A Look Back at the Earthquake that Devastated Ka‘ū 150 Years Ago

Destruction caused by the 1868 great Ka‘ū earthquake included the Wai‘ōhinu church, shown here, in the Ka‘ū District of Hawaiʻi Island. With a magnitude estimated at 7.9, the earthquake is the largest in Hawaiʻi’s recorded history. Photo by Henry L. Chase, published in “Volcanoes of Kīlauea and Mauna Loa on the Island of Hawaiʻi” by W.T. Brigham, Bishop Museum Press, 1909.

This week marks 150 years since the largest earthquake to strike Hawai‘i in the last two centuries. Estimated to have been at least magnitude 7.9, this earthquake struck near Pāhala in the Ka‘ū District of the Island of Hawaiʻi on April 2, 1868.

Known as the great Kaʻū earthquake, the event had the same maximum intensity as the 1906 San Francisco earthquake, defined as “extreme shaking” on the Modified Mercalli Intensity Scale. It was felt as far away as Kauaʻi and stopped clocks on Oʻahu. In Kaʻū, where people were bounced like balls from shaking that went on for several minutes, the destruction was nearly total. Stone buildings and walls were destroyed as far away as Hilo.

The shaking caused landslides from Kaʻū to Hawaiʻi Island’s northern Hāmākua coast and induced a small eruption on Kīlauea Volcano’s Southwest Rift Zone. A mudslide in Wood Valley north of Pāhala buried 31 Hawaiians. A tsunami, consisting of at least eight waves over several hours, was estimated to be more than 20 feet high in Kaʻū. The waves caused damage from South Point (Kalae) to Cape Kumukahi (Kapoho), destroyed more than 100 structures, and took 47 lives.

If it happened today, the great Kaʻū earthquake would be one of the world’s strongest earthquakes of this past year. Its size would also rival two of the most deadly events of the past decade: the magnitude 7.8 Nepal earthquake, which killed more than 8,000 people on April 25, 2015, and the magnitude 7.9 Sichuan (China) earthquake, which killed nearly 90,000 people on May 12, 2008. Because the island of Hawai‘i was sparsely populated in 1868, the loss of life from the Ka‘ū earthquake was limited.

In Hawai‘i, the most destructive earthquakes occur along a gently sloping fault between the base of the volcanoes and the ancient ocean floor on which they are built. This fault, located at a depth of approximately 7 miles, is known geologically as a décollement, from the French word “décoller,” which means “to detach from.”

A large part of the island of Hawai‘i moved during the 1868 event. Based on measurements of how much the earth moved during Hawaiʻi’s magnitude 7.7 Kalapana earthquake in 1975, which also occurred on the décollement, the entire island south and east of Mauna Loa’s summit and rift zones moved seaward and subsided several yards during the great Kaʻū earthquake of 1868.

The April 2 great Kaʻū earthquake was part of a larger volcanic crisis that unfolded over 16 days. On March 27, an eruption quietly began in Mokuʻāweoweo, the caldera at the summit of Mauna Loa. Seismic activity increased through the day, and by the afternoon of March 28, a magnitude 7.0 earthquake occurred in Kaʻū, which caused extensive damage from its own very strong to violent shaking.

During the following four days, nearly continuous ground shaking was reported in Kaʻū and South Kona. Earthquakes continued at rates of 50 to 300 per day, including a magnitude 6.0 each day, leading up to April 2, when the great Ka‘ū earthquake, 15 times stronger than the magnitude 7.0 foreshock, occurred at 4 p.m. A severe aftershock occurred on April 4, and aftershocks of decreasing magnitudes continued for decades.

The great Kaʻū earthquake unlocked Mauna Loa’s Southwest Rift Zone, and on April 7, 1868, an eruptive fissure opened low on the mountain, just above today’s Highway 11 and east of Hawaiian Ocean View Estates. This eruption and the lava flows it produced will be the focus of next week’s Volcano Watch.

Though we do not know how often events as large as the great Kaʻū earthquake occur, we do know that, in Hawaiʻi, active volcanoes drive the stresses that generate the largest earthquakes. Mauna Loa’s hazards, therefore, include eruptions, as well as large earthquakes along the décollement in Kaʻū and South Kona—for example, the magnitude 6.9 earthquake that occurred near Captain Cook in 1951.

Because of this, Hawai‘i island residents are encouraged to be prepared for both volcanic eruptions and potentially damaging earthquakes.

Volcano Activity Updates

This past week, Kīlauea Volcano’s summit lava lake level fluctuated with summit inflation and deflation, ranging about 75–115 feet below the vent rim. On the East Rift Zone, the 61g lava flow remained active with breakouts on the upper part of the flow field within 1.6 miles of Pu‘u ‘Ō‘ō. There were no active lava flows on the pali, coastal plain, or entering the ocean. The 61g flows do not pose an immediate threat to nearby communities.

Mauna Loa is not erupting. Rates of deformation and seismicity have not changed significantly over the past week, but persist above long-term background levels. Only a few small-magnitude earthquakes occurred beneath the volcano, primarily at depths shallower than 8 miles. GPS and InSAR measurements continue to show slow deformation related to inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone. No significant changes in volcanic gas release or fumarole temperature were measured.

One earthquake with three or more felt reports occurred in Hawaii this past week. On March 24, at 12:32 a.m. HST, a magnitude-2.5 earthquake occurred 2 miles southwest of Volcano.

Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.