August 27: After Fire, Flood (Hurricane Lane)

August 22, 2018. USGS: “Parts of Kīlauea’s caldera floor are now a jumble of down-dropped blocks and surface cracks. HVO field crews carefully hiked along Crater Rim Drive yesterday to verify the locations of USGS benchmarks (lower left), which will be used for additional geophysical work that will help document the recent summit changes. The view is to the northwest with one flank of Mauna Loa visible in the distance (upper right).” (Full-sized)
Weekly Eruption Summary

After a busy few months, Kilauea continues to rest with only a pilot light on, so to speak. This week’s big news was that Hurricane Lane passed offshore of the Big Island on Thursday through Saturday, causing extensive flash flooding. But there’s still a little news to report on the dying (?) embers of Kilauea’s 2018 eruption.

On Friday morning, the Hawaii County Fire Department observed a small lava pond still visible deep in Fissure 8’s cone. For most of the week, there was no visible activity apart from a few small jets deep in the cone throwing weak spatter on Monday morning:

August 20, 2018. USGS: “This morning, USGS scientists flying over fissure 8 noticed a change in the vent from yesterday. Gas jets were throwing spatter—fragments of glassy lava (light gray deposits)—from small incandescent areas deep within the cone. This activity is an indication that the lower East Rift Zone eruption may be paused rather than pau (over).” (Full-sized)

The sputtery jets proved to be temporary:

August 21, 2018. USGS: “Southward facing aerial view of the fissure 8 cone. The two small areas of incandescence, gas jetting, and spatter from yesterday photograph appeared crusted over today.” (Full-sized)

Down at the ocean at Kapoho, there were a few weak dribbles of lava continuing to drain out of the delta at the beginning of the week:

August 20, 2018. USGS photo of residual lava entering ocean, posted on their facebook page here.

Sulfur dioxide emissions continue to be very low both at the summit and the coast. In fact, on Tuesday, they dropped too low in the Lower East Rift Zone for instruments to measure, although not too low for highly-sensitive human noses to detect.

Video from August 17 posted on the 20th— full-sized version here.

Heavy rain from Hurricane Lane on Friday and Saturday put a hold on USGS overflights and field observations and knocked out a few sensors on the east side of the island. But Kilauea’s extensive sensor network means there was no gap in volcano monitoring, and field crews were on call just in case.

The hurricane had no impact on the volcano apart from heavy rainfall hitting hot rocks and turning to steam in Pu’u O’o’s crater and on the not-yet-cooled lava flows of the LERZ. There were some reports of local white-out conditions from this steam. Rain may also have triggered a few rockfalls at the summit.

The other big Kilauea news this week is that Hawaii Volcanoes National Park has set a target reopening date for September 22, aiming to reopen at least the Visitor Center and (they hope) some kind of viewing area from which visitors will be able to see the new, larger Halema’uma’u Crater. They’re also hoping to open Volcano House, but they need to check the stability of the cliffs on which it stands.

USGS Volcano Watch

Whoops! I think I missed last week’s edition. This is Hawaiian Volcano Observatory’s weekly column with photos and in-depth information on some aspect of Kilauea.

Continue reading August 27: After Fire, Flood (Hurricane Lane)

August 5: Pele Taking It Easy This Week

“Since May 16, 2018, the crater depth has more than tripled and the diameter has more than doubled.” ~ HVO

Kilauea summit changes, 2018. USGS: “Here’s another ‘then and now’ look at Halema‘uma‘u (view is to north). At left, Halema‘uma‘u, as we once knew it, and the active lava lake within the crater are visible on April 13, 2018. At right is a comparable view captured on July 28, 2018, following recent collapses of the crater. The Hawai‘i Volcanoes National Park Jaggar Museum and USGS-HVO can be seen perched on the caldera rim (middle right) with the slopes of Mauna Loa in the background.” (Full-sized)
Current Eruption Summary

Volcanic activity has decreased over the past few days, at both the summit and down in the Lower East Rift Zone. However, as HVO warns us (and has stated many times), eruptions wax and wane, and can even stop and start up again. So we don’t yet know whether Pele’s winding down or simply taking a breather.

