Shortly before midnight on July 5, 1975, Mauna Loa Volcano awakened with a shudder. Quickly responding to a seismic earthquake/tremor alarm at 11:18 p.m., USGS Hawaiian Volcano Observatory (HVO) staff rushed to their offices, where, at 11:42 p.m., they noted red glow above the mountain. The 1975 eruption lasted less than a day, but it ended Mauna Loa’s then longest-known repose period.
The post-World War II years had brought gradual improvements to HVO’s volcano monitoring network, including a seismic station at the rim of Moku‘āweoweo, Mauna Loa’s summit caldera. This station was the first to radio its signal from the summit area to HVO for review.
For many years, HVO’s seismic monitoring began with the scan of seismograms to compile daily counts of earthquakes in key regions of the volcanoes. For sufficiently well-recorded earthquakes, locations—or hypocenters—were also computed, as they are now, to help describe the earthquake and volcanic processes in greater detail.
In April 1974, more than a year before the 1975 eruption, HVO staff noted a clear increase in the daily earthquake counts beneath Mauna Loa. An initial flurry of earthquakes extended into mid-May, when earthquake counts dropped, but still persisted above the April daily averages.
In late July 1974, Mauna Loa earthquake activity abruptly returned, and the rate increased to hundreds of detected earthquakes per week. Then, from August 1974 to the July 5-6, 1975, eruption, counts of hundreds of earthquakes per day were consistently compiled. Geodetic measurements spanning the summit of Mauna Loa in August 1974 and June 1975 were consistent with volcanic inflation.
Complementing the 1974 and 1975 earthquake counts, the hypocenters showed that Mauna Loa earthquakes were generally clustered beneath Moku‘āweoweo, the volcano’s Southwest Rift Zone, and 5-6 km (3-4 mi) west of the summit. The western group was somewhat deeper than the two other clusters.
Though lacking in the detail and precision available to us now, HVO’s observations in August 1974 would have likely resulted in an upgrade of Mauna Loa’s Volcano Alert Level and Aviation Color Code to Advisory and Yellow, respectively—had the USGS Alert-Notification System for Volcanic Activity existed at that time (the system was established in 2006; more info click here. Persistent, though fluctuating, rates of hundreds of earthquakes each week would arguably have sustained an upgraded classification through the fall of 1974.
As early as 1915, HVO scientists had postulated relationships between Mauna Loa eruptions and moderately strong, possibly precursory, flank earthquakes. On November 30, 1974, such an earthquake, magnitude-5.4, occurred in the Ka‘ōiki fault system beneath Mauna Loa’s southeast flank.
That earthquake alone might not have warranted elevating Mauna Loa’s Volcano Alert Level and Aviation Color Code from Advisory/Yellow to Watch/Orange, but, over three days in early December 1974, earthquake counts jumped from 100-200 to over 1,000 per day.
On December 15, a shallow magnitude-4.6 earthquake occurred beneath Moku‘āweoweo and daily earthquake counts peaked at 1 per minute (1491 per day). The size and location of the M4.6 earthquake and the extremely high counts might well have encouraged raising Mauna Loa’s status to a Watch/Orange designation.
A second shallow magnitude-4 earthquake struck beneath Mauna Loa’s southeast summit region on March 26, 1975. Thereafter, an apparently accelerating rate of shallow magnitude-3+ earthquakes beneath the summit would have provided additional basis to change the Volcano Alert Level and Aviation Color Code prior to the eventual eruption in July.
In late spring 1975, HVO staff members Bob Koyanagi, Elliott Endo, and Jennifer Ebisu (Nakata) circulated a paper that described their observations and announced Mauna Loa’s reawakening. In their world, without Internet and USGS Volcano Activity Notices, among many other differences compared to now, their paper appeared in print in September 1975, after the eruption.
Modern monitoring strategies have improved HVO’s ability to recognize and act upon clear precursors leading to Mauna Loa’s next eruption. We understand however, that while building toward its next eruption, the volcano will not necessarily follow the same patterns noted in connection with earlier eruptions.
HVO continues to carefully track volcanic and seismic activity on Mauna Loa, Kīlauea, and other active Hawaiian volcanoes, and will issue appropriate notifications based on the best information available to us.
Volcano Activity Updates
Kῑlauea Volcano is not erupting and its USGS Volcano Alert level remains at NORMAL. For definitions of USGS Volcano Alert Levels.
Rates of deformation, gas release, and seismicity on Kīlauea have not changed significantly over the past week.
Deformation at Kīlauea’s summit has been consistent with slow magma accumulation within the shallow portion of the summit magma system. However, gas measurements have not indicated shallowing of large volumes of magma.
On Kīlauea’s East Rift Zone, deformation continues to show motions consistent with slowed refilling of the deep magmatic reservoir in the broad region between Puʻu ʻŌʻō and Highway 130.
The south flank of Kīlauea continues to creep seaward at elevated rates following the May 4, 2018, M6.9 earthquake near Kalapana. Elevated rates of motion on faults after a large earthquake are common and are not cause for alarm.
Real-time sulfur dioxide emission rates are low at the summit and are below detection limits at Puʻu ʻŌʻō and the Lower East Rift Zone.
Three earthquakes with three or more felt reports occurred in Hawaiʻi this past week: a magnitude-2.9 quake 13 km (8 mi) southwest of Leilani Estates at -0 km (-0 mi) depth on July 6 at 08:07 a.m. HST; a magnitude-3.4 quake 6 km (4 mi) south of Volcano at 30 km (19 mi) depth on July 3 at 06:48 p.m. HST; and a magnitude-3.8 quake 5 km (3 mi) south of Volcano at 30 km (19 mi) depth on July 3 at 06:35 p.m. HST.
Hazards remain at the lower ERZ and summit of Kīlauea. Residents and visitors near the 2018 fissures, lava flows, and summit collapse area should heed Hawai‘i County Civil Defense and Hawaiʻi Volcanoes National Park closures and warnings. The 2018 lava flows are primarily on private property, and people are asked to be respectful and to not enter or park on private property.
The USGS Volcano Alert level for Mauna Loa was changed on July 2, 2019, to ADVISORY, because, for the past several months, earthquake and ground deformation rates at the volcano have exceeded long-term background levels. This increase in alert level does not mean that an eruption is imminent nor that progression to an eruption is certain. A similar increase in activity occurred between 2014 and 2018 and no eruption occurred.
Seismicity on Mauna Loa remains elevated, with an average of at least 50 shallow small-magnitude earthquakes per week following an earthquake swarm in October 2018. This compares to a rate of fewer than 20 earthquakes per week beneath the volcano in the first half of 2018.
Deformation measurements show continued summit inflation, suggestive of renewed recharge of the volcano’s shallow magma storage system. This rate of inflation has not changed since the alert level was raised on July 2.
No significant changes in volcanic gas release on the Southwest Rift Zone were measured, and fumarole temperatures there and at the summit remain unchanged.
For more info on the status of Mauna Loa, click here.
HVO continues to closely monitor both Kīlauea and Mauna Loa for any signs of increased activity.
Photo caption: As the sun rose above Mauna Kea (background) on July 6, 1975, eruptive fissures along the Northeast Rift Zone of Mauna Loa fed voluminous ‘a‘ā lava flows that quickly moved down the north flank of the volcano. USGS photo by D. Peterson.
Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.