma supply to the Kīlauea Volcano magma reservoir or storage system, something that has occurred many times during the ongoing East Rift Zone eruption. Increased supply and shallow storage can explain the higher magma column in the Overlook crater, as well as the continuing inflation and elevated earthquake activity in the summit region. Higher volumes of magma moving throughout the summit and upper East Rift Zone pressurizes the reservoir and magma transport system and causes small earthquakes and inflationary tilt.
As long as magma supply is elevated, we expect continued high lava lake levels accompanied by additional overflows. Lava from these overflows could cover more of the Halemaʻumaʻu Crater floor, form a perched lake, or result in some combination of these two processes. Spattering or lava fountaining sources can migrate across the surface of the lava lake, as recently observed. We expect continued rockfalls, intermittent explosions and ash fall, and continued high levels of gas release.
The evolution of unrest in the upper East Rift Zone is less certain. It is possible that a surge of lava will reach Puʻu ʻŌʻō and lava flow output will increase, both on the flanks and within the crater of Puʻu ʻŌʻō. It is also possible that lava will form a new vent at the surface. If this happens, it will most likely occur along a portion of the East Rift Zone between Pauahi Crater and Puʻu ʻŌʻō. Other outbreaks in the summit area or along either rift zone on Kīlauea cannot be ruled out. If a new outbreak or surge in lava to Puʻu ʻŌʻō occurs, we will expect a drop in the summit lava lake.
HVO continues to closely monitor Kīlauea Volcano. We are especially watching for any sign of unrest that may precede a new outbreak of lava or a change in output at either Puʻu ʻŌʻō or the summit Overlook crater vent. We will continue to post daily eruption updates on the HVO web site, along with photos, videos, and maps as they are available at: http://hvo.wr.usgs.gov/activity/kilaueastatus.php
An annotated photograph showing summit features named in this statement, such as Overlook crater and Halemaʻumaʻu, is posted at: http://hvo.wr.usgs.gov/archive/summit-labels.jpg
In light of numerous inquiries about the disclosure of P-Card usage by government employees, the state Office of Information Practices (OIP) is generally advising agencies to disclose unredacted P-Card records to requesters, because all purchases made on the cards are supposed to be justified as work-related expenses.
In rare circumstances, there may be confidential information that should be redacted because of a significant privacy interest, such as medical information.
P-Card usage is distinguished from personal credit card reimbursements sought by employees for work expenses. In the case of employees’ requests for reimbursement of work-related expenses paid for by their personal credit cards, it is proper to redact all personal or confidential information on the personal credit card invoices, such as all non-work related purchases, personal address, credit card number, interest rates, balances, payments due, and rewards points.
P-Card records to requesters, agencies are further cautioned to redact confidential P-Card account numbers and any taxpayer identification numbers for vendors. Oftentimes, a vendor’s taxpayer ID number is a person’s social security number, which should be redacted prior to disclosure.
For the latest open government news, check for archived copies of What’s New articles that are posted here, or e-mailed upon request. To be added to OIP’s e-mail list, please e-mail firstname.lastname@example.org. Also, if you would like to receive What’s New articles or attachments in a Word format, please contact OIP at (808) 586-1400 or email@example.com.
Unfortunately the ship had to turn around once it got to the Big Island because the water in Hilo Harbor was not deep enough for the ship to port.
The NAVY has released the following statement:
In an abundance of caution and as advised by the embarked State Dept. of Transportation Harbor Pilot, the Commanding Officer of USS Chung-Hoon (DDG 93) felt it was prudent to not proceed with entering Hilo Harbor this morning due to the shallow depth of the harbor.
Sharing the Navy with the people of Hilo is important. We certainly value the opportunity to showcase our Navy to the American people. Our partnership with the Hilo Council is an outstanding example where a community and the military join together to create an environment of mutual support and broad benefit and the Navy looks forward to continuing this partnership for many years to come, and we deeply regret the inconvenience this has caused to our friends and neighbors in Hilo.