But for the moment, at least, Fissure 8 is putting out much less lava than before— in fact, this morning (August 5) its level is so far down that it’s barely feeding the channel. Lava levels were already lower and sluggish, and today the river is mostly crusted over and/or moving as thicker, crumbly a’a flows. However, blockages downstream are still causing overflows and breakouts.

“View of the fissure 8 cone and spillway from HVO’s overflight early this morning, during which geologists observed eruptive activity that was much less vigorous than in past days.” (Full-sized)

Despite the slowdown at the source, lava continues to ooze into the ocean along a long section of the southern flow front. It’s edged a little bit closer to the boat ramp and local park that’s become a symbol for residents mourning the loss of so many other beloved places:

August 5, 2018. USGS: ” A diffuse laze plume afforded a clear view of Isaac Hale Beach Park and the ocean entry, which was being fed across a broad front by viscous pāhoehoe. Lava was oozing laterally, but was still about 70 m (230 ft) southeast of the Pohoiki boat ramp as of this morning.” (Full-sized)

Lava tour boat operator Ikaika Marzo did not see any signs of slowdown at the flow front this morning, and he reported that lava has claimed claimed another popular local surf spot called “Dead Trees.”

At the summit, intervals between collapse events are lengthening. As of 5 pm August 5, it’s been over three days since the last summit collapse event. Today’s mini-update on HVO’s website states:

Rates of seismicity and deformation at summit and lava output from fissure 8 have decreased since most recent collapse event at 11:55 am HST August 2. Too soon to tell if the decrease will persist. Hazardous conditions remain.

Lower East Rift Zone USGS lava map as of 10 am, August 3. (Full-sized)
Friday, August 3 USGS Thermal Map of Lower East Rift Zone as of 12:30 pm. (Full-sized)
Latest Satellite Imagery

The most recent scenes, acquired on August 1, 2, and 5, show little overall motion, which is consistent with the slowing of deformation in the summit area over the past few days. — HVO

Kilauea Caldera satellite radar imagery, May 5-August 5, 2018. (Full-sized)
Volcano Watch, August 3

And on August 3— before today’s significant lava decrease at Fissure 8— HVO posted out its weekly Volcano Watch column:

Outline of the rest of this post:
  • Summary of USGS presentation at Thursday Volcano Village meeting
  • Review of USGS eruption images from past few days (plus video)
  • News and Kilauea-related information from other official agencies
  • Kilauea-related headlines from local news media
  • Overflight photos/videos of LERZ from @Hotseathawaii, etc
  • USGS Q&A about eruption (and recent signs of change) on social media

Continue reading August 5: Pele Taking It Easy This Week

July 17: New and Old Views of Halema’uma’u

July 17, 2018. USGS: “During this morning’s overflight, USGS scientists captured this image of sunrise above Kīlauea’s lower East Rift Zone. Fissure 8 continues to feed a channelized lava flow that reaches the ocean, forming a large plume at the coast (upper right).” (Full-sized)
Today’s Eruption Summary

And we’re back to routine, except that Fissure 8’s providing a minor puzzle to keep HVO busy. Yesterday it didn’t exhibit the surge behavior that’s been typical after summit collapses for the week or so. Today, nowhere near the time of a collapse event, “surging was noted at the Fissure 8 cone during the [morning] overflight but had stopped by the time ground crews arrived to verify it.” Otherwise, the channel’s lava level was low this morning. No other were fissures active.

July 17, 2018. USGS: ” During their overflight, scientists used a telephoto lens to photograph the surface of the fissure 8 lava channel. Incandescent lava is visible through pieces of darker crust that forms as the flow surface cools. Note the apparent symmetry on either side of the channel center, where lava flows more quickly than it does along the channel margins—a visual representation of flow velocity across the channel width.” (Full-sized)

Both the strong southern ocean entry and weak “ooze-outs” north along the edge of the lava delta continue. Onshore, the southern margin of the flow front was reported to be half a mile from the Pohoiki boat ramp this morning. Unfortunately, that flow edge has stalled but not stopped, and a DLNR official warned Isaac Hale Park is still within its sights.

