Halemaʻumaʻu Crater (six syllables: HAH-lay-MAH-oo-MAH-oo) is a pit crater within the much larger summit caldera of Kīlauea in Hawaii Volcanoes National Park. The roughly circular crater was 770 meters (2,530 ft) x 900 m (2,950 ft) before collapses that roughly doubled the size of the crater after May 3, 2018. Halemaʻumaʻu is home to Pele, goddess of fire and volcanoes, according to the traditions of Hawaiian religion. Halemaʻumaʻu means "house of the ʻāmaʻu fern".
Halemaʻumaʻu contained an active lava lake for much of the time before 1924, and was the site of several eruptions during the 20th century. The crater again contained an active lava lake between 2008 and 2018, usually fluctuating between 20 to 150 meters below Halemaʻumaʻu's crater floor, though at times the lava lake rose high enough to spill onto crater floor.
As new volcanic vents opened in lower Puna in May 2018, the level of the lava lake began to drop in early May 2018, eventually to the point where the lava lake was no longer visible. The subsidence of the lava lake was accompanied by a period of explosions, earthquakes, large clouds of ash and toxic gas, and finally a gradual collapse of the summit caldera around Halemaʻumaʻu Crater, resulting in the closure of the Hawaii Volcanoes National Park from May 10 to September 22, 2018. The collapse events ceased abruptly on August 2, 2018.
Astonishment and awe for some moments rendered us mute, and like statues, we stood fixed to the spot, with our eyes riveted on the abyss below. Immediately before us yawned an immense gulf, in the form of a crescent, about two miles (3 km) in length, from north-east to south-west, nearly a mile in width, and apparently 800 feet (240 m) deep. The bottom was covered with lava, and the south-west and northern parts of it were one vast flood of burning matter, in a state of terrific ebullition, rolling to and fro its "fiery surge" and flaming billows.
It was like gazing at the sun at noon-day, except that the glare was not quite so white. At unequal distances all around the shores of the lake were nearly white-hot chimneys or hollow drums of lava, four or five feet high, and up through them were bursting gorgeous sprays of lava-gouts and gem spangles, some white, some red and some golden--a ceaseless bombardment, and one that fascinated the eye with its unapproachable splendor. The more distant jets, sparkling up through an intervening gossamer veil of vapor, seemed miles away; and the further the curving ranks of fiery fountains receded, the more fairy-like and beautiful they appeared.
The level of the lava lake varied over the decades. In 1924, unusual explosive eruptions sent dust high into the atmosphere and doubled the diameter of the crater. Fractures allowed the lava lake to drain to the east until its surface was 366 m (1,200 ft) below the caldera floor. Subsequent eruptions have mostly refilled the crater. Most of the current crater floor was formed in 1974. A 1982 eruption covered a small portion of the northeastern crater floor.
Crater eruption - 2008 to 2018Edit
Beginning of the eruptionEdit
Halemaʻumaʻu was quiet for 25 years after the 1982 eruption, with eruptive activity at Kīlauea being focused on the volcano's east rift zone beginning in 1983. However, Hawaiian Volcano Observatory scientists observed a gradual increase in activity beginning in late 2007, including an increase in sulfur dioxide emissions and an increase in seismic tremor. By March 2018, these parameters were several times higher than normal.
Crater activity began to increase when between March 10 and March 14, 2008 gas began to vent from the east wall fumarole directly below the Crater Overlook. At 02:58 am HST on March 19, 2008, HVO personnel recorded seismic events, and sunrise revealed a 20–30 meter (65–100 foot) diameter hole blown in the side where the vent once was; the explosion scattered debris and spatter across 0.30 square kilometers (74 acres) and damaged the Crater Overlook. Pieces as large as 20 millimeters (1 in) were found on Crater Rim Drive while 0.3 m (1 ft) blocks hit the crater overlook area. This was the first explosive eruption of Halemaʻumaʻu Crater since 1924, and the first lava eruption from the crater since 1982. The new crater formed in the explosion was informally named "Overlook Crater" by Hawaiian Volcano Observatory staff.
Sulfur dioxide gas emissions increased rapidly at the beginning of the episode. On March 13, HVO recorded a rate of 2,000 tons/day, the highest rate since measurements began in 1979. A concentration of over 40 ppm on Crater Rim Drive was measured, prompting alerts and other public safety measures. Halemaʻumaʻu crater continued to intermittently emit high levels of volcanic gases, ash, spatter, Pele's Tears, and Pele's Hair until the second episode.