Capt. Mark Manfredi, Chief of Staff, Navy Region Hawaii will still attend tonight’s Merrie Monarch Festivities and the U.S. Pacific Fleet Band will be flown over here to march and perform in the Merrie Monarch Parade tomorrow morning.
This map shows recent changes to Kīlauea’s active East Rift Zone lava flow field.
Click to enlarge
The area of the flow on March 10, before shutting down near Pāhoa, is shown in pink, while widening and advancement of the flow based on satellite imagery from April 1 is shown in red. Some recent changes north of Puʻu ʻŌʻō are not shown, as that part of the flow field was hidden from satellite view by clouds.
NextEra Energy, Inc. and Hawaiian Electric Company, Inc., Hawaii Electric Light Company, Inc. and Maui Electric Company Limited (collectively referred to as Hawaiian Electric), today announced that the companies will be hosting a series of 13 open house informational meetings across Hawaii to introduce residents to NextEra Energy and the benefits of the companies’ pending merger as well as to provide members of the public with the opportunity to provide input directly to company officials.
The open houses will take place on Oahu, Hawaii Island, Maui, Molokai and Lanai from April 7 to April 16.
“Since we announced our merger late last year, we’ve been gratified at the reception we’ve received as well as the high level of interest in this important topic for Hawaii,” said Eric Gleason, president of NextEra Energy Hawaii, LLC. “NextEra Energy shares Hawaiian Electric’s vision of increasing renewable energy, modernizing its grid, reducing Hawaii’s dependence on imported oil, integrating more rooftop solar energy and, importantly, lowering customer bills. We recognize that addressing Hawaii’s energy challenges requires Hawaii-specific energy solutions, and that is why we look forward to meeting with and listening to residents across Hawaii. The meetings will provide us with the opportunity to receive valuable feedback while allowing residents to learn more about NextEra Energy and the significant near- and long-term benefits this merger will deliver to Hawaiian Electric customers and the state of Hawaii.”
“In selecting NextEra Energy as our partner, we will join a company that shares our community and environmental values, has a proven track record of lowering electric bills, is the world’s largest generator of renewable energy from the wind and sun, and is committed to rooftop solar in Hawaii,” said Alan Oshima, Hawaiian Electric’s president and chief executive officer. “We can’t imagine a better match to help us accelerate the clean energy transformation we all want for Hawaii. We hope our customers will take the opportunity to meet members of the NextEra Energy team and learn firsthand why NextEra Energy is the right partner to help us achieve a cleaner and more affordable energy future for Hawaii.”
About the Open House Meetings
Each open house meeting will be held from 5 to 8 p.m. Hawaii Standard Time. Senior leaders and other employees from NextEra Energy and Hawaiian Electric will be available to discuss NextEra Energy’s track record of increasing renewable energy, lowering customer bills, creating innovative solutions for modernizing the grid, and supporting local communities, as well as all the expected benefits from the proposed merger with Hawaiian Electric.
The dates and locations for the meetings are as follows:
Central Maui: Maui Electric Auditorium
South Maui: Kihei Community Center
West Maui: Lahaina Civic Center
Lanai: Lanai Community Center
Molokai: Kaunakakai Elementary School Cafeteria
Hilo, Hawaii: Hilo High School Cafeteria
Puna, Hawaii: Pahoa High School Cafeteria
West Hawaii: Kealakehe High School Cafeteria
Waimea, Hawaii: HPA Village Campus Dining Hall
West Oahu: Kapolei High School Cafeteria
Leeward Oahu: Pearl City High School Cafeteria
Honolulu: Ward Warehouse, Kakaako Conference Room
Windward Oahu: Windward Community College, Hale Akoakoa
As the 2015 Legislature reached its midway point this week, a number of bills introduced by Puna Representative Joy San Buenaventura are now up for consideration by the Senate after being passed by the full House of Representatives.
Reps. Joy San Buenaventura and Richard Creagan on the House floor.