July 17, 2018. USGS: “South margin of the fissure 8 lava flow ocean entry. As of this morning, the flow was about 750 m (just under 0.5 mi) from the Pohoiki boat ramp.” (Full-sized)

We’re still awaiting the next summit collapse, which looks like it’s going to thwart HVO’s new “Northeast Caldera Rim” livestream by happening at night.

Speaking of the northeast rim, here’s the July 12 collapse event with sound from that vantage point:

Also out today is this impressive new Kīlauea Digital Elevation Model.

The split-second info card at the end says the floor of Halemaʻumaʻu Crater has dropped 450 m (1480 ft). Prior to the current eruption, it was 85 m (~280 feet) deep. So it’s about 1760 feet deep now. (World Trade Center One is 1776.)

Continue reading July 17: New and Old Views of Halema’uma’u

July 16: Lava Boat Tourists Injured

July 16, 2018. USGS: “The active ocean entry along the southernmost margin of the fissure 8 flow is a hazardous area. The interaction of lava and seawater creates “laze,” a corrosive steam plume laced with hydrochloric acid and fine volcanic glass particles that is blown downwind and can irritate the skin, eyes, and lungs. Lava flows entering the ocean can also result in explosive interactions, littoral explosions, that can hurl fragments of molten lava and rocky debris hundreds of meters (yards) inland and seaward.” (Full-sized)
Today’s Eruption Summary

The big news today was a lava tour boat getting pelted by lava chunks from an ocean entry explosion, resulting in burns, bruises, and one broken leg. Next to that, the science of this eruption seems a bit trivial. But this blog is primarily oriented towards the latter, so let’s get volcanology news out of the way first.

The Italian Space Agency released a new CosmoSkyMed radar scan of Kīlauea’s summit. Let’s hope this really is the new northern extent of Halemaʻumaʻu:

May 5-July 16, 2018. USGS: “Over time, expansion of the summit eruptive vent within Halema‘uma‘u crater and the widening of Halema‘uma‘u itself are obvious. Starting in late May, the development of several cracks outside Halema‘uma‘u is clear, and inward slumping of a large portion of the western, southwestern, and northern crater rim begins. Much of this motion appears to be coincident with the small explosions from the summit that have taken place on a near daily basis since early June. The most recent radar scene, from July 16, shows continued motion along cracks over a broader area of the caldera floor, extending east of Halema‘uma‘u. We expect this slumping to continue as long as the collapse events and overall subsidence persist.” (Full-sized)

This morning, over 24 hours after the previous summit collapse, the lava channel below Fissure 8 was full but not overflowing. Even after today’s 11:42am summit collapse, there was no observed surge— “Nothing notable in the way of overflows.” Last night’s field crews heard Fissure 22 grumbling to itself, but saw no visible signs of renewed activity.

According to Civil Defense this afternoon, the southern edge of the main lava flow has stalled 1 km from Isaac Hale Park / Pohoiki boat ramp. Just north of there, the new ocean entry at Ahalanui is vigorous and dangerous. That’s where @hotseathawaii filmed an offshore explosion four days ago. There were more explosions this morning, “with at least one being quite strong” (USGS).

(The summit collapse was M 5.3 again. The livestream is still ailing, but even so it captured rockfalls, camera shake, and the earthquake’s progression from far to near in the field of view.)

July 16 Map of Active Lava Flows

Lava delta is up to 690 acres, by the way. “Tiny no-longer-island” is next to the c in “former coastline.”

USGS map of LERZ lava flows as of July 15, 2018, 1 pm HST. Yes, the tiny no-longer-an-island is visible in the full-sized image.