Another explosive event occurred during the night of April 9, 2008, which widened the Overlook Crater by an additional 5–10 meters (15–30 feet), ejected debris over some 60 m (200 ft) and further damaged the overlook as well as scientific monitoring instruments.
In response to the second episode, scientists and local government officials on April 9, 2008 ordered hundreds of people to evacuate from the Park and nearby villages because the sulfur dioxide concentration levels had reached a critical level and a hazardous vog plume extended downwind from the crater. The evacuation lasted two days.
On April 16, 2008, a third significant explosive event occurred at Halemaʻumaʻu, spreading ash and debris throughout the area. Subsequently, a second evacuation of the park and surrounding areas was ordered on April 23, 2008.
Activity continued through the next few months, with Halemaʻumaʻu continuing to emit a plume of ash and gases. A fourth explosive event occurred on August 1, 2008, and a fifth on August 27, 2008.
September 2008: Lava lake becomes visibleEdit
A Hawaii Volcano Observatory news release and images dated September 5, 2008 confirmed the first recorded images of a lava lake 130 feet below the lip of the Overlook Crater. The HVO had alluded to the presence of lava within the vent, including the sporadic ejecting of lava materials from the vent due to explosive episodes, but this gave officials the first opportunity to visually confirm that active lava was present. The report also noted that the lava could not be seen from observation points around the crater.
September 2008 to April 2018: Sustained lava lakeEdit
The lava lake within Halemaʻumaʻu's Overlook Crater vent was visible nearly continuous from March 2008 until May 2018. During the period, the Overlook Crater slowly enlarged. The height of the lava lake fluctuated. In May 2015, the lake rose high enough to spill onto the Halemaʻumaʻu crater floor for the first time, adding a layer of lava approximately 30 feet (9 m) thick to the crater floor..
For three years from 2015 to 2018 the lava lake level remained close to the rim, with a further minor overflow event in October 2016 and a significant one in April 2018 that covered a majority of the crater floor in new lava.
In April 2018, a significant series of overflows had reportedly covered most of the Halema'uma'u Crater floor with new lava.
April to July 2018: Drainage of lava lake and the collapse of the summitEdit
On April 30, the Pu'u O'o crater on Kīlauea's east rift zone collapsed. Several days later, lava began to emerge from fissures on the lower east rift zone in Leilani Estates. On May 1, concurrent with the shift of activity on Kīlauea's east rift zone, the summit lava lake within Halemaʻumaʻu's Overlook Crater began to drop; the US Geological Survey's status update on the evening of May 6 reported that Halemaʻumaʻu‘s Overlook Crater lava lake had dropped by 722 feet (220 m) since April 30. By May 10, the lava lake was no longer visible. Geologists believed that the draining of the lava lake was driven by a steady withdrawal of magma from Kīlauea's summit to feed the eruption on the volcano's lower east rift zone. Several small explosive events occurred between May 16 and May 26, ejecting ash and small blocks within a few hundred meters of the vent. An explosion on May 17 created an ash plume that reached 30,000 feet above sea level.
Beginning near the end of May, the floor of Kīlauea Caldera around Halemaʻumaʻu began to subside in a series of 62 separate collapse events. At each collapse event the floor of the caldera dropped several meters and there was a magnitude 5.2 to 5.4 earthquake. Between each collapse event, an escalating swarm of earthquakes would occur. Notably, more than 700 earthquakes of a magnitude 4.0 or higher occurred each day during the collapse period. The collapse events enlarged and deepened Halemaʻumaʻu. The crater's volume increased from about 54-60 million cubic meters to 885 million cubic meters, and the depth of the crater increased by more than 500 meters. During the collapse, the former Halemaʻumaʻu overlook and its parking lot were lost when segments of the crater rim slumped into the crater. The summit collapse events ceased abruptly on August 2, 2018, two days before the eruptive activity on Kīlauea's east rift zone decreased significantly.
White-tailed tropicbird is flying directly over the Halemaʻumaʻu vent, 2008
Time lapse video of Halemaʻumaʻu Crater, 2014
Time lapse video of the lava lake in Halemaʻumaʻu Crater, 2016
Time lapse video of Halemaʻumaʻu Crater, 2017
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