VACCINATIONS FOR THOSE AS YOUNG AS 16 were given today at a mass event. It was sponsored by Kaʻū Hospital's sister facility, Hilo Medical Center, and was held at Edith Kanakaʻole Stadium. It was the island's biggest vaccine event to day, with Over 5,000 recipients of the Pfizer vaccine. Today marked the first day eligibility was opened to everyone 16 years and older. High school and college students were among those receiving their vaccines today. Hilo Medical Center hit another milestone administering its 25 thousandth dose. It went to Hilo resident Noah Hegerfeldt.
College and high school youth took the vaccine at the mass clinic today in Hilo. Photo from Hilo Medical Center |
The next mass vaccination clinic will be held on April 24. The alternate clinic for weekday and kupuna-friendly appointments is located at the Arc of Hilo. Pfizer is the only vaccination currently approved for those who are 16 and older. Johnson & Johnson and Moderna are approved for 18 years and older.
To read comments, add your own, and like this story, see Facebook. Follow us on Instagram and Twitter. See our online calendars and our latest print edition at kaucalendar.com.SEVEN NONPROFITS WILL HELP THOSE IN NEED OF RENTAL ASSISTANCE ON HAWAIʻI ISLAND. Applications for the county's Emergency Housing Rental Assistance Program will be available starting Monday, April 12 at 8 a.m.
ERAP is funded by the County of Hawaiʻi through federal funding and will provide rent and utility grants to an estimated 3,400 households that income qualify and can prove hardship due to COVID-19 for each month they needed assistance from March 2020 to December 2021. Funding will be limited to households; primary residence on Hawaiʻi Island. Households will be limited to 12 months or total rent assistance.
Hawaiʻi County ERAP will be led by local nonprofit community development financial institution, Hawaiʻi Community Lending. Six Hawaiʻi Island-based nonprofit partners will process applications and payments will be directly to landlords, property managers, or utility providers. Approved applicants will also have access to financial counseling and other housing stability services. The partners are HOPE Services Hawaiʻi, Hawaiʻi First Federal Credit Union, Neighborhood Place of Puna, Habitat for Humanity Hawaiʻi Island, The Salvation Army, and Hawaiʻi County Economic Opportunity Council.
Hawaiʻi Mayor Mitch Roth said, "We are honored to be able to provide relief to our local families by alleviating some of the financial pressures caused by the COVID-19 pandemic. With the help of local nonprofit organizations, we will keep the roofs over the heads of 3,400 households and that, to me, is something pretty special Through continued partnerships and the community's support, we will thrive through this pandemic together."
Household income maximums to apply are $46,720 for one person, $53,360 for two $60,000 for three, $66,640 for four, $72,000 for five $77,360 for six; $82,640 for seven and $88,000 for eight.
Priority is given to families earning 50 percent of area median income and have been unemployed for 90 days.
To read comments, add your own, and like this story, see Facebook. Follow us on Instagram and Twitter. See our online calendars and our latest print edition at kaucalendar.com.
LAVA LAKES OF KILAUEA, THEN & NOW is the title of this week's Volcano Watch, which says: One of the most interesting aspects of the current activity in Halemaʻumaʻu is the occasional oozing of lava around the edges of the entire crater while the lava surface is rising. Has that phenomenon been reported before in any accounts of previous Kīlauea activity?
Halemaʻumaʻu filled and drained numerous times during the nineteenth and early twentieth centuries. One such cycle of rising lava level occurred between 1914 and 1918. Lava levels fluctuated but rose slowly until the 180 m (600 ft) deep pit was filled, finally spilling over the rim in February 1918.
Over the next 21 months, the pit overflowed more than dozen times, and lava erupted from a crack 200 m (650 ft) northeast of the pit. All Halemaʻumaʻu surface activity abruptly ceased on November 28, 1919, when the lava surface dropped 180 m (600 ft) in a single morning, leaving a small triangular lava lake at its bottom.
Thomas Jaggar, founder of the Hawaiian Volcano Observatory, observed much of this activity and afterward noted that the pit walls were covered with "a veneer of glowing matter moulded against the walls of the pit, and ... striated vertically."
