July 3 Steve Brantley Slideshow at Pahoa Meeting

[Note: this is when the overflows around Kapoho Crater got started, but the main flow front/ocean entry was still mostly north.]

I was hoping NLTV would post a video of last Tuesday evening’s Pahoa Community meeting as they usually do, since BigIslandVideoNews records Steve Brantley’s slideshows by pointing the camera at him and skipping most of the slides, but no such luck.

BIVN posted various excerpts of the meeting, including these non-geology segments: Live poll, Hwy 130 Reopening Discussed, Residents question Civil Defense. 

Here’s Steve Brantley’s USGS presentation:

Transcript

Steve Brantley, Deputy Scientist-in-Charge of HVO:

Continue reading July 3 Steve Brantley Slideshow at Pahoa Meeting

July 10: Regrouping After Yesterday’s Overflows

USGS: “View from Bryson’s quarry around 11:45 p.m. HST last night looking uprift past Halekamahina (an older ash cone) to fissure 8, which is creating the glow behind the cone. Bright areas indicate incandescent lava, with the brightest areas showing the trace of the lava channel. A blockage in the channel produced overflows that are seen as spotty incandescence. Lava flows in the foreground are near the base of the quarry cinder pit.” (Full-sized)
Today’s Eruption Summary

The chaos of yesterday has settled down a bit. Stormy weather has moved out, most of the overflows up-channel from Kapoho Crater have stopped, and lava is has returned to the main channel leading to the ocean, although not at the same volume as before. Yesterday’s breakout flow towards Cinder Road stalled last night. As of 4AM this morning, the only overflows still active were on the south (brown) side of the lava channel, including a new side-flow on the west side of Kapoho Crater (ocean is in the background haze):

July 10, 2018, morning overflight. USGS: “Aerial view of Kapoho Crater looking toward the south-southeast. Part of the lava channel became blocked just upstream of Kapoho Crater yesterday, diverting flows to the west and then south around the crater (center right). Lava exiting a crusted section of the channel continued flowing in the channel pathway (lower center to left).” (Full-sized)

It sounds like the southern edge of the ocean entry area has stalled too, giving Ahalanui Pond a respite (although the lava’s very, very close). But the northern side has continued to ooze as well. Today’s report from the mayor’s office said two of the the three remaining Kapoho Beach Lots homes were lost to lava in the past day or so.

There’s still multiple “ooze out” fingers along the edge of the delta in addition to the main channel. And Fissure 22 continues to sputter weakly.

July 10, 2018. USGS: “Fissure 8 and a full lava channel as seen during HVO’s early morning overflight. The visible road is Nohea Street in the Leilani Estates subdivision. Steam generated from heated rain water rose from the tephra deposits and lava flows surrounding fissure 8.” (Full-sized)

As of 10pm HST, we’re still waiting for the next collapse/explosion at the summit. (Should we be calling them explosions any more, or just collapses?)

In the meantime, the USGS has updated the caldera subsidence timelapse from Keanakāko‘i Overlook:

Continue reading July 10: Regrouping After Yesterday’s Overflows

June 9: Fissure 8 Rearranges the Furniture

July 9, 2018. USGS: “Lava entering the ocean as seen through steam and rain early this morning.” (Full-sized)
Today’s Eruption Summary

Wild weather, overflows and significant channel reorganization have made the Lower East Rift Zone more interesting today than those living near Bryson’s cinder pit would like.

July 9, 2018. USGS: “This photograph taken during this morning’s overflight shows heavy, localized rain at fissure 8 in Leilani Estates.” (Full-sized)

Sunrise overflights by the USGS and @hotseathawaii spotted a torrential downpour centered directly over the upper lava flow (above). A rain gauge in Leilani Estates measured 9.22″ rainfall at 7am for the past 24 hours; another just a little farther away measured 6″ over the same span. All that updraft, convection and condensation even produced a modest… lavaspout…? captured on video (strong language warning):

The Kapoho end of the LERZ eruption was even more chaotic. Over the weekend, several non-USGS sources had reported that lava was starting to shift back to the south after passing Kapoho Crater, forming a slow-moving flow headed for Ahalanui Ponds (and sparing 3 of the 4 remaining Kapoho Beach Lots houses). This morning, HVO status updates confirmed the change: “The main lava channel has reorganized and is nearly continuous to the ocean on the south side of the flow, expanding the south margin by several hundred meters.” Also, while the ocean entry was still a very broad 2.5 mile front at sunrise, it’s started to coalesce a bit and shift towards the south:

July 9, 2018 (later in the morning; can’t be afternoon because of sun position). USGS: “Sourthern end of the active fissure 8 flow margin north of the Analannui Park [sic], known as the warm ponds. The flow margin is estimated to be about 500 m (0.3 mi) from the park.” (Full-sized)
However, blockages in the braided section of the lava river caused further havoc later in the day. HVO’s afternoon status update reported that, “Early this afternoon, observers reported multiple overflows occurring along both sides of the main lava channel, in an area extending from near the ‘Y’ intersection at Pohoiki Road eastwards to an area just west of Kapoho Crater. Overflows on the upper part of the channel did not extend beyond areas previously covered in lava. Overflows further down the channel have reached beyond the flow field, including one flow lobe that is moving northeast from the main channel towards Cinder Rd.”

July 9, 2018. USGS: “The lower section of the fissure 8 lava channel appears to be almost completely crusted over, and the lava level in the channel was lower during this morning’s overflight.” (Full-sized)

[HVO afternoon status update cont’d] “Based on information from ground observers and morning and afternoon overflights, the lower part of the main lava channel has undergone significant reorganization. In particular, the channel that had been open near Four Corners is now mostly crusted over, and plumes from ocean entry are significantly reduced. It is likely this is due to a blockage that formed in the early morning in the main channel upstream of Kapoho Crater. Flow volumes coming out of Fissure 8 remain significant, and it is possible that changes in flow channels will continue to occur in the coming days.”

Meanwhile, up at the summit, it’s business as usual. This morning’s collapse event occurred at 9:20am, registering once again as 5.3:

USGS posted yesterday’s thermal map first thing this morning, plus a 2pm map today showing these changes:

Continue reading June 9: Fissure 8 Rearranges the Furniture