Continue reading July 16: Lava Boat Tourists Injured

July 13: Hawai’i Has a New Island (For Now)

July 13, 2018. USGS: “A tiny new island of lava has formed on the northernmost part of the ocean entry. During this morning’s overflight, HVO’s field crew noticed the island was oozing lava similar to the lava oozing from the broad flow front along the coastline.” (Full-sized)
Today’s Eruption Summary

Fissure 8’s lava flow has settled into its new course, turning right just before Kapoho Cone and proceeding south-southeast to the ocean in a strong channelized a’a flow. Some lava, apparently following the earlier paths (lava tubes, maybe?) to the sea, is still squeezing out of the broad 6km (3.7) mile lava delta to the north of the new ocean entry.

A fascinating footnote: while the northern “ooze-outs” are weakening, a tiny lava island popped up just offshore of them last night, and it is itself oozing lava:

July 13, 2018. USGS: “A closer view of the new “island,” which was estimated to be just a few meters offshore, and perhaps 6-9 meters (20-30 ft) in diameter. It’s most likely part of the fissure 8 flow that’s entering the ocean—and possibly a submarine tumulus that built up underwater and emerged above sea level.” (Full-sized)

Fissure 22 has stopped spattering. However, many inactive fissures were steaming today, “possibly due to the increasing humidity in the area.”

Today’s summit collapse occurred at 7:06pm HST, with the energy equivalent of a 5.3 earthquake, as usual. HVO is setting up a new livestream from Volcano House, but it’s not fully operational yet, so we made do with the ailing HVO webcam today (video clip).

July 13, 2018. USGS: “View of Halema‘uma‘u and Kīlauea caldera just before 8:00 a.m. HST today, as seen from HVO’s observation point near Volcano House. Gusty winds were blowing quite a lot of rock-fall dust, visible both within and along the rim of the crater.” (Full-sized)

It’s been fascinating watching geologists collect data, figure things out, and incorporate these discoveries into their daily Kilauea alerts. Just as the HVO team  started predicting the summit’s cyclical collapse/explosions, now they’ve started predicting (or at least watching for) Fissure 8’s lava surges and possible spillovers a few hours after each summit collapse. Sure enough:

Also, we’ve got a new view of ever-expanding Halema’uma’u Crater in Kilauea’s summit caldera this morning:

July 13, 2018. USGS: “USGS scientists captured this stunning aerial photo of Halema‘uma‘u and part of the Kīlauea caldera floor during a helicopter overflight of Kīlauea’s summit this morning. In the lower third of the image, you can see the buildings that housed the USGS Hawaiian Volcano Observatory and Hawai‘i Volcanoes National Park’s Jaggar Museum, the museum parking area, and a section of the Park’s Crater Rim Drive. Although recent summit explosions have produced little ash, the drab gray landscape is a result of multiple thin layers of ash that have blanketed the summit area during the ongoing explosions.” (Full-sized)

I couldn’t find a comparable aerial photo with the observatory and Jaggar in shot, but this 2009 photo of Halema’uma’u is facing in approximately the same direction. (Look for Crater Rim Rd behind the crater on the left, and note the parking lot obscured by the lava lake’s plume in 2009— lava lake, parking lot, and part of that road collapsed into the crater in June.)

Continue reading July 13: Hawai’i Has a New Island (For Now)

July 5: Lava Takes Aim at Last of Kapoho Beach Lots

July 5, 2018: USGS: “Near the Kapoho Crater, in the area called Four Corners, the lava channel makes a 90-degree bend. After lava exits the bend, it makes a short drop to form a lavafall. A side channel makes a short surface diversion before rejoining the existing channel.” (Full-sized)
Today’s eruption summary

The LERZ eruption continues with minor variations. This morning’s USGS overflight crew observed that Fissure 8’s fountain and lava level in the upper channel appeared to be slightly lower. However, the lava flow rate down at Kapoho Beach Lots —where there were only a few houses left, as of this morning — seems to have picked up slightly.  Meanwhile, overflows spilling out from the constricted turn around Kapoho Crater have nearly reached Beach Rd about 0.2 miles north of Four Corners. Lava continues to enter the ocean along a very broad front, mostly on the northern side of the delta.

