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August 4, 2022

The ongoing eruption at the summit of Kīlauea hasn’t made the news recently, but that doesn’t mean the recent eruptive activity hasn’t been noteworthy.  It’s just been operating quietly in the background, without much fanfare. 

Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.

Color photograph of lava lake
Lava lake activity continues in Halema‘uma‘u, at the summit of Kīlauea. This photo looks east, and shows that the lake surface is composed of large crustal plates separated by incandescent spreading zones, with spattering along the east margin. The lake and the surrounding crater floor, formed by solidified lava, are being gradually uplifted due to endogenous lava supply beneath the surface. USGS photo by M. Patrick.

In fact, the slow and steady lava lake activity in Halemaʻumaʻu crater has been quite fascinating, so it deserves another "Volcano Watch" visit.

The first thing to appreciate is that we are witnessing a pattern that has typified Kīlauea’s summit behavior for centuries—the cycle of collapse and refilling.  The caldera floor collapses and/or subsides—often due to an eruption on the rift zone—and subsequent summit eruptions fill the depression with new lava.  Destruction and reconstruction, set on repeat. 

Numerous cycles of collapse and refilling occurred during the 1800s and early 1900s.  These ranged from large to small, some spanning much of the caldera floor, with others limited to just the Halemaʻumaʻu area.  In each instance, lava eventually returned to the summit and filled much or all of the depression. 

The collapse of the crater floor in 2018 was one of the largest such events in the past 200 years.  Over the past year and a half, lava has been erupting in Halemaʻumaʻu crater and slowly refilling the new depression.  Since returning to Halemaʻumaʻu in December 2020, lava has refilled about 17% of the volume of the 2018 collapse. 

Watching the current activity is like having a time machine to an earlier century on Kīlauea. 

The second thing that is interesting about the current activity is the manner in which the lava is refilling the crater.  In the simplest scenario, we might imagine the lava in Halemaʻumaʻu simply pouring in over earlier flows, stacking up and filling the crater.

While a portion of the refilling is being done in this manner, a major amount of the refilling is “endogenous.”  In other words, lava from the vent is supplied beneath the solidified surface crust, out of view, lifting the crater floor.  It’s akin to inflating a giant air mattress. 

We can track this growth with unprecedented detail using modern tools.  A continuous laser rangefinder measures the lava surface every second, with centimeter precision.  Webcams operating on the rim of Halemaʻumaʻu show the nature of uplift clearly. 

The process of endogenous growth is particularly well illustrated with the webcam on the east rim of Halemaʻumaʻu (the B1cam).  Timelapse images from this webcam show the central portion of the crater floor is being lifted like a piston, intact and largely without fracturing. 

The active lava lake—forming a relatively small portion of the crater floor—has essentially been lifted up gradually with the remainder of the crater floor.  The laser rangefinder shows short-term fluctuations in the level of the active lava in the lake, superimposed on a gradual upward trend of the crater floor due to this slow uplift. 

Around the perimeter of this central portion of the crater floor, a series of large cracks have developed.  Beyond the cracks, along the margins of the crater floor, the behavior is more complex than simple piston-like uplift.  This outer region is often tilted and deformed from the endogenous growth below. 

At the same time, this zone along the margins of the crater floor is often resurfaced due to ooze-outs—basically lava that is squeezed out from beneath the crater floor, onto the surface.    

This type of endogenous growth, or “bodily uplift,” was also observed in the 1800s and early 1900s.  But it hasn’t been observed so much in the past hundred years on Kīlauea.  And it certainly hasn’t been observed this clearly before, given our modern tools such as laser rangefinders and webcams.  

You can bear witness to this important phase in the lifecycle of Kīlauea, and a fascinating period in Hawaiian volcanism. Volcano watchers on the Island of Hawaiʻi can see the summit lava lake filling Halemaʻumaʻu crater by visiting the public viewing areas in Hawaiʻi Volcanoes National Park. For those off island, Hawaiian Volcano Observatory webcams showing the lake and crater are operating 24/7 on the HVO website ( 



Volcano Activity Updates


Kīlauea volcano is erupting. Its USGS Volcano Alert level is at WATCH ( Kīlauea updates are issued daily.    

Over the past week, lava has continued to erupt from the western vent within Halemaʻumaʻu crater. All lava is confined within Halemaʻumaʻu crater in Hawai‘i Volcanoes National Park. Sulfur dioxide emission rates remain elevated and were last measured at approximately 1,900 tonnes per day (t/d) on August 1. Seismicity is elevated but stable, with few earthquakes and ongoing volcanic tremor. Over the past week, summit tiltmeters recorded two deflation-inflation sequences (DI-events). For more information on the current eruption of Kīlauea, see

Mauna Loa is not erupting and remains at Volcano Alert Level ADVISORY. This alert level does not mean that an eruption is imminent or that progression to an eruption from the current level of unrest is certain. Mauna Loa updates are issued weekly.     

This past week, about 206 small-magnitude earthquakes were recorded below the summit and upper elevation flanks of Mauna Loa—the majority of these occurred at shallow depths less than 15 kilometers (9 miles) below sea level. 90 of the earthquakes were part of a swarm that occurred beneath Mauna Loa’s summit caldera from August 2-3. Most of these earthquakes occurred around 2 mi (3 km) below the surface and the largest event in the swarm was a magnitude-2.8.  During the earthquake swarm, a minor tilt increase of 1.5 microradians was observed on one tiltmeter (MOK) at the summit, though a small part of this signal includes normal diurnal effects. Global Positioning System (GPS) measurements show low rates of ground deformation over the past week. Gas concentrations and fumarole temperatures at both the summit and at Sulphur Cone on the Southwest Rift Zone have remained stable over the past week. Webcams show no changes to the landscape. For more information on current monitoring of Mauna Loa, see:  

Three earthquakes were reported felt in the Hawaiian Islands during the past week: a M3.4 earthquake 20 km (12 mi) SE of Hāna at 8 km (5 mi) depth on August 1 at 5:33 p.m. HST, a M3.7 earthquake 10 km (6 mi) ENE of Pāhala at 33 km (20 mi) depth on August 1 at 9:20 a.m. HST, and a M2.8 earthquake 8 km (4 mi) NE of Puakō at 22 km (13 mi) depth on August 1 at 2:26 a.m. HST.

HVO continues to closely monitor Kīlauea's ongoing eruption and Mauna Loa for any signs of increased activity.    

Please visit HVO’s website for past Volcano Watch articles, Kīlauea and Mauna Loa updates, volcano photos, maps, recent earthquake info, and more. Email questions to    

Volcano Watch is a weekly article and activity update written by U.S. Geological Survey Hawaiian Volcano Observatory scientists and affiliates.

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