“I’m pleased that we’ve been able to keep these bills alive halfway through the very rigorous process of creating legislation,” Rep. Buenaventura said. “They represent real solutions to everyday issues and problems faced by the people of Puna in the aftermath of life changing natural disasters, and I will continue to push for them even as they move to the Senate chambers.”
Among the bills are several measures that seek to address concerns raised by residents affected by the recent natural disasters that have impacted the Puna region.
HB737, HD2 helps current and future homeowners who reside in lava zone areas that has been declared to be in a state of emergency to obtain and renew property insurance policies. This Act also enables a homeowner, in such a lava zone, who had no prior property insurance coverage to purchase insurance coverage to be effective within six months from the date of policy acceptance. (Co-introducer)
HB1314 HD1 establishes the emergency home relocation special fund to assist persons dispossessed of their homes as a result of a natural disaster by providing for infrastructure development, grants, and loans. (Primary Introducer)
HB376 HD2 makes specific changes to the Chief Election Officer including designating the position as an at-will employee; and requires the State Elections Commission to conduct a performance evaluation and to hold a public hearing on the performance of the Chief Elections Officer. (Primary introducer)
Others bills introduced by Rep. San Buenaventura and passed by the House include:
HB847, HD1 appropriates funds for an Interdisciplinary Hawaii Health Systems Corp. (HHSC) Primary Care Training Program at Hilo Medical Center to address the shortage of primary care physicians—particularly on the neighbor islands and in rural communities. (Co-introducer)
HB851, HD1 appropriates funds to establish an advanced life support ambulance based in Puna. (Co-introducer)
HB1107 appropriates funds for the establishment and maintenance of a bookmobile that will serve the rural areas of the island of Hawaii. (Primary introducer)
HB1370, HD1 provides statutory authority for the Employees’ Retirement System Administrator to make direct payment to a former spouse of a member of benefits or portion thereof pursuant to valid court judgment, order or decree. (Primary introducer)
HB87 shields process servers from prosecution under criminal trespass statutes when performing their duties. (Primary introducer)
This map shows the active lava tube system that has been mapped from Pu’u O’o vent down to Kaohe Homestead area of Puna.
The yellow line represents the active tube. (Click to enlarge)
The flow travels at a faster pace underground then it does on the surface.
Today’s Hawaii County Civil Defense reported:
This is an eruption and lava flow information update for Tuesday March 10th at 8:00 AM.
Surface activity and activity along both margins extending from the west or just above the stalled flow fronts to the summit area continues with numerous small breakouts. The surface breakouts along the length of the flow pad continues to provide an indication that the tube system is being supplied and lava from the source is making its way to the down slope areas.
The June 27 Lava Flow remains very active and has advanced over 240 yards in the last few days.
Click to enlarge
There were two breakouts from the upper tube system on and at the foot of Puʻu ʻŌʻō Cone (right center). The largest and most active was the breakout nearest Puʻu Kahaualeʻa in the left center of the photograph.
Closeup of the new breakout near Puʻu Kahaualeʻa. Click to enlarge
The leading edge of the lobe nearest Pahoa Marketplace is still stalled but, for the past few days, a new breakout has been advancing along its southern margin and is approaching the Apaʻa St. firebreak.
Click to enlarge
Several breakouts were active upslope of the stalled front. This breakout issued from an inflated tumulus along the north margin of the June 27th flow.
Click to enlarge
The thin crust over the lava lake within the Halemaʻumaʻu Overlook crater was moving slowly to the southeast.
Click to enlarge
During the USGS overflight, there was no spattering and wispy gas emissions allowed clear views.
Contrary to some reports, the Hawaiian Electric Companies are continuing to accept solar photovoltaic (PV) applications through the current net energy metering process, which includes a technical review for safety and reliability. The companies are also making significant progress clearing pending applications on circuits that already have very high amounts of solar.
Overall, Hawaiian Electric, Maui Electric and Hawaii Electric Light continue to lead the nation in rooftop PV. An estimated 12 percent of the utilities’ customers have rooftop solar system, compared with the national average of less than one percent.