He concluded that a cylindrical shell of molten lava (ring dike) surrounding the more solid interior fill of the crater had remained liquid and that its "lubricating action...accounts for the extraordinary quietness and quickness" of draining on November 28th. He also noted that surface features of the new pit floor bore a strong resemblance to the features present before the collapse—the crater fill had dropped like a piston!
The pit began to refill almost immediately, first with an enlarging, rising lava lake, followed by bodily uplift of the floor. Molten lava emerged between the crater wall and the floor material, tilting the edges of the pit floor inward to create a basin in the center of the floor. Lava then flowed from a narrow circular lake between the pit walls and the uplifted floor edges to the central basin, forming a ring-shaped island. Jaggar considered this further evidence of a ring dike.
The eruption in Kīlauea Iki in 1959 provided another opportunity to document lava lake behaviors. The eruption proceeded through 17 episodes of spectacular lava fountains in about five weeks, partially filling a pre-existing crater. The entire crust of the lava lake was frequently broken up by what is now called foundering.
"The process ... began with molten lava lapping over the leading edge of the crust. Within seconds, or at most a minute, a major crack would form several feet back in the crust parallel to the edge...Then lava would rapidly well up in the major crack...tilting the detached block so that it slipped forward, or was dragged under, into the molten lava. The upwelling lava also lapped over the new leading edge of the old crust setting the stage for another cycle."
During the eighth episode, scientists on the east edge of the lake noticed that the lake crust was slightly higher in the middle and it primarily foundered around the lower edges as overall lava level rose.
Which process is occurring at Halemaʻumaʻu now? The current lake surface shows no sign of being tilted radially inward by a ring dike around its edges as in 1919. Jaggar's ring dike also produced lava emerging around the entire crater floor, but the current oozing activity usually appears briefly in limited areas cumulatively expanding the lake surface over time. Crust over a lava lake rising in a pit shaped like an inverted funnel may slowly open gaps between the crust edge and the pit walls. The crust around the edges are the newest and thinnest facilitating foundering.
Over the next 21 months, the pit overflowed more than dozen times, and lava erupted from a crack 200 m (650 ft) northeast of the pit. All Halemaʻumaʻu surface activity abruptly ceased on November 28, 1919, when the lava surface dropped 180 m (600 ft) in a single morning, leaving a small triangular lava lake at its bottom.
Thomas Jaggar, founder of the Hawaiian Volcano Observatory, observed much of this activity and afterward noted that the pit walls were covered with "a veneer of glowing matter moulded against the walls of the pit, and ... striated vertically."
In 1918, Isabel Jaggar, wife of Hawaiian Volcano Observatory Director Thomas A. Jaggar Jr., stands near the edge of Halema'uma'u during a period of lava overflowing onto the crater floor. |
The pit began to refill almost immediately, first with an enlarging, rising lava lake, followed by bodily uplift of the floor. Molten lava emerged between the crater wall and the floor material, tilting the edges of the pit floor inward to create a basin in the center of the floor. Lava then flowed from a narrow circular lake between the pit walls and the uplifted floor edges to the central basin, forming a ring-shaped island. Jaggar considered this further evidence of a ring dike.
The eruption in Kīlauea Iki in 1959 provided another opportunity to document lava lake behaviors. The eruption proceeded through 17 episodes of spectacular lava fountains in about five weeks, partially filling a pre-existing crater. The entire crust of the lava lake was frequently broken up by what is now called foundering.
"The process ... began with molten lava lapping over the leading edge of the crust. Within seconds, or at most a minute, a major crack would form several feet back in the crust parallel to the edge...Then lava would rapidly well up in the major crack...tilting the detached block so that it slipped forward, or was dragged under, into the molten lava. The upwelling lava also lapped over the new leading edge of the old crust setting the stage for another cycle."
During the eighth episode, scientists on the east edge of the lake noticed that the lake crust was slightly higher in the middle and it primarily foundered around the lower edges as overall lava level rose.
Which process is occurring at Halemaʻumaʻu now? The current lake surface shows no sign of being tilted radially inward by a ring dike around its edges as in 1919. Jaggar's ring dike also produced lava emerging around the entire crater floor, but the current oozing activity usually appears briefly in limited areas cumulatively expanding the lake surface over time. Crust over a lava lake rising in a pit shaped like an inverted funnel may slowly open gaps between the crust edge and the pit walls. The crust around the edges are the newest and thinnest facilitating foundering.