July 5, 2018. USGS: “Lava enters the sea along the Kapoho coastline, building a delta that is now over 555 acres in size.” ( full-sized )

Fissure 22 is “sporadically spattering,” and its flow  may have stalled.

At the summit, today’s collapse/explosion occurred at  1:20 PM HST, registering as a magnitude 5.2. Once again, I noticed rockfalls picking up about a minute before the big shake, although it might be coincidence (they’re happening at other times of the day as well):

The Italian Space Agency has posted a new satellite radar image of Kilauea Caldera, showing the ongoing subsidence across much of the crater floor (you may have to view full-sized version for the animation):

USGS: “This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and July 4 at about 6:00 a.m. HST…Over time, expansion of the summit eruptive vent within Halema‘uma‘u crater and the widening of Halema‘uma‘u itself are obvious. Starting in late May, the development of several cracks outside Halema‘uma‘u is clear, and inward slumping of a large portion of the western, southwestern, and northern crater rim begins. Much of this motion appears to be coincident with the small explosions from the summit that have taken place on a near daily basis since early June. The most recent radar scene, from July 4, shows continued motion along cracks over a broader area of the caldera floor, extending east of Halema‘uma‘u (these cracks are the scarps seen in recent photographs from the Keanakākoʻi overlook area).” (Full-sized)

By the way, if anyone else was confused by recent Hawaii Tribune Herald articles that said SO2 levels had climbed tenfold at the summit, I checked with @USGSVolcanoes, who suggested a minor mixup. That increase is occurring down in the Lower East Rift Zone. At the summit, according to Kyle Anderson during today’s media conference call, SO2 levels have dropped to the level they were before the lava lake first appeared.

 

Continue reading July 5: Lava Takes Aim at Last of Kapoho Beach Lots

July 1: Fissure 22 Is Back; Kilauea Caldera Is Sinking

Fissure 8 gushes on unchallenged and unchanged, while Fissure 22 — remember the chief subject of Lavacam?— has started spattering 50-80m and sending out a modest lava flow headed NE along the edge of previous flows.

USGS photo from morning overflight, July 1, 2018. Fissure 8 in the distance, Fissure 22 in the middle ground across from PGV. (Full-sized)

Down at the coast, lava continues to ooze out from under much of the northern part of the delta along a broad front, with “pasty” lava squeezing out in several places along Kapoho Beach Lots.

As of 8:30pm 11pm HST, I’m waiting for confirmation of the next summit collapse/explosion.

Besides Fissure 22 reactivating in earnest, the news today is that new digital elevation maps and satellite images give us a clear view of the subsidence of Kilauea Caldera around Halema’uma’u, which has begun to show in livestream and webcam views lately.

First of all, USGS seismologist Kyle Anderson posted this color-coded slide of caldera ground deformation in his Thursday evening talk:

The colors compare the new June 19, 2018 drone-surveillance digital elevation map with a DEM of the caldera captured in 2009. Presumably the light gray areas within Halema’uma’u don’t correspond to anything on the older map, so can’t be compared. Green patches are earthquakes over the past few days indicating stress. And “300+ ft” marks the last known position of the NPIT GPS sensor before it sank out of radio contact. (Full-sized)

Next, the Italian Space Agency’s trusty Cosmo-Skymed satellite has sent us another radar survey of Kilauea. Even though I’d observed dramatic subsidence of the caldera floor in recent livestream and webcam images, the last frame of this animation made me gasp:

