Just over a month ago, the Hawaiian Volcano Observatory (HVO) raised the curtain on its new website. The change was part of an overall update to how the U.S. Geological Survey’s (USGS) Volcano Hazards Program provides information to both the
Just over a month ago, the Hawaiian Volcano Observatory (HVO) raised the curtain on its new website. The change was part of an overall update to how the U.S. Geological Survey’s (USGS) Volcano Hazards Program provides information to both the scientific community and the general public.
The new HVO website (https://volcanoes.usgs.gov/hvo/) provides a portal to a wide range of information about the two ongoing Kilauea eruptions and current unrest on Mauna Loa. Other Hawaiian volcanoes are also featured on the website, including the island chain’s youngest and still submarine volcano, Loihi.
Somewhat coincident with the debut of HVO’s updated website, eagle-eyed web surfers have noticed recent increases in earthquake activity at Loihi. Although we have no seismic stations near Loihi, which is centered 24 miles southeast of Pahala in Hawaii County’s Ka‘u District, HVO has been tracking earthquake activity there from land-based seismic stations for over 50 years.
Indeed, since the end of February 2017, HVO seismic analysts have noted a slight uptick in the numbers of earthquakes near Loihi. From January 2015 through February 2017, there was, on average, one located Loihi earthquake per month. Since then, the rate of earthquakes has gradually increased. This month alone (as of June 22), there have been 51 located earthquakes in the Loihi region.
Without permanent seismic stations at Loihi — because the highest point of the volcano is still 0.6 miles underwater — it is not possible to locate earthquakes there as accurately as we can at Kilauea or Mauna Loa. However, we can state that the June 2017 earthquakes appear to be clustered roughly 6–7 miles below sea level and extend from beneath the summit region of Loihi to the south.
Interestingly, the roughly 170 earthquakes located in the area of Loihi between 2010 and 2016 occurred away from the summit region. They were primarily beneath the northern flanks of Loihi, and extended to significantly greater depths below the volcano. The significance of this difference is unclear.
As early as 1952, HVO scientists interpreted occasional earthquake swarms in the Loihi region as reflecting active volcanism there. In fact, the earthquakes were key to recognizing that the seamount is actually an active volcano!
Earthquake activity alone does not conclusively indicate that Loihi is erupting. But the locations of recent earthquakes directly beneath the volcano’s summit region plausibly suggest magmatic or volcanic origin, such as adjustments within the magma reservoir or volcanic edifice. We would, however, expect to see many more earthquakes associated with an eruption.
The most recent confirmed eruption of Loihi occurred in 1996. That year, an energetic earthquake swarm began in July and quickly intensified, motivating a scientific expedition to Loihi to seize an unprecedented opportunity to possibly observe a submarine eruption. Thousands of earthquakes, including over a dozen with magnitudes greater than 4.5, were recorded from beneath the summit and south flank of the volcano between July and September 1996.
Subsequent viewing and mapping of the Loihi summit region showed that, consistent with magma movement from beneath the summit area, a significant portion of it had collapsed. Fresh pillow lavas and glassy fragments collected during submersible dives also confirmed the occurrence of an eruption.
Because Loihi is still so deep beneath the ocean’s surface, the USGS regards Loihi as a low- to very low-threat volcano. Thus, there are no immediate plans for additional monitoring instruments and our views of Loihi for the foreseeable future will be strictly seismological.
Volcano Activity Updates
This past week, Kilauea Volcano’s summit lava lake fluctuated in concert with summit inflation and deflation, with levels ranging 22–40 m (72–130 ft) below the vent rim. On the East Rift Zone, the 61g flow remained active, with lava entering the ocean near Kamokuna. The new lava delta is approximately 3.2 acres in size, extending about 100 m (328 ft) from the sea cliff. Scattered surface breakouts continue on the upper flow field just downslope of Pu‘u ‘Oo. The 61g flows do not pose an immediate threat to nearby communities.
Mauna Loa is not erupting. During the past week, only a few small-magnitude earthquakes occurred beneath the volcano, primarily in the south caldera and upper Southwest Rift Zone at depths less than 5 km (3 mi). A few earthquakes also occurred on the west flank of the volcano at depths of 0–13 km (0–8 mi). GPS measurements continue to show deformation related to inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone. No significant changes in volcanic gas emissions were measured.
Two earthquakes were reported felt on the Island of Hawaii during the past week. On June 21, at 10:09 a.m. HST, a magnitude-4.5 earthquake occurred 28 km (17 mi) southeast of Hawaiian Ocean View at 38 km (24 mi) depth. On June 19, at 06:43 a.m. HST, a magnitude-2.5 earthquake occurred 9 km (6 mi) southeast of Leilani Estates at 0 km (0 mi) depth.
Please visit the HVO website (https://volcanoes.usgs.gov/hvo) for past Volcano Watch articles, Kilauea daily eruption updates, Mauna Loa weekly updates, volcano photos, recent earthquakes info, and more. Call for summary updates at 967-8862 (Kilauea) or 967-8866 (Mauna Loa). Email questions to askHVO@usgs.gov.
Volcano Watch (http://hvo.wr.usgs.gov/volcanowatch/) is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists.
