Volcano Watch — Spatter erupted from the heart of the Koa‘e fault system at Kīlauea

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Seldom does one find evidence of an eruption where none was known before. We generally assume that Kīlauea erupts only at the summit or along its two rift zones. That view has to change, if only slightly, because of a discovery made on June 22, 2012.

In early June, a small earthquake swarm shook the west-central part of the Koa‘e fault system, which connects the east and southwest rift zones south of Kīlauea's summit. The Hilina Pali Road runs along the fault system from the Chain of Craters Road to Kulanaokuaiki Campground, where the road bends across a pali, escapes the fault system, and heads for Kīpukanēnē.

The earthquakes, centered 1–2 km (0.6–1.2 mi) west of the campground, were small, and no one examined the ground for new cracks until a marvelous InSAR image became available on June 21. This radar image, obtained from space, showed that significant ground deformation took place during the earthquakes.

On June 22, an HVO geologist examined the area on the ground and found many small new cracks. This was exciting, but the big news came when, at 11:15 a.m. and totally unexpectedly, he found tiny bits of spatter lying next to an older, pre-2012 crack. On July 5, similar material was found 700 m (765 yd) farther east along the same crack system.

Spatter is ejected during eruption, but no eruption was known in the fault system—until now. There's not much spatter but enough to tell that it was spit from a wide crack and mostly blown a few tens of meters southward by the trades.

The eruption was tiny, to judge from the two very limited areas in which spatter fell. But an eruption is an eruption, and this one tells us that a dike of magma must have been injected underground into the fault system between Kīlauea's rift zones.

How old is the newly discovered spatter? It did not erupt during the early June earthquake swarm; it is too discolored and otherwise modified to be so young. It was erupted within the past 220 years, because it fell onto volcanic ash formed in 1790. Chemical tests are underway to compare it with lava erupted at known times since 1790. We hope to find some resemblance that will help date the eruption.

Magma intrusion into the Koa‘e had been previously suggested. Earthquakes in 1973, and probably also in 1965, propagated westward into the fault system from an eruption site on the east rift zone, as if magma were moving underground. Also in 1973, surveying at three places across the fault system showed that the ground was arched up along what was thought to be a dike. Two geophysical surveys likewise suggested that magma intruded a short distance into the Koa‘e in 1973.

These interpretations were all reasonable, but no smoking gun—volcanic ejecta—had been found. It still hasn't been found for the 1973 and 1965 events, but now we know that magma did intrude and erupt in the fault system at least once since 1790. This makes it likely that the interpretations of magma intrusion in 1973 (and probably in 1965) are correct.

The recognition of dikes in the fault system helps explain two puzzling observations. Given all the open cracks in the Koa‘e, why isn't the earth's gravitational field warped? With less rock mass, gravity should be weaker than elsewhere. But if many of the cracks are filled with solidified magma at shallow depth, there would be little mass deficit and no gravity anomaly.

The fault system is a barrier to seaward groundwater flow. With open cracks, one would think the reverse would be true. Dikes in the Koa‘e, filling cracks underground, might form natural barriers to water flow, as happens elsewhere in Hawai‘i.

The emerging picture is that magma can intrude and occasionally erupt in the Koa‘e fault system during eruptions at adjacent parts of the east rift zone, between Hi‘iaka and Mauna Ulu. Can magma in the southwest rift zone also intrude the fault system? Does there even have to be an accompanying eruption in a rift zone?

The two spatter discoveries have triggered new questions about the Koa‘e fault system, an important but often overlooked part of Kīlauea.

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Volcano Activity Update

A lava lake within the Halema‘uma‘u Overlook vent resulted in night-time glow that was visible from the Jaggar Museum overlook and by HVO's Webcam during the past week. The lake level fluctuated slowly between about 60 to 80 m (200–260 ft) below the floor of Halema‘uma‘u Crater, matching cycles of summit inflation and deflation. There were also several rise-fall cycles, during which the level fluctuated more rapidly.

On Kīlauea's east rift zone, surface lava flows on the coastal plain and pali have been relatively weak over the past week. As of Wednesday, August 8, the active flow front was more than 2 km (1.2 miles) from the ocean. There was no active ocean entry. Incandescence was visible from three degassing vents within Pu‘u ‘Ō‘ō, including the pit on the northeastern side of the crater floor that has held a small lava pond. The lava pond was too low to be directly visible via webcam.

One earthquake was reported felt on the Island of Hawai‘i during the past week. On August 4th at 3:20 p.m., HST, a magnitude-3.1 earthquake occurred to 14 km (9 mi) to the WSW of Waiki‘i at a depth of 17 km (11 mi).