- Loihi Seamount
Infobox Seamount
Name=Lōokinaihi Seamount
Depth= 975 m (3,200 ft)
Height=
Summit =
Location= Southeast ofIsland of Hawaii
Group=
Coordinates =coord|18.92|N|155.27|W|type:mountain |display=title,inline
Country =
Type=Submarine volcano
Volcanic group=Hawaiian-Emperor seamount chain
Age=
Last eruption=1996 (active) [ [http://hvo.wr.usgs.gov/volcanoes/loihi/main.html Lo`ihi Seamount, Hawai`i - Hawaiian Volcano Observatory, U.S. Geological Survey] ]
Discovered=
Discovered_by=
First_visit=
Translation=
Pronunciation=
Photo=Loihiflank.jpg
Photo caption= Yellow iron oxide covered lava rock on the flank of Lōokinaihi.Lōokinaihi is a
seamount and underseavolcano in the Hawaiian archipelago, located at 18.92° N, 155.27° W — roughly 30 km (19 mi) south of the southeast coast of the Island of Hawaiokinai. It is one of three active volcanoes (the other two areMauna Loa and Kīlauea) thought to presently sit over theHawaii hotspot . The greatest distance between the summits of these volcanoes is about 80 km (50 mi), approximately the diameter of the hot spot. Lōokinaihi has yet to build to the surface of the ocean, although it is now over 3,000 m (10,000 ft) high (taller thanMount St. Helens ). The top of Lōokinaihi lies 975 m (3,200 ft) below the surface. [ [http://www.volcano.si.edu/world/volcano.cfm?vnum=1302-00- Smithsonian Institution Global Volcanism Program: Loihi Seamount] ] If the rate of upward building is about the same as nearby Kīlauea, Lōokinaihi should appear at the surface in several tens of thousands of years.Like Kīlauea, Lōokinaihi lies on the flank of
Mauna Loa , the largestshield volcano on the planet. The summit has acaldera -like depression, and three craters. The crater called Pele's Pit is known to have formed in July 1996 when a vent collapsed forming a depression with 200 m (660 ft) high, vertical walls. Therift zone for this volcano is about 31 km (19 mi) long and oriented northwest-southeast across the 2.8 by 3.7 km (1.7 × 2.3 mi) caldera. The eruption in 1996 was confirmed by scientists at the University of Hawaiokinai, becoming the first such confirmation of an active eruption occurring on a seamount. In 1997,cite web |url= http://www.hanahou.com/pages/magazine.asp?Action=DrawArticle&ArticleID=573&MagazineID=37 |title= Earth, Whales & Fire |author= Michael Shapiro |work=Hana Hou! Vol. 10, No. 3, June/July 2007 |publisher= Photo by Wayne Levin |quote= In 1997, University of Hawai‘i scientists installed the Hawai‘i Undersea Geo-Observatory (HUGO), a submarine observatory designed to monitor a newly hatched volcano… Among HUGO's instruments was ahydrophone (a submersible microphone) to listen in on the eruption… HUGO went offline in 1998 after its power supply failed, but it left behind hours of recordings of haunting, unearthly sounds that had never before reached human ears: humpback whales singing against the backdrop of a volcanic eruption. ( [http://www.soest.hawaii.edu/HUGO/about_hugo.html About HUGO, on the Loihi Seamount] .)] the university installed a submarine observatory on the summit of Loihi Seamount. Another active undersea volcano, named Vailuokinauluokinau, was confirmed in 2001 in the Manuokinaa Group,Samoa .Lōokinaihi is being studied by manned
submersible dives to its surface and placement of recording instruments and remote observatories on the summit. The volcano is actively ventinghydrothermal fluids and thermal vents there are being studied forthermophilic extremophile s (organisms associated with extreme temperature conditions). In 1999, a never before seen jelly-like organism surrounding the 160°C vents was collected forincubation and study at NSF'sMarine Bioproducts Engineering Center (MarBEC).References and external links
* Hazlett, R. W., and D. W. Hyndman. 1996. "Roadside Geology of Hawaiokinai".
* [http://www.soest.hawaii.edu/GG/HCV/loihi.html Hawaiokinai Center for Volcanology] , University of Hawaiokinai.
* [http://hvo.wr.usgs.gov/volcanoes/loihi/ Lōokinaihi Seamount] — USGS website.
* [http://www.oar.noaa.gov/spotlite/archive/spot_loihi.html Lōokinaihi Submarine Volcano: A unique, natural extremophile laboratory] — NOAA research site.
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