These efforts are part of the companies’ commitment to meet three overarching energy commitments by 2030. These include:
Nearly tripling the amount of distributed solar
Achieving 65 percent renewable energy use
Lowering customer bills by 20 percent
“We know rooftop PV is an important option for our customers. We are continuing to follow the current net energy metering process while the Public Utilities Commission considers our proposal to transition to a fairer, more sustainable program. It’s critical for our community that we increase solar in a way that maintains reliability and is safe and fair for all customers,” said Jim Alberts, Hawaiian Electric senior vice president for customer service.
A recent letter to some Hawaii Electric Light customers who submitted applications for projects in areas of Hawai‘i Island with high amounts of solar has been mischaracterized by a national solar group as an effort by the Hawaiian Electric Companies to stop all solar installations.
“We apologize for the confusion and want to assure our customers that we are continuing to process solar applications. We are reviewing our notification procedures to improve communication with our customers,” Alberts said.
Highlights of progress made
Earlier this week, Hawaiian Electric reported to the Hawaii Public Utilities Commission that it notified an additional 548 O‘ahu customers who have been waiting for their net energy metering applications to be processed. Hundreds more are now being approved.
This was the first large group of Oahu customers to be cleared from a backlog of 2,749 applications, all from neighborhoods with high existing amounts of PV as of last October. Hawaiian Electric has committed to clearing 90 percent of that backlog by April, with the remaining customers applications to be approved by the end of 2015.
In addition, Maui Electric approved 331 applications in neighborhoods with high amounts of solar, nearly clearing its entire backlog. Hawaii Electric Light had 336 applications under review in neighborhoods with high amounts of solar, and approvals have since begun.
Overall, more than 3,000 net energy metering applications have been approved since the beginning of the year across the five islands that the Hawaiian Electric Companies serve.
In January, Hawaiian Electric, Maui Electric, and Hawaii Electric Light proposed a new program that would support the continued growth of rooftop solar while ensuring equitable rates for all customers. The new transitional distributed generation program would help address the current growing cost shift for operating and maintaining electric grids from customers who have rooftop solar to customers who don’t. At the end of 2013, that cost shift was approximately $38 million. By the end of 2014, that subsidy borne by non-solar customers had grown to $53 million.
In conjunction with this transitional distributed generation program, the utilities expect to be able to help the growth of solar by more than doubling the threshold for neighborhood circuits to accept solar systems. This would eliminate in most of those cases the need for a longer and costly interconnection study.
Community Policing Officers are working with the Hawaiʻi County Planning Department to protect the public from illegal “rave” parties.
As a result of this partnership, the Planning Department issued a $5,000 fine to a property owner in connection with a “rave” party in Hawaiian Acres last year.
The two-day event held October 31 through November 1 was advertised on social media outlets. Community Policing Officers from the Puna District were made aware of the event and warned the property owner that he did not have the proper permit to conduct such an event on his property.
The party was held despite police warnings, and enforcement action was taken near the property on the night of the event to ensure public safety. Police conducted a follow-up investigation with the assistance of the Planning Department that resulted in the fine.
Police are reminding property owners that conducting an unpermitted non-agricultural commercial event on agricultural property is prohibited. The Hawaiʻi Police Department will continue to work with members of the public, property owners and the Planning Department to ensure compliance and enhance public safety.
Kīlauea’s East Rift Zone lava flow has not advanced any closer to Pahoa Marketplace, but is still active. Breakouts were also active near the True/Mid-Pacific geothermal well site, and along the distal 3 km (2 miles) of the flow, where a narrow lobe has been advancing toward the north-northeast.
The view is to the southwest. (Click to enlarge)
This shows a comparison of a normal photograph with a thermal image of the flow front. The white box shows the rough extent of the thermal image. White and yellow pixels in the thermal image show areas of active breakouts.
Although the leading tip of the flow has stalled, the thermal image shows that active breakouts are present a short distance upslope of the stalled tip. (Click to enlarge)
This view, looking northeast, shows the distal part of the flow, with the flow lobe behind Pahoa Marketplace to the right and the newer north-northeast advancing lobe to the left.