USGS: “This animated GIF shows a sequence of radar amplitude images that were acquired by the Agenzia Spaziale Italiana CosmoSkyMed satellite system. The images illustrate changes to the caldera area of Kīlauea Volcano that occurred between May 5 and June 30 at about 6:00 a.m. HST[…] Over time, expansion of the summit eruptive vent within Halema‘uma‘u crater and the widening of Halema‘uma‘u itself are clear. Starting in late May, the development of several cracks outside Halema‘uma‘u is clear, and inward slumping of a large portion of the western, southwestern, and northern crater rim begins. Much of this motion appears to be coincident with the small explosions from the summit that have taken place on a near daily basis since early June. The most recent radar scene, from June 30, shows the formation of cracks over a broader area of the caldera floor, extending east of Halema‘uma‘u (these cracks are the scarps seen in recent photographs from the Keanakākoʻi overlook area). We expect this slumping to continue as long as the collapse events and overall subsidence persist. (Full-sized)
We are well on our way to a nested caldera, with Halema’uma’u taking up over half the larger caldera floor. I’m hoping those earthquakes indicate where the edge of the new inner caldera will be, but I’m not a geologist. Here’s those scarps they mentioned, posted a few days ago:

USGS: “Comparison of photographs taken on June 13 and 26 from near Keanakāko’i Crater overlook in Hawai’i Volcanoes National Park shows a subsidence scarp that formed as the Kīlauea Crater floor subsided. Scientists estimate the dramatic dropping of the crater floor in this area occurred sometime between June 23 and 26. The view is to the west. Halema‘uma‘u crater is in upper right.” (Full-sized)

Last but not least, the USGS posted this map of the fracturing around Halema’uma’u. Note that the diagram is projected onto a satellite photo of the pre-May caldera, so there’s a ghostly image of the Halema’uma’u we remember in that dark gray area.

USGS: “This map shows major fractures in yellow (as of June 29) on a base image acquired by the WorldView-2 satellite before the current sequence of events began at Kīlauea. The area of major subsidence has expanded east and south, and slightly west, of the main Halema‘uma‘u crater area. The large, red-shaded area east of Halema‘uma‘u is moving down within a scarp-bounded area, as seen in recent photographs of the summit. Some fractures have also formed to the east-northeast of the red-shaded area of accelerated motion, and also on the south caldera rim where parts of the caldera wall have slumped into the rapidly moving caldera floor below. The dark gray-shaded area within the red shaded area shows the region of most significant down dropping and is currently the deepest part of Kīlauea caldera.” (Full-sized)

So there you have it.  Who would’ve thought the draining of the lava lake, which was minuscule compared to the whole summit caldera, would’ve had a domino effect this large?


The rest of this post is a fairly sparse weekend roundup of a few news stories, videos and photos, plus of course the usual science geeking with USGS. Which leaves you time to browse the USGS Thursday evening talk I transcribed today!
Continue reading July 1: Fissure 22 Is Back; Kilauea Caldera Is Sinking

June 28: USGS Talk on Latest Changes to Kilauea Caldera [Pt. 1 of 3]

On Thursday, there was an hour and a half meeting with the USGS, National Park Service and residents of Volcano Village. Above is a video of the whole meeting. As usual, I’m interested in the geology, and so I’ve made a transcript of that part of the meeting. The first half of Kyle Anderson’s talk rehashes the “collapse/explosion” events that we’ve covered before, but the second half has a timelapse of Halema’uma’u from June 1st to June 28th — which I’ve rebuilt frame by frame, since I could just make out the timestamps— plus the latest Digital Elevation Model of Kilauea’s summit showing the slumping not only in Halema’uma’u, but across part of the caldera floor.

Scientist-in-Charge Tina Neal (HVO)

[5:40] [Introductory remarks, greetings and thanks]

[6:20] So tonight you’ll hear from familiar faces, Kyle Anderson and Don Swanson, who will give you an update on what the volcano is doing, what we think is happening, and we’ll touch on this very important question of how long and how big. Those are very hard questions to answer, so let me just preview that we’re not going to give you a wonderful take-away that will solve all that uncertainty. But we’ll do the best we can.

