Pu‘u ‘Ō‘ō
From Freepedia
| Pu‘u ‘Ō‘ō | |
|---|---|
| Image:Puu Oo cropped.jpg | |
| Elevation: | 2,290 ft (698 m) |
| Location: | Hawaii, USA |
| Range: | Hawaiian Islands |
Pu‘u ‘Ō‘ō-Kūpa‘ianahā eruption
The Pu‘u ‘Ō‘ō 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 Pu‘u ‘Ō‘ō vent. Over the next three years, 44 eruptive episodes with lava fountains as high as 460 m (1500 ft) stopped traffic at vantage points across east Hawai‘i. The fallout of cinder and spatter from the towering lava fountains built a cone 255 m (835 ft) high. In July 1986, the conduit feeding magma to Pu‘u ‘Ō‘ō ruptured, and the eruption abruptly shifted 3 km downrift to form the Kūpa‘ianahā vent. With the new vent came a new style of eruption: continuous, quiet effusion from a lava pond replaced the episodic high fountaining. Overflows from the pond built a lava shield—a broad, low hill shaped like an overturned wok.
In November 1986, lava from Kūpa‘ianahā reached the ocean, 12 km (7 miles) to the southeast, innundating the small community of Kapa‘ahu in its path. For the next five years, much of the lava erupted from Kūpa‘ianahā streamed directly into the sea via a lava tube system that led from the lava pond.
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 the Hawaii Volcanoes National Park. The volume of lava erupted from Kūpa‘ianahā declined steadily through 1991, and, in early 1992, the vent died. The eruption then returned to Pu‘u ‘Ō‘ō, 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 Napau Crater, a short distance southwest of Pu‘u ‘Ō‘ō.
Image:Kilauea 1997 cutaway.gif On the evening of January 29, 1997, a swarm of earthquakes struck Kilauea's east rift zone. Deep within the rift zone, magma was escaping from the conduit leading to the Pu‘u ‘Ō‘ō vent, cutting off the supply to the ongoing eruption. The lava pond at Pu‘u ‘Ō‘ō 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 Pu‘u ‘Ō‘ō cone collapsed. A few hours later, as magma found a new path to the surface, the ground cracked in nearby Napau Crater, and lava fountains lit up the night sky.
References
- USGS Volcano Hazards Program: The Pu`u `O`o-Kupaianaha eruption: still flowing after all these years (public domain)
- U.S. Geological Survey fact sheet 144-02: The Pu`u `O`o-Kupaianaha eruption of Kilauea Volcano, Hawai`i, 1983 to 2003 (public domain)
External links
- Live web cam of the Pu‘u ‘Ō‘ō vent
- USGS map shows lava flows erupted during the 1983-present activity of Pu`u `O`o and Kupaianaha.
- Maps and aerial photos
- Street map from Google Local or Yahoo! Maps
- Topographic map from TopoZone
- Aerial image or topographic map from TerraServer-USA
- Satellite image from Google Local or Microsoft Virtual Earth
| Note: This page contains IPA phonetic symbols in Unicode. |