Ainaloa at top left. (Click to enlarge)
The north-northeast lobe is following a drainage that leads to the steepest-descent path that crosses Highway 130 about 1 km (0.6 mi) south of the Maku`u Farmer’s Market. The flow, however, is still 3.5 km (2.2 mi) upslope from that spot and moving slowly.
This photo shows a closer view of the narrow north-northeast advancing lobe about 2.5 km (1.6 mi) upslope from the Pahoa Markplace. The view is to the northwest. (Click to enlarge)
USGS Hawaiian Volcano Observatory (HVO) scientists conducted a helicopter overflight of the June 27th lava flow this afternoon and mapped its perimeter. At the time of the flight, surface breakouts along the distal part of the flow were scattered between 1 and 3.5 km (0.6 and 2.2 mi) upslope from the Pahoa Marketplace and posed no immediate threat.
Amongst this activity, a narrow flow lobe (about 2.5 km (1.6 mi) upslope from Pahoa Marketplace) was advancing toward the north-northeast. This lobe has entered a drainage that leads to the steepest-descent path that crosses Highway 130 about 1 km (0.6 mi) south of the Makuʻu Farmer’s Market, but the flow is still 3.5 km (2.2 mi) uplsope from that point and moving slowly. Small breakouts were also active in an area of persistent activity about 7 km (4 mi) upslope from Pāhoa. (Click to enlarge)
Daily updates about Kīlauea’s ongoing eruptions, recent images and videos of summit and East Rift Zone volcanic activity, and data about recent earthquakes are posted on the HVO Web site at http://hvo.wr.usgs.gov.
This large-scale map uses a satellite image acquired in March 2014 (provided by Digital Globe) as a base to show the area around the front of Kīlauea’s active East Rift Zone lava flow. The area of the flow on December 30 at 2:30 PM is shown in pink, while widening and advancement of the flow as mapped on January 6 at 11:30 AM is shown in red.
Click to enlarge
The most active parts of the flow were in an area 400 to 900 m (440 to 980 yards) behind the stalled tip of the flow above Pahoa Marketplace, and at the front of a flow lobe that branches off to the north about 3 km (2 miles) behind the stalled flow tip. Other active breakouts on the distal part of the flow were scattered between these two areas.
The blue lines show steepest-descent paths calculated from a 1983 digital elevation model (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.
This small-scale map shows Kīlauea’s active East Rift Zone lava flow in relation to lower Puna. The area of the flow on December 30 at 2:30 PM is shown in pink, while widening and advancement of the flow as mapped on January 6 at 11:30 AM is shown in red. Click to enlarge
The next lava flow community update meeting will be held with representatives from Hawai‘i County Civil Defense and the Hawaiian Volcano Observatory on Thursday, January 8 at 6:30 p.m. at the Pāhoa High School Cafeteria.
A view of Pu’u O’o going off today and the flow below it.
USGS Hawaiian Volcano Observatory (HVO) scientists conducted a helicopter overflight of the June 27th lava flow this afternoon and mapped its leading edge. At the time of the flight, the tip of the flow was stalled about 0.7 km (0.4 miles) from the Pahoa Marketplace, measured in a straight line, but lava was active in several places immediately behind the front.
A small, but fairly vigorous, breakout was active this afternoon about 1 km (0.6 miles) behind the tip of the flow. (click to enlarge)
One or more of these other active lobes could overtake the stalled front in the coming hours to days, or the stalled front could reactivate. Numerous breakouts were also active along the flow in an area extending from 1 to 3 km (0.6 to 2 miles) upslope from the front of the flow, in the ground crack area near the True/Mid-Pacific well pad, and about 3 km (2 miles) downslope from Puʻu ʻŌʻō.
Daily updates about Kilauea’s ongoing eruptions, recent images and videos of summit and East Rift Zone volcanic activity, and data about recent earthquakes are posted on the HVO Web site at http://hvo.wr.usgs.gov.