View at dusk, June 1983
|Elevation||2,290 ft (700 m)|
|Location||Hawaii County, Hawaii, US|
|Parent range||Hawaiian Islands|
|Topo map||USGS Kalalua|
|Age of rock||33 years|
|Mountain type||Cinder/spatter cone|
|Volcanic arc/belt||Hawaiian-Emperor seamount chain|
Puʻu ʻŌʻō (often written Puu Oo, pronounced [ˈpuʔu ˈʔoːʔoː]) is a volcanic cone in the eastern rift zone of the Kīlauea volcano of the Hawaiian Islands. Puʻu ʻŌʻō has been erupting continuously since January 3, 1983, making it the longest-lived rift-zone eruption of the last two centuries.
By January 2005, 2.7 cubic kilometers (0.65 cu mi) of magma covered an area of more than 117 square kilometers (45 sq mi) and added 230 acres (0.93 km2) of land to the Southeast coast of Hawaiʻi. So far, the eruption has claimed 189 buildings and 14 kilometers (8.7 mi) of highways, as well as a church, a store, the Wahaʻula Visitor Center, and many ancient Hawaiian sites, including the Wahaʻula heiau. The coastal highway has been closed since 1987, as it has been buried under lava up to 35 meters (115 ft) thick.
The hill was initially nicknamed "Puʻu O" by volcanologists, as its position when marked on a map of the area coincided with an "o" in "Lava flow of 1965". Later, the elders of the village of Kalapana were asked to name the new hill, and chose Puʻu ʻŌʻō, meaning hill of the digging stick. The name is also often translated as "Hill of the ʻŌʻō Bird".
Puʻu ʻŌʻō-Kūpaiʻanahā eruption
The Puʻu ʻŌʻō eruption began when fissures split the ground in the remote rainforest of the eastern rift zone. By June 1983, the activity had strengthened and localized to the Puʻu ʻŌʻō vent. Over the next three years, 44 eruptive episodes with lava fountains as high as 460 meters (1,510 ft) stopped traffic at points across east Hawaiʻi. The fallout of cinder and spatter from the towering lava fountains built a cone 255 meters (837 ft) high.
In July 1986, the conduit feeding magma to Puʻu ʻŌʻō ruptured, and the eruption abruptly shifted 3 kilometers (1.9 mi) downrift to form the Kūpaʻianahā vent. With the new vent came a new style of eruption: continuous, quiet effusion from a lava lake replaced the episodic high fountaining. After a few weeks, a roof formed over the main lava outflow channel, which created a lava tube. The lava tube allowed the fluid pahoehoe lava to retain heat and flow long distances. In less than a year, overflow from the lake created a broad and low shield about 55 meters (180 ft) above Kūpaʻianahā.
Lava streams were first visible from the town of Kapaʻau in November, 1986. In the course of that month, lava cut a swath through Kapaʻahu, covered the coastal highway, and finally reached the ocean 12 kilometers (7.5 mi) from the vent. Some weeks later, the lava flow shifted eastwards and buried 14 houses in the town of Kalapana within one day. The lava flow at Kalapana ceased when the lava tube system shut down.
In 1990, the eruption entered its most destructive phase when flows turned eastward and totally destroyed the villages of Kalapana and Kaimū. Kaimū Bay and Kalapana Black Sand Beach were also completely covered with lava. Over 100 homes were destroyed by the ever-broadening flow field in a nine-month period. New tubes diverted lava away from Kalapana early in 1991, and lava once again entered the ocean within Hawaii Volcanoes National Park. The volume of lava erupted from Kūpaʻianahā declined steadily through 1991, and in early 1992 the vent died. The eruption then returned to Puʻu ʻŌʻō, where flank vents on the west and southwest sides of the cone constructed a new lava shield. Soon lava tubes were feeding lava from the vents to the ocean, with few surface flows in between. The flank vents have held center stage ever since, with the exception of a two-month pause in activity early in 1997 that followed a brief fissure eruption in Nāpau Crater, a short distance southwest of Puʻu ʻŌʻō.
On the evening of January 29, 1997, a series of earthquakes struck Kīlauea's east rift zone. Deep within the rift zone, magma was escaping from the conduit leading to the Puʻu ʻŌʻō vent, cutting off the supply to the ongoing eruption. The lava pond at Puʻu ʻŌʻō drained, and residents 10 miles (16 km) away heard a low, rumbling roar as the crater floor dropped 500 feet (150 m) and the west wall of the Puʻu ʻŌʻō cone collapsed. A few hours later, as magma found a new path to the surface, the ground cracked in nearby Nāpau Crater, and lava fountains lit up the night sky. However, activity in this area was short-lived, and the center of activity soon shifted back to Puʻu ʻŌʻō.
As of 2008[update] Puʻu ʻŌʻō cone was in its twenty-fifth year and 57th eruptive episode. This is the largest volume of lava in the past five centuries to erupt from the volcano's east rift zone. For over a decade the eruption flowed from flank vents on the south and west sides of the cone.
As of January 2007, 3.1 cubic km of lava had covered 117 km2 (45 mi2) and added 201 hectares (500 acres) to Kīlauea's southern shore. The new shoreline is 15.6 km (9.7 mi) long. The lava flows have destroyed 189 structures and covered 14 km (8.7 mi) of highway with as much as 35 m (115 ft) of lava.
