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A section of the Great Crack that shows the 1823 lava flow that flowed to the ocean. A 1,500 to 3,000 year old cinder cone is in the background. A National Park Service public meeting from noon to 2 p.m. Saturday at Pāhala Community Center aims to draw community comment to plan management of the area. NPS Photo by Janice Wei |
THE GREAT CRACK AND ALA WA'I PUBLIC INPUT MEETING IS SATURDAY noon to 2 p.m. at Pāhala Community Center. The National Park Service posted the following: "Your input is needed. Come talk story with the park this Saturday in Pāhala about future access and use of the Great Crack and Ala Waiʻi parcels." These new park lands totaling more than 4,700 acres are located makai of Hwy 11 between Pāhala and Volcano.
The park recently accepted stewardship of the 1,951-acre Great Crack and the adjacent 2,750-acre Ala Waiʻi area to protect them from development.
"The areas, located in the remote southwest rift zone of Kīlauea, harbor unique geologic, biological and cultural resources and are managed as wilderness. Bring your manaʻo and join us at the Pāhala Community Center this Saturday, Sept. 23 from noon to 2 p.m. to talk-story with park staff about these special areas."
The public is also invited to email input at havo_planning@nps.gov.
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| This landscape image was taken in Ala Waiʻi looking east across an old pāhoehoe lava flow fronting a deep, prominent earth crack with vegetation in the far distance. NPS Photo by D. Foster |
MAUNA LOA SUMMIT CABIN REOPENED FRIDAY. The remote, high-elevation cabin in Hawaiʻi Volcanoes National Park near the summit of Mauna Loa volcano had been closed since November of 2022 when the volcano was getting ready to erupt.
The cabin is accessible from ʻĀinapō Trail and Kapāpala Ranch. A statement from Hawai'i Volcanoes says, "This extremely grueling, rocky and steep 10.2-mile hike is not for everyone. Hikers are urged to be prepared and know their limits. Water is available at the cabin, but must be treated before drinking."
Cabin permits and gate access through the ranch are required and a high-clearance 4WD is needed for ʻĀinapō Road. Safety information, preparedness tips and directions to obtain a permit for Mauna Loa Summit Cabin are on the
park website. Permits cost $10 (plus the park entrance fee) and can include up to 12 people for as many as three nights.
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Mauna Loa Summit Cabin reopened Friday, September 22, 2023. It had been closed since October 5, 2022, preceding the anticipated Mauna Loa eruption of November 2022. NPS Photo by A. LaValle |
State of Hawaiʻi manages
ʻĀinapō Trail and ʻĀinapō Cabin at Halewai (7,750 feet), where most hikers spend the night before heading to Mauna Loa Summit Cabin (13,250 feet). Overnight use of ʻĀinapō Cabin requires a state permit, the per-night fees are $30 for Hawaiʻi residents; $50 for non-residents. Visit the Hawaiʻi State Parks'
Wiki Permits webpage for reservation information.ʻĀinapō Trailhead and ʻĀinapō Cabin are accessed via the rough and bumpy eight-mile
ʻĀinapō Road, an infrequently maintained 4WD road that passes through Kapāpala Ranch for 5.7 miles and continues another 2.3 miles through the Kapāpala Forest Reserve to the ʻĀinapō Trailhead. Limited parking is available. From ʻĀinapō Trailhead it is a challenging 2.7-mile hike to ʻĀinapō Cabin. From ʻĀinapō Cabin it is another difficult 7.5-mile hike to reach Mauna Loa Summit Cabin.
For access through Kapāpala Ranch, go to
Forest Reserve Access (Kapāpalaranch.com) and submit the new online form. Although some hikers have trekked up from Highway 11 to Mauna Loa Summit Cabin, this adds an additional eight miles on foot to the 10.2-mile hike and still requires cabin permits and gate access.
To prepare the cabin for reopening, Hawaiʻi Volcanoes National Park staff replaced the solar charger and batteries in the main lua (pit toilet), replaced the lua roof, installed rain catchment gutters on the cabin roof and shoveled out 565 pounds of waste that was flown off the mountain. Hawaiʻi State Trails staff recently conducted cabin maintenance and reflagged ʻĀinapō Trail.
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Aerial photo of northern rim of Mauna Loa showing extensive lava extrusion from the November 2022 eruption.
NPS Photo by Janice Wei |
Mauna Loa Trail above Red Hill Cabin remains closed due to damage and hazards from the November 2022 Mauna Loa eruption.
Lava from the eruption covered the floor of Mokuʻāweoweo caldera and about four miles of Mauna Loa Trail in eight different areas. Flow thickness ranges from a few feet to almost 70 feet and presents significant hazards. In addition to increasing the risk of getting lost in the absence of a trail, thin layers of solidified lava can collapse if walked on, causing lacerations or injury by falling into a cavity.
More information, a video and a story map about the
2022 Mauna Loa eruption is available on the park website.
TSUNAMIS POSE A MAJOR THREAT TO HAWAI'I, says this week's
Volcano Watch, sponsored by USGS Hawaiian Volcano Observatory and written by Jonathan R. Weiss, a geophysisist with NOAA/NWS/Pacific Tsunami Warning Center: Weiss sets the stage:
It's 3 a.m. and you're halfway through a 12-6 a.m. graveyard shift at the NOAA Pacific Tsunami Warning Center in Honolulu, Hawaii. Fortunately, you slept before your shift began so you're feeling alert while you alternate between performing checks on the global seismic and sea level data analysis systems and doing research aimed at improving the speed and accuracy of earthquake magnitude estimation.
