Follow site author @kenrubin on Twitter
January 3, 2014 marked the 31st anniversary of the Pu`u `O`o eruption on the
east rift zone of Kilauea Volcano. It has the distinction of being the
longest-lived rift zone eruption in the 200-year-long historic record of
Kilauea Volcano. It is also the most voluminous (>2.7 km3)
and one of the most compositionally variable (5.7-10.1 wt% MgO) in the
Kilauea historic record.
This on-going eruption has produced a broad field of new lava flows
that have buried over 117 sq km of the volcano's south flank
and added more than 230 hectares of new land to the island.
Lavas from this eruption have unfortunately destroyed several communities
and numerous man-made structures along the south coast of the Big Island of
Hawaii, including 189 houses, a National Park Service Visitor Center
at Waha`ula, a church, a store, the Waha'ula Heiau (a 700 year old
Hawaiian place of worship), and many other ancient Hawaiian sites.
The coastal highway in this part of the Big Island has been closed for
13 years, as flows covered 14 km of it with lava now as deep as 35 m.
The eruption started on 3 January 1983 when ground fissures opened up and "curtains of fire" (long thin fountains of molten lava) issued from a 7-km long discontinuous fissure system in the remote rainforest of the middle east rift zone of the volcano. From this "typical" sort of beginings a very atypical rift zone eruption unfolded.
By June 1983, the activity had localized to one central vent and there it stayed for the first 3.5 years (and 44 eruptive episodes) of the eruption. At times, spectacular lava fountains (up to 460 m) high could be seen throughout east Hawaii. During this period, the eruption settled into a regular pattern of brief eruptive episodes, each lasting less than 24 hrs (with the exception of the-384-hr-long episode 35A) and each separated by repose periods averaging 25 days. The fallout of cinder and spatter from the towering lava fountains built a cone at the Pu`u `O`o vent that was measured to be 255 m high by HVO. During this time, a shallow magma reservoir developed beneath the Pu`u `O`o vent. The reservoir was estimated from ground deformation to be 1.6-km long, 2.6-km deep but only about 3-m wide. This reservoir was open at the top, which promoted rapid cooling of the magma (believed to be at a rate of ~5% in 20 to 30 days).
In July 1986, the locus of lava production abruptly shifted 3-km downrift to form the Kupaianaha shield, which was active nearly continuous until early 1992 (Kupaianaha means "mysterious one" in Hawaiian). With this vent shift came a new eruption style: continuous, quiet effusion from a lava pond replaced the episodic high fountaining. Overflows from the pond built a broad, low lava shield. In November 1986, lava from Kupaianaha reached the ocean, some 12 km away. It covered the small community of Kapa`ahu in its path. Over the next five years, much of the lava erupted from Kupaianaha streamed directly into the sea via a lava tube system that led from the lava pond to the coast.
In 1990, the eruption entered its most destructive phase when flows flooded the village of Kalapana. Over 100 homes were destroyed in a 9-month period. Eventually, new lava tubes formed, diverting lava away from Kalapana early in 1991; Lava resumed ocean entry within the confines of the National Park. The volume of lava erupted from Kupaianaha declined steadily through 1991, particularly during and after episode 49, a 3 week period during which new vents formed along the rift zone in between Kupainaha and Pu`u `O`o. In early 1992, the Kupainaha vent died, marking the end of episode 48 of the eruption.
The eruption shifted back to to Pu`u `O`o in early 1992, where flank vents on the west and southwest sides of the cone constructed a new lava shield. Lava effusion has persisted more or less continuously at this location through the present, except for a brief eruption at Napau Crater, a few km to the west of Pu`u `O`o in late January 1997, followed by a two-month pause in activity at Pu`u `O`o. Lava flows now typically feed from the vents through lava tubes to the ocean, with few surface flows in between.
Activity within the past year at the Pu`u `O`o cone is detailed on our eruption update web page. This period has seen a collapse of the cone, a rapid buildup of the lava shield surrounding the cone, and a few overflow events this past summer, wherein lava actually spilled over the rim of the cone rather than feed out at its base through lava tubes.
Some Other Interesting Eruption Details...
You may be wondering just how much lava issues forth from Kilauea during an "average" Pu`u `O`o eruption day. Unfortunately, lava production rates are difficult to estimate. They appear to have fluctuated but have remained vigorous (300,000 to 600,000 m3/day) with no signs of slowing down or stopping over the long-term. However, the volcano did undergo a 24 day hiatus in all eruptive activity in early 1997, as it has done periodically in the past. There is thought to be a well developled magmatic plumbing system connecting the mantle source for the volcano (where rock is first melted to form magma) with the eruption site. Although the longevity of the current eruption is unique in the brief era of scientific observation at Kilauea, occasional long-lived rift zone eruptions during each 1000 years or so have probably been significant in building up the volcano [For instance, Delaney, 1993 (full reference is given below) estimated that the east rift zone may have experineced eruptions that lasted for most of a century].
With this sort of history, there is no reason to expect that this eruption will end any time soon simply because it has already lasted for so long. On the other hand, little is known about why some long-lived Kilauea east rift zone eruptions, like the 1969 to 1974 Mauna Ulu eruption, abrubtly stop.
You may be wondering what happens when molten lava interacts with the sea? Well, as indicated above, new lava has moved down the south flank of Kilauea through well-established lava tubes to the coastal plain during much of this eruption. Much of the lava from the tube system enters directly into the ocean and new land is built up (some of which then slides into the sea). In the process, a spectacular steam plume is created. This steam cloud is composed of predominantly water vapor, but also has a significant amount of SO2 (derived from S in the lava) and Cl (derived from sea water) in it, as well as tiny shards of volcanic glass. This situation makes viewing the eruption up-close hazardous to your health and contributes to the volcanic smog ("vog") that has plagued the southern parts of the Big Island (and other parts of the state) during this and other eruptions.
|HCV Home||Hawaiian Volcanoes||Loihi||Kilauea||Mauna Loa||Hualalai|
This page created and maintained by
The information on this page was compiled by Mike Garcia and Ken Rubin from personal accounts, HVO reports, and published scientific literature.
Other credits for this web site.
Last page update on 23 Jan 2014