June 29: New Ways to Watch Changes at the Summit

Today’s Eruption Summary

Fissure 8 and the summit explosions continue their status quo. However, for the last few days, the lava flow at Kapoho has been encroaching on new areas on its northern and southern boundaries at the coast.

At least 3 more Kapoho Beach Lot houses have burned on the north side, and the southern edge of the flow is burning vegetation and/or farmland west of Highway 137. I gather these new lateral outbreaks are due to the lava channel crusting over, about half a mile inland from the new coastline (see Wednesday’s thermal map). So instead of pouring straight from the channel into the ocean, lava is fanning out under the crust of the 2-mile-wide lava delta laid down earlier this month, then oozing out the sides.

[USGS drone footage of Fissure 8 from before dawn. They’re using drones for the first time to map flows, look for outbreaks and measure the lava river’s speed.]

At Kilauea’s summit, today’s collapse explosion occurred at 7:51am HST, June 29, with an ash-poor steam plume that rose 500 feet. (Steam?)The energy release dropped slightly to 5.2. I didn’t do a video capture, since the summit was blanketed in morning fog.

The “new news” today is that HVO has added two new views to its Kilauea Webcams page. One I’ve mentioned before, the old “Kilauea East” webcam from HVO’s 1990s website which has annoying reflections but a great view of the subsidence/collapse on the east side of Halema’uma’u Crater:

June 25, 2018 screengrab from “Kilauea East” webcam.

The other is a new heat-sensitive webcam which should make it possible to see “collapse explosions” at night:

Screengrab of Halema’uma’u Thermal webcam at sunset, June 29.

Also, in this week’s “Volcano Watch” newsletter, Hawaiian Volcano Observatory scientists explain the “piston” model they’ve developed to account for the daily collapse explosions at the summit:

(See also the “Kilauea Earthquakes FAQ” they posted earlier this week.)

This is big news. They’ve solved the mystery of the summit explosions! Subject to revision, of course; they’re still untangling the complexities of Kilauea’s current eruption. But the “piston” model accounts for the cyclical pattern they’re seeing better than the “steam explosion” model.

Continue reading June 29: New Ways to Watch Changes at the Summit

June 27: Farm Animals Airlifted

Prelude

Here’s an excellent 13-minute retrospective of Kilauea’s eruptions from the early 20th century right through June 25, 2018.

Now back to the present.

Today’s Eruption Summary
USGS: “At 10:41 p.m. HST on June 26, after approximately 25 hours of elevated seismicity, a collapse explosion occurred at the summit producing an ash-poor steam plume that rose less than 1,000 ft above the ground surface before drifting to the southwest. The event was captured by an HVO webcam in moonlight (plume in bottom of photo), located in the HVO observation tower.” (Full-sized)

It’s 11:30pm HST, and it looks like today’s “collapse explosion” is going to happen tomorrow. Are the explosion spacing themselves out more now?  Too early to tell. There has been always some variation in their timing, despite the fact that it feels like we’re watching a magmatic equivalent of Old Faithful.

View of Fissure 8 cone and lava channel from USGS morning overflight. (Full-sized)

Meanwhile, Fissure 8 continues exactly what it has for— what, a month now? Fountains contained within its 180-foot spatter cone continue to pour out an 8-mile river of lava. Occasional spillovers near the head of the river usually don’t go past the margin of previous flows in this eruption. Fissure 22 is once again showing “incandescence” and pushing out small, short lava flows.

The ocean entry area fans out across a 1-km stretch of coast, but the bulk of the lava is dumping into the sea from Fissure 8’s main channel. Unfortunately, the northern margin of the lava flow has reactivated, too, pushing further into what’s left of Kapoho Beach Lots community.

USGS on Twitter: “Morning overflight revealed northern margin of flow field at the coast is oozing fresh #lava at several points in the area of #KapohoBeachLots. Small channel overflows feed short #pahoehoe flows.” (Full-sized)

USGS: “Lava continues to enter the sea along the southern Kapoho coastline. Lava enters the ocean primarily through an open channel, but also along a 1-km (0.6 mi) wide area. Also visible in the image (center right) is an area at the northern margin of the flow field that is oozing fresh lava at several points in the area of Kapoho Beach Lots.” (Full-sized)

And that’s about it. Except that even with status quo, there’s some unusual sights and itoday. Such as this literal “Lava boat”:

Continue reading June 27: Farm Animals Airlifted