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The locations, years, and maximum reported Hawai'i runups (i.e., wave heights) for significant Pacific-wide tsunamis. Red-orange-yellow contours indicate the travel time to Honolulu for a tsunami with different origins. For example, an earthquake generated locally on the southeast coast of the Island of Hawaiʻi would arrive in Honolulu in less than an hour. Waves generated by a Japan earthquake might take 8 hours to reach Honolulu. Tsunami waves from the Aleutians would arrive in Honolulu in about 5 hours. The inset map in the upper right corner shows maximum runups for waves generated by the 1946 Aleutian Islands earthquake (meters/feet).
See this link for map credits and more information. |
The Inouye Regional Center, located on Ford Island in the middle of Pearl Harbor, is quiet and the lights are dim. This time of day at PTWC can be spooky; you and your colleague (asleep in one of the standby rooms) are the only people in the repurposed and modernized World War II-era airplane hangar. Every glimmer and rattle raises your eyebrows.
You brew some coffee and as you wait one of your beepers goes off notifying you that an earthquake has just occurred in the southwest Pacific Ocean. You abandon your warm beverage and hustle to the operations center. You have one minute to perform a preliminary assessment before the standby scientist is alerted.
There are only a few seismic stations on remote islands in the southwest Pacific, so it is critical to work fast as the seismic waves propagate outwards from the source. A quick visual inspection of the data scrolling across one of the monitors indicates that a large and potentially tsunamigenic event has just occurred.
The computer-generated automatic solutions confirm your suspicion. The earthquake was shallow and probably had a magnitude (M) greater than 8.5. Your stress level increases but your training has prepared you to handle the event. You immediately send a "PLEASE RESPOND" page to your teammate and you begin to further analyze the seismic information to better constrain the earthquake location and magnitude.
A moment later your coworker emerges ready to assist you with issuing initial tsunami threat messages, forecasting tsunami wave arrival times and amplitudes using numerical models, and monitoring coastal sea-level gauges and seafloor pressure sensors to confirm that a tsunami was generated. The phone rings and you hear the voice of a concerned colleague from the Tonga Meteorological Office on the line. Two minutes have passed since the initial pager alarm sounded. It's going to be a long and nerve-racking day.
The scenario described above is hypothetical and intended to paint a picture of life working at PTWC. An M8.5 or greater earthquake in the southwest Pacific would likely be deadly;
the 2009 M8.1 Samoa Islands earthquake and tsunami killed hundreds of people and caused catastrophic damage to Samoan and Tongan coastal communities and marine ecosystems.
Despite ongoing enhancements to the global network of seismic instruments and continued efforts aimed at improving community preparedness,
tsunamis, whether caused by a submarine earthquake, volcanic eruption, or landslide, still pose a major threat globally. The Hawaiian Islands, located in the center of the Pacific Ocean, are in a precarious position. The largest tsunamigenic earthquakes, which typically occur in places like Japan, the Aleutian Islands, and Chile, generate waves that more often than not head directly to Hawai'i.
The 1946 M8.6 Aleutian Islands earthquake and tsunami, which led to the establishment of PTWC, killed 159 people in Hawaii.
The 1960 M9.5 Chile earthquake (the largest ever recorded) and tsunami caused Pacific-wide destruction and killed 61 Hawai'i residents. However, it has been well over half a century since Hawai'i was heavily impacted by a damaging tsunami. Even
the 2011 M9.1 Japan earthquake and tsunami, which wreaked havoc across large swaths of the Pacific, caused relatively minor damage in Hawai'i.
The recent wildfires in Maui have focused a spotlight on natural disaster preparedness and response. In addition, September is
National Preparedness Month. Hawai'i will likely be threatened again by a potentially deadly tsunami considering
the frequency of past events. PTWC, the NOAA National Tsunami Warning Center in Alaska, and Tsunami Service Providers around the world serve as the first line of defense but coastal community residents can do their part to educate themselves about all natural hazards, including earthquakes and tsunamis. For more information visit
tsunami.gov and
tsunamiwave.org.
Volcano Activity Updates: Kīlauea is not erupting. Its USGS Volcano Alert level is ADVISORY.
The Kīlauea summit eruption that began on September 10th stopped on September 16. Summit
seismicity has remained low, with very few earthquakes over the past week, and tremor is at background levels. Since the eruption, summit tilt has alternated between minor deflation and inflation. A sulfur dioxide (SO2)
emission rate of approximately 240 tonnes per day was measured on September 19.
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| Wreckage of a clubhouse on Kamehameha Avenue in Hilo, Hawai'i, caused by a tsunami generated by the April 1, 1946, earthquake in the Aleutian Islands. Portions of downtown Hilo were devastated by the tsunami associated with the 1946 Aleutian Islands earthquake. Coastal communities in Hawaii are not immune to such an event happening again. Photo courtesy of the U.S. Army Corps of Engineers. |
Mauna Loa is not erupting. Its USGS Volcano Alert Level is at NORMAL.Webcams show no signs of activity on Mauna Loa.
Seismicity remains low. Summit ground
deformation rates indicate slow inflation as
magma replenishes the reservoir system following the recent eruption. SO2 emission rates are at background levels.
One earthquake was reported felt in the Hawaiian Islands during the past week: a M3.3 earthquake 10 km (6 mi) E of Pāhala at 31 km (19 mi) depth on Sept 14 at 7:07 p.m. HST.
HVO continues to closely monitor Kīlauea and Mauna Loa. Visit HVO's website for past Volcano Watch articles, Kīlauea and Mauna Loa updates, volcano photos, maps, recent earthquake information, and more. Email questions to
askHVO@usgs.gov.
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