Continue reading June 28: USGS Talk on Latest Changes to Kilauea Caldera [Pt. 1 of 3]

June 20: Jaggar Museum Collection Rescued

Today’s Eruption Summary:

Status quo continues, with Fissure 8 feeding a large, fast-flowing channel to the ocean, where it’s entering on the south side of the lava delta today. Upstream along the river, there’s occasional spillovers, but these never travel far from the levees. Top speeds on June 18 were measured at 20mph, by the way. Fissures 6 and 16 have reverted to fuming. (I see no white speck left of Fissure 8 on the LERZ webcam [correction: it’s back at 9:45pm]). Today’s summit explosion occurred at 4:22am (5.3ish), with a minor ash plume rising 6,000 feet above sea level (2000 feet above Kilauea).

Saying Goodbye (At Least For Now)
USGS: “The rock wall at the Jaggar Museum Overlook is cracked and crumbling.
USGS image taken June 18, 2018.”

Today’s big news was confirmation that Jaggar Museum has evacuated its exhibits:

Hawaii Volcanoes NPS: “The cracks on the floor are from earthquake damage. Structural damage from the quakes may have already compromised the building. The observation deck has a new and noticeable tilt. The bigger worry is the increasing and dangerous instability of the crater rim under the building.”

Meanwhile, HVO staff is “making arrangements to remove as much archival and historical material as possible from the buildings,”  They’re so busy monitoring this eruption that I think they may need to hire movers:

Outside, it’s time to bid farewell to the old Halema’uma’u overlook & parking lot:

USGS: “View of the southern edge of the growing Halema‘uma‘u crater (middle right) during yesterday’s [Jun 19] helicopter-assisted work at Kīlauea’s summit. The once-popular parking lot (closed since 2008) that provided access to Halema‘uma‘u is no longer–the parking lot fell into the crater this past week as more and more of the Kīlauea Crater floor slides into Halema‘uma‘u. The Crater Rim Drive road (middle) now ends at Halema‘uma‘u instead of the parking lot. The view is toward the west-northwest.” (Full-sized)
More USGS PHOTOS

Continue reading June 20: Jaggar Museum Collection Rescued

June 6: Summit Explosions Explained (And Predicted!)

USGS/HVO photo of Fissure 8, spatter cone and rainbow, June 6.
Today’s Eruption Update:

Last night, USGS scientist Steve Brantley explained the current eruption in an informative 10 minute talk. I transcribed it as a separate post, but here’s a rough summary: Magma heading down to the Lower East Rift Zone is causing the summit to deflate. Deflation is causing a pattern of more and more earthquakes over 30-50 hours until the summit releases the strain with an explosion, accompanied by an ash cloud.

Sure enough, there was an M5.6 explosion and 10,000 foot ash cloud at 4:32pm. HVO’s Twitter account had a great impromptu Q&A session about it (see below).

Meanwhile, down in the Lower East Rift Zone, Fissure 8 shows no signs of slowing. It’s wiped out Vacationland and nearly all of Kapoho Beach Lots, and is continuing to create new (crumbly, hazardous) beachfront real estate.

USGS has also been posting some striking imagery today.

Video description: “HVO’s mid-day overflight on June 5 shows ongoing partial collapse of Halema‘uma‘u at the summit of Kīlauea Volcano. To the north of the former visitor Overlook parking area (closed in 2008) is the site of the former lava lake—now a deep hole piled with wall-rock rubble. The western portion of Halema‘uma‘u has moved down and toward the center of the crater as new cracks form on the caldera floor to the west. Kīlauea’s summit continues to subside due to withdrawal of magma towards the volcano’s East Rift Zone.”

They’ve also posted drone footage of Fissure 8 lava flow on June 3. Houses give a sense of scale:

(Link to video description)

Here’s this morning’s USGS helicopter overflight of Fissure 8:

More images, lots of great geology info below the cut. But first, a 2-minute USGS briefing, since we skipped yesterday’s:

Continue reading June 6: Summit Explosions Explained (And Predicted!)