At the Hawaiian Volcano Observatory (HVO), we continuously strive to improve our capability to monitor the volcanoes that we live upon. We have made great improvements to our monitoring networks in recent years, both in instrumentation to measure seismicity, gas and deformation of the ground, and in the communications infrastructure that brings the data from these instruments to HVO for analysis.
At the Hawaiian Volcano Observatory (HVO), we continuously strive to improve our capability to monitor the volcanoes that we live upon. We have made great improvements to our monitoring networks in recent years, both in instrumentation to measure seismicity, gas and deformation of the ground, and in the communications infrastructure that brings the data from these instruments to HVO for analysis.
We are particularly concerned with monitoring areas with dense populations atop and downslope of active rift zones, such as the lower east rift zone of Kilauea in lower Puna. The lower Puna region has been a challenge to monitor instrumentally because of the difficulties of relaying the data via traditional radio links to the observatory (due to the topography and dense vegetation) and the need for secure locations in this heavily populated area. A couple of weeks ago, we wrote in this column about the innovative and successful NetQuakes Initiative, in which homeowners volunteer to host a seismometer, allowing much more data to be collected for seismic monitoring and research.
While the seismic network in lower Puna has been modestly improved through new NetQuakes instrumentation, our deformation monitoring efforts in lower Puna have suffered serious blows recently due to theft and vandalism at key sites.
Within the last year, two stations that housed borehole tiltmeters — instruments that very precisely measure the slope of the ground and transmit their data to the observatory in real time — were stripped of their solar panels, batteries and radio communication equipment.
At one site, even the tiltmeter itself was lifted out of the ground and taken. This instrument would cost about $13,000 to replace (not counting installation costs) but it’s hard to imagine that it’s worth more than the cost of scrap metal to the thieves.
The cost of the stolen materials is well over $40,000. The addition of our costs in planning, installing, and trying to protect these sites raises the cost of the thefts to the taxpayers to at least $100,000. The thefts have been reported to Hawaii County police and the FBI.
More important than the monetary cost, however, is the gap left in our deformation monitoring network on the lower east rift zone. It’s clear that we can’t continue to maintain sites in isolated, unsupervised areas.
Inspired by your willingness to take part in the NetQuakes program, we again ask for your help. Instead of installing more tiltmeters, however, which are prohibitively expensive and would require drilling boreholes, we would like to find homes, actually yards, for GPS instruments. GPS is well-suited to monitor the subtle changes of the ground, as we can process the data at the observatory to track the position of the GPS antenna to within a centimeter (less than half an inch).
GPS instruments use satellites to accurately determine their position. Thus, the main requirement for a GPS installation is to have an unobstructed view of the sky. Clearly, full unobstructed views are unlikely in Puna; however; the instruments do need to be able to see the sky at an angle of least 50 degrees down from straight overhead in most directions, and more in some directions. The site needs to be at least 30 feet from structures, like one-story houses and in an area that will remain undisturbed under normal circumstances. In order to get the data back to HVO, we would need either a good cell phone reception or line-of-sight views to Mauna Kea or Pu‘u Honua‘ula.
The whole setup fits within a 5-foot by 5-foot area with nothing higher than the 5-foot antenna. It would take us about half a day to install it, and we would need to service it, on average, about once per year.
If this sounds interesting and you would like to be part of the effort to monitor and contribute to research in understanding Kilauea Volcano, please give HVO a call at 967-8804.
Kilauea activity
update
A lava lake within the Halema‘uma‘u Overlook vent produced nighttime glow that was visible from the Jaggar Museum overlook and via HVO’s Webcam during the past week. The lake level over the past week fluctuated, due to deflation-inflation cycles, and was generally 165-200 feet below the floor of Halema‘uma‘u. On Kilauea’s east rift zone, breakouts from the Peace Day tube remain active above the pali and on the coastal plain. Small ocean entries are active on both sides of the Hawaii Volcanoes National Park boundary. The Kahauale‘a flow is no longer active, its front stalling about 3 miles northeast from Pu‘u ‘O‘o.
There was one felt earthquake in the past week. On Thursday, April 25, 2013, at 2:21 a.m., HST, a magnitude-3.1 earthquake occurred 4 miles north of Mountain View at a depth of 1 mile.
Visit the HVO website (http://hvo.wr.usgs.gov) for Volcano Awareness Month details and Kilauea, Mauna Loa, and Hualalai activity updates, recent volcano photos, recent earthquakes, and more; call 967-8862 for a Kilauea summary; email questions to askHVO@usgs.gov.
Volcano Watch (http://hvo.wr.usgs.gov/volcanowatch/) is a weekly article and activity update written by scientists at the U.S. Geological Survey’s Hawaiian Volcano Observatory.