Volcano Watch — Jaggar's prediction comes true—the 1935 eruption of Mauna Loa

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After working for 20 years building the Hawaiian Volcano Observatory (HVO), Thomas Jaggar had achieved almost everything he set out to do. He had directed continuous observations of Kīlauea Volcano, installed seismic monitoring instruments at four locations around the Island of Hawai‘i, and published these findings regularly. His budget for the fiscal year 1931–1932 from the U.S. Geological Survey (USGS) was his largest ever—$35,000.

But these were the years of the Great Depression. Over the next two years, HVO's budget was slashed to $6,000, forcing a reduction in publishing and requiring supplemental funding from HVO's private funding source, the Hawaiian Volcano Research Association (HVRA), to pay salaries.

While government funding was being cut, volcanic and seismic activity on Hawai‘i did not diminish. In late 1933, a six-week-long swarm of earthquakes culminated in a 17-day-long eruption within Moku‘āweoweo, the summit caldera of Mauna Loa. Almost a year later, Halema‘uma‘u Crater at the summit of Kīlauea erupted for a month.

On March 26, 1934, Jaggar gave a bold speech titled "The Coming Lava Flow," in which he predicted—based on analyses of 60 years of Mauna Loa eruptions—that "A lava flow from Mauna Loa, or else another summit eruption, is expected within two years." He further predicted that, if it was a Mauna Loa lava flow, it would break out along the Northeast Rift Zone and flow in the "likely direction" of Hilo.

Jaggar also pointed out that, despite the coming lava flow, HVO had been reduced to two staff, including himself. He further campaigned for increased membership in HVRA to hopefully make up for the federal funding cuts.

The HVRA funding did not come, and, as of July 1, 1935, HVO was transferred from the USGS to the National Park Service under what was then known as Hawaii National Park (HNP). While this looked like defeat for Jaggar, it may have been a blessing.

Edward G. Wingate, a USGS topographical engineer, had worked at HVO for two years before being selected as HNP Superintendent in November 1933. After HVO was transferred to the Park, he was able to provide Jaggar with additional staff and funds when needed. So, when Mauna Loa erupted on November 21, 1935, as Jaggar had predicted, Wingate directed Park staff to the eruption site to make observations and relay information to HVO.

The 1935 Mauna Loa eruption started from a 6.4-km- (4-mi-) long fissure that extended from the summit caldera down the Northeast Rift Zone. Several lava flows moved northward down the flank of the volcano toward the Saddle area between Mauna Loa and Mauna Kea.

Contrary to Jaggar's prediction, these flows would probably flow toward Kona if they continued, not toward Hilo. Still, Jaggar's predicted time frame and location of the eruption source were spot-on.

But then, on November 27, smoke was observed from a patch of ground east of the 1935 lava flows, well away from the Northeast Rift Zone, at the 2,590 m (8,500 ft) elevation. ‘A‘ā lava (later called the Humuula flow) soon issued from that location and flowed north into the Saddle area. It stalled, but was followed by a pāhoehoe flow that ponded in a flat area between Mauna Loa's 1843 ‘a‘ā flow and Pu‘uhuluhulu, an ancient cinder cone.

After ponding for two weeks, the Humuula flow began moving and advanced eastward past Pu‘uhuluhulu. The increasingly steep slope resulted in a narrow flow advancing at an alarming rate of 1.6 km (1 mi) per day.

Fearing that the flow would reach the headwaters of the Wailuku River, which supplied water for the town of Hilo, Jaggar called on the Army Air Service on December 22 to bomb the lava flow source. His hope was that the lava tubes or channels could be destroyed, robbing the advancing flow to feed another flow that would re-cover the same area. The flow was bombed on December 27 and the flow stopped during the night or early morning of December 30-31.

Despite severely reduced funding and staffing, Jaggar made an important and successful prediction based on Mauna Loa's past pattern of eruptions. Whether or not the bombing caused the 1935 lava flow to stop is still a controversial topic.

Volcano Activity Update

Kīlauea continues to erupt at its summit and East Rift Zone. During the past week, in concert with summit inflation and deflation, the summit lava lake level varied between about 16 m and 36.5 m (52–120 ft) below the vent rim within Halema‘uma‘u Crater. On the East Rift Zone, the "61g" lava flow continued to enter the ocean. The lava flow does not pose an immediate threat to nearby communities.

Mauna Loa is not erupting. Seismicity remains elevated relative to the long-term background rate, with earthquakes occurring mostly in Mauna Loa's south caldera and upper Southwest Rift Zone at depths less than 5 km (3 mi). Global Positioning System (GPS) measurements show deformation related to inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone, with inflation occurring mainly in the southwestern part of the magma storage complex. 

Four earthquakes were reported felt on the Island of Hawai‘i this past week. On September 7, 2016, at 2:03 p.m., HST, a magnitude-2.7 earthquake occurred 1.6 km (1.0 mi) southwest of Kīlauea's summit at a depth of 1.1 km (0.7 mi). On September 6 at 4:25 a.m., a magnitude-4.0 earthquake occurred 3.6 km (2.2 mi) south-southeast of Mauna Loa's summit at a depth of 1.2 km (0.7 mi). On September 3 at 8:05 p.m., a magnitude-3.3 earthquake occurred 5.1 km (3.2 mi) southeast of Waimea at a depth of 14.9 km (9.3 mi). On September 1 at 12:11 a.m., a magnitude-3.7 earthquake occurred 25 km (15.5 mi) southeast of Waimea at a depth of 24.6 km (15.3 mi).