#Volcano #MaunaLoa After a 30-year repose, Mauna Loa may be slowly stirring to life. While there are no signs of impending eruption, the Hawaiian Volcano Observatory has recorded an increased level of seismic activity on the flanks and summit of Mauna Loa over the past 13 months. Four distinct earthquake swarms — clusters of earthquakes occurring closely in time and location — have occurred since March 2013. Each swarm began with earthquakes northwest of the summit (Moku‘āweoweo Crater) at 4 to 15 km (2.5-9 mi) deep, followed by shallow earthquakes at the summit from several days to one month later. These earthquakes have all been less than magnitude-2.2, except for a magnitude-3.5 earthquake on May 9, 2014. The recent swarms have not been associated with the deformation of the ground surface that we would expect from intrusion of significant amounts of magma into shallow levels beneath Mauna Loa. However, ground deformation indicating shallow magma accumulation has been measured during many of the past 30 years, including two episodes of very rapid inflation immediately following the most recent eruption in 1984, and again from 2004-2006. The latter inflation started with a swarm of deep, long-period earthquakes at 45 km (28 mi) under the volcano. Prior to the 1984 eruption, seismicity was elevated for at least three years, with 28 earthquakes greater than magnitude 3, and 2 earthquakes greater than magnitude 4. The magnitude-6.7 earthquake on November 16, 1983, may also have been triggered by the pressurizing magma system of Mauna Loa. Earthquakes prior to the 1984 eruption were typically located northwest of the summit at depths greater than 5 kilometers (3 miles) and on the upper Southwest Rift Zone at depths less than 5 km (3 mi). The seismic network that monitors Mauna Loa has been significantly improved since 1984. As part of the American Recovery and Reinvestment Act in 2011, all of the seismic stations in the HVO seismic network were upgraded to use technology that results in less noise and better recordings. The current seismic network is better able to detect and locate smaller earthquakes than the network prior to these upgrades. It is likely that many of the small earthquakes that we currently observe would not have been detected by HVO’s seismic monitoring prior to the 1984 eruption. Though the size and number of earthquakes observed over the past 13 months has been significantly smaller than those observed in the three years prior to the 1984 eruption, they have been occurring in the same general areas of the volcano. More at link!
Posted on: Sun, 15 Jun 2014 20:56:44 +0000
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