While much of the attention is on the lava flows and burning homes in lower Puna, there have been dramatic events at the summit of Kīlauea. The pit crater of Halemaʻumʻau that has been the subject of untold thousands of tourist photos has become almost unrecognizable.
The plume of volcanic gasses from Halemaʻumaʻu under the starsHalemaʻumʻau is a pit crater created by the ever changing eruptions of Kīlauea. Half a mile across, this crater sits within the much larger Kīlauea caldera at the summit of the volcano. A nearly circular pit that lies at the center, home to many eruptions across the centuries. This often fiery pit is reputed to be the home of Pele, the goddess of fire and creation in Hawaiian mythology.
Step outside and you can smell the sulfur… In Waikoloa!
The Kona airport wreathed in vog on May 29, 2018This is a first. The vog has been bad, but never this bad, the entire island is wreathed in a heavy haze of volcanic emissions. As I write this I feel my eyes are irritated, stepping outside you can see it in the streetlights.
Deb and I drove to Kona this afternoon. The usually pretty drive was simply gray, gray with a tinge of yellow-brown. No views of the mauna, no views of the ocean. You could barely see the airport from the highway as we passed.
The vog has been the subject of conversation everywhere, online in social media, and in every single casual conversation you happen into today. The volcano, so devastating to those in lower Puna, has reached out to touch us all.
Vog map May 29, 2018The vog mapping done by the University of Hawaii showed that mid-day, the vog was sweeping right through the Saddle at Waikoloa and the Kona coast from the current eruption site in lower Puna. Fortunately the predictions are for resumed northeast trade-winds tonight, clearing much of the island of vog into tomorrow.
Things could be worse. An explosion at the caldera today showered surrounding communities with ash and Pele’s hair. Plus, there is much to be said about not having a lava flow, or three, flowing though your neighborhood.
The ground beneath us is one constant in life you just expect to never change. Solid and unyielding, we build our lives upon the firm foundations of the Earth. When this constant betrays us it is truly disconcerting. The world loses some of its comforting stability.
Last Friday was a day when our islands were reminded of the instability of our world in a rather abrupt fashion.
USGS Earthquake Map for May 6, 2018It was clear weeks ago that the volcano was restless. volcanophiles like myself found ourselves checking the reports and charts daily. The deformation graphs are a good indication of what is going on inside the volcano.
The tiltmeters indicated that pressure in the caldera and Puʻu Oʻo had been building steadily. At the same time the activity in the 61g lava had been waning. Where was the magma going?
While speculation was rife, no one really knew what was coming. Three decades of eruptions from Puʻu Oʻo has become somewhat routine. People forget that Kilauea can be, and usually is much more unpredictable. That destruction can appear anywhere on her flanks.
Lava emerges from a fissure in the Leilani Estates subdivision on May 5th, 2018, photo from the USGSThe first lava surfaced Thursday afternoon in the neighborhood of Leilani Estates. The observatory staff had gathered to celebrate a pau hana that afternoon, an early Cinco De Mayo celebration with Mexican food. Many of us ate our tacos and quesadillas in the conference room, where the large screen was showing drone video of the first fissures.
We worried about the homes in the neighborhood and the people we knew who lived in the area. We compared notes, recalling who lived exactly where, fearing the lava flows would quickly spread. This was looking like a worst case scenario, a repeat of 1955 with more people and homes in the way.
Despite the outbreaks of lava in the rift zone the previous afternoon, we expected a routine Friday atop Mauna Kea. I had a list of tasks to complete… Inspect the K1 azimuth wrap, drill some anchor points to allow installation of the new ice monitor receiver on the roof, look for some spare parts for an encoder.
It should be an easy day on the summit… It was not.
Friday became a day I will remember for a long time to come.
This morning began with a series of strong earthquakes along the eastern rift zone of Kilauea. The island was buzzing about it, the local news, social media, it was the main subject of conversation in our trucks headed to the summit. By this evening there have been over 250 earthquakes, including many of 3rd and 4th magnitude, along the rift zone, a clear sign of lava moving underground.
USGS Earthquake Map for 1May2018Avid volcano watchers like myself have been keeping close tabs on the eruption for the last couple weeks. The 61g lava flow that has been the main outlet for lava for the last two years has faded into inactivity. The deformation data at the main caldera and at the Puʻu Oʻo vent has indicated steadily increasing pressure in the volcano.
The increasing pressure has raised the level of the lava lake at Halemaʻumaʻu to the point of overflowing into the larger crater multiple times over the last week. This alone can be spectacular as it is easily viewed from the viewpoint at the Jaggar Museum in Hawaii Volcanos National Park.
61G lava flow this morning, first time I have been out since the shelf collapse, what a difference, it just pours out of the tube. There is a small fragment of the old shelf, it continues to collapse, heard and watched a couple truck sized chunks fall out of it and into the surf.
Did another dawn attack, arriving at the flow about 2am, staying until after sunrise. The new rope line is stupidly far back, so far back no one was honoring it. I stayed about 200-300 yards away, but saw folks on the top of the cliff over the tube where I had seen glowing globs land just half an hour before.
The 61G flow after the shelf collapse on 15 Jan 2017