Ka‘ū News Briefs, Friday , Sept. 3, 2021

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HAWAI'I FARMERS UNION UNITED KAʻŪ CHAPTER MEETS THIS SUNDAY at Wood Valley Farm for a session on indigenous microorganisms. It will be taught by HFUU East Hawai'i Chapter president Drake Weinert from 9AM to 11:30AM. He will offer hands-on instruction on how to set an IMO box, hands-on practice applying microbes and general theory on the subject.
    After the class attendees are invited for lunch, provided by the host, Matt Drayer, president of Ka`u's Hawai'i Farmers Union chapter. A statement from HFUU says, "This is an opportunity to get to know your fellow chapter members in Hilo and Ka`u, network, and learn new ways to up your home gardening, or farming game with Indigenous Microbes."
The farm is located at 96-2232 South Rd, ust above Pahala off Wood Valley Road. HFUU member price is $20. Non-member price is $30. RSVP to sign up by emailing chefmattdre@gmail.com.To read comments, add your own, and like this story, see www.facebook.com/kaucalendar/. See latest print edition at kaucalendar.com.

ERUPTION? INTRUSION? WHAT'S THE DIFFERENCE? That is the title of this week's Volcano Watch, written by USGS Hawaiian Volcano Observatory Scientists and affiliates:
   We know that when a volcano erupts, molten red rock makes it to the surface, while during an intrusion it doesn’t. The difference between the two processes, if we depend on seismicity (earth shaking) or deformation (changes in ground surface) instrumentation, is not obvious. The events during the start of either are identical. But we can’t be certain that an intrusion will lead to an eruption.
    What are symptoms leading up to an eruption? The main player in monitoring volcanoes is seismicity—the frequency and magnitude of earthquakes. When magma enters the volcanic edifice, it accumulates and makes space for itself by compressing many tiny void spaces. Continued filling by magma creates pressure on the walls of reservoirs, causing slip, faults, or cracking in the surrounding brittle rock. All these motions result in the generation of earthquakes.
    Ground deformation may precede, accompany, or follow increased seismicity. We track changes in tilt—an adjustment of the surface of a volcano as magma moves into, or through, it. Networks of Global Positioning System (GPS) sensors spread across our volcanoes also detect minute changes in latitude, longitude, and elevation that helps pin point where deformation is occurring in near real-time.
    Satellite data is another part of our toolkit: Interferometric Synthetic Aperture Radar (InSAR) is an effective way to measure changes in land surface elevation, providing island-wide coverage and helps monitor our volcanoes. As magma intrudes underground, it can begin to deform the surface. The InSAR satellite is sensitive enough to record changes of a few centimeters at the volcanoes' surface outlining areas where magma is moving near the surface.
    So what happened last week? At 4:30 p.m. HST on August 23, HVO seismologists noted a flurry of earthquakes beneath the south caldera region at the summit of Kīlauea. This increase in earthquakes was accompanied by an increase in tilt at our Sandhill station. At 1:30 a.m., on August 24, the seismicity ramped up dramatically. Our interpretation was that magma was on the move.
    Based on the above sequence of events the U.S. Geological Survey's Hawaiian Volcano Observatory (HVO) issued a Volcano Observatory Notification for Aviation (VONA) and Volcano Activity Notice (VAN) on August 24, changing the aviation color code and volcano alert-level from Yellow/Advisory to Orange/Watch. Was the volcano going to erupt? Symptomatically, all the signs consistent with magma movement were observed, including increased seismicity and ground deformation. We took a “wait and see” approach, while we continued to closely monitor the situation. All the geologists were primed to go to the field at a moment’s notice!    Over the next 36 hours, the earthquake counts diminished, and tilt rates decreased—implying that an eruption was less likely. Based on the observed decline in activity, HVO issued a second VONA and VAN on August 26, changing the status of the volcano from Orange/Watch back to Yellow/Advisory. Making the call on whether or not a volcano is going to erupt is not easy, and Pele still seemed primed for action.
    Subsequently, on the evening of August 26, at 6:00 p.m., tilt west of the caldera ramped up, and was followed by an increase in seismicity at 8:30 p.m. The increase in earthquakes and in deformation suggested the intrusion was still being supplied with magma. Characteristically, all the elements that contribute to an eruption were present. But notably, seismicity remained at deeper levels within the volcano, and movement of magma toward the surface was not detected.
    How do we as volcanologists deal with the uncertainties of whether or not the volcano will erupt? One way is to look at past eruptive behavior. Last week’s Volcano Watch reviewed examples of past volcanic activity. Intrusions happened in the 1960s, 1970s, early 1980s, and more recently in 2006 and 2015. The only time an eruption occurred, following the many intrusions, was in 1974.
    All the events of the past week had volcanologists on high alert, ready to respond as our data indicated magma was on the move. Was the volcano going to erupt? We had no idea how the story would end. We are only able to closely monitor the situation, and watch as things unfold. This time we observed an intrusion. For residents, visitors, and geologists hoping to see red rock, the intrusion was a failed eruption.