In 2007, after a cluster of earthquakes, activity in Puʻu ʻŌʻō subsided and the crater floor collapsed, with no incandescence visible in the crater after the end of August. Lava began emerging from a series of cracks in the northeast rift zone and spread slowly east and south as a perched flow, with slow advances of ʻaʻā. The flow spread mostly over flows of 1983-1986, with minor incursions into adjoining forests.
In late July 2008, additional flows extended from the eastern vents of Puʻu ʻŌʻō and in October multiple new fissures opened along the length of the tube expanding into Royal Gardens Subdivision and covered a large area of the coastal flats in November, 2008.
On March 5, 2011, the floor of the Puʻu ʻŌʻō crater deflated, then collapsed. Two hours later, a new eruption occurred in Kilauea's middle east zone, between Puʻu ʻŌʻō and Napau Crater. Lava fountains were reported to be 65 feet (20 m) high.
On March 26, 2011, lava began to refill the crater's floor being visible in USGS HVO webcam. USGS states that accumulation of lava has put the crater floor about 39 m (128 ft) below the eastern crater rim as of June 1.
On September 21, 2011, lava in the west lava lake in Puʻu ʻŌʻō Crater fed a series of lava flows that traveled down the west flank of Puʻu ʻŌʻō during 20–21 September. At about 0225 on 21 September activity in the crater and overflows to the west suddenly decreased, as lava broke through the upper east flank of Puʻu ʻŌʻō, bypassing the crater. The new fissure fed a channelized ʻaʻā lava flow that advanced rapidly downslope 2.5 km (1.6 mi) southeast. A second flow to the west of the first began the next day. In addition, a small pad of lava actively refilled the bottom of the drained east lava lake and small flows were barely active at the west edge of Puʻu ʻŌʻō Crater. The channelized ʻaʻā lava flow reached 3.7 km (2.3 mi) long on 23 September and then stalled within the Kahauale'a Natural Area Reserve. Most of the active lava spread south and west of Pu'u Halulu (1.3 km or 0.8 mi northeast of Puʻu ʻŌʻō) during 23–27 September. Minor lava activity resumed within Pu'u 'O'o Crater with short lava flows issuing from the base of the east wall on 25 September and from the west wall base during 25–26 September. The crater floor of Puʻu ʻŌʻō slowly subsided. Lava activity resumed within the east lake on 26 September. The floor of the crater continued to subside during 26–27 September, opening up cracks in the north crater floor.
The 2011 activity ultimately destroyed all remaining homes in the Royal Gardens Subdivision. Jack Thompson evacuated his home March 2, 2012. His evacuation and return to the property was documented by Leigh Hilbert.
On June 27, 2014, new vents opened on the northeast flank of the Puʻu ʻŌʻō cone that fed a narrow lava flow to the east-northeast. On August 18, the flow entered a ground crack, traveled underground for several days, then resurfaced to form a small lava pad. The sequence was repeated twice more over the following days with lava entering other cracks and reappearing farther downslope. In this way, the flow had advanced approximately 13.2 km (8.2 miles) from the vent, or to within 1.3 km (0.8 miles) of the eastern boundary of the Wao Kele o Puna Forest Reserve, by the afternoon of September 3. Advancing to the northeast at intermittent rates, the flow had entered the village of Pāhoa and was within 25 meters (27 yards) of the waste recycling center on October 31.
Smoke could be seen rising along the 2014 lava flow from aerial positions along the East Rift Zone. Hot lava spots could also be seen along the flow which indicated that lava was present in lava tubes below the surface. Current status of the Pu'u 'O'o vent can be checked at the Hawaiian Volcano Observatory website.
- C. Heliker, D.A. Swanson, T.J. Takahashi: The Puʻu ʻŌʻō-Kūpaianaha Eruption of Kīlauea Volcano, Hawaiʻi: The First 20 Years. In: U.S. Geological Survey Professional Paper. 1676, 2003. Online Version
- "Puʻu ʻŌʻō crater floor collapse followed by middle east rift zone eruption". USGS Hawaiian Volcano Observatory. 2011-03-05.
- "Recent Kilauea Status Reports, Updates, and Information Releases". Hawaii Volcano Observatory. USGS. Retrieved 2012-10-14.
- "Kilauea". Weekly Volcanic Activity Reports. Smithsonian/USGS. Retrieved 2012-10-14.
- "Lava Claims Final Home". Hawaii Tribute Herald.
- "Jack Thompson's royal Gardens Home".
- "Recent Kilauea Status Reports, Updates, and Information Releases". Retrieved 2014-09-05.
- "Recent Kilauea Status Reports, Updates, and Information Releases". Retrieved 2014-10-31.
- This article incorporates public domain material from the United States Geological Survey document: "USGS Volcano Hazards Program: The Puʻu ʻŌʻō-Kūpaʻianahā eruption: still flowing after all these years".
- This article incorporates public domain material from the United States Geological Survey document: "U.S. Geological Survey fact sheet 144-02: The Puʻu ʻŌʻō-Kūpaʻianahā eruption of Kīlauea Volcano, Hawaiʻi, 1983 to 2003".
|Wikimedia Commons has media related to Puʻu ʻŌʻō.|