Volcano Watch: What Was Happening at Kīlauea Volcano 10 Years Ago?
Kīlauea has now passed the one-year anniversary of the episode 61g lava flow reaching the Pacific Ocean.
But what was this busy volcano up to a decade ago? Were things as dynamic then as they are now?
Slightly more than 10 years ago—on July 21, 2007—episode 58 of the ongoing East Rift Zone eruption got underway with a dramatic collapse of the Pu‘u ‘Ō‘ō crater floor. At the same time, new fissures opened high on the northeastern flank of Pu‘u ‘Ō‘ō. These fissures unzipped the ground and erupted lava to the northeast as far as the 1986-1992 Kupaianaha lava shield, about 2 miles downrift.
Activity soon became localized at the northeastern end of the new fissures. This vent, called Fissure D, produced a series of short-lived ‘a‘ā flows. By late August, the open lava channel feeding the ‘a‘ā flows began to overflow its banks. The overflows raised the enclosing levees to form a “perched” lava channel that eventually stood about 150 feet above the pre-existing ground!
This feature was somewhat unusual in that it represented a cross between an elongate lava channel and a lava lake. Perched lava ponds or lakes are formed by a similar process, with periodic overflows raising the levees and elevating the pool of molten lava above its surroundings. This process has been observed only once with Kīlauea Volcano’s current lava lake at Halemaʻumaʻu, but the phenomenon was common at summit lava lakes in the late 1800s and early 1900s.
The episode 58 perched lava channel provided some interesting observations of “seeps,” as they were called by USGS Hawaiian Volcano Observatory (HVO) geologists. The seeps, extrusions of sticky lava through the enclosing levees of the perched channel, produced short toothpaste-like flows adjacent to the channel.
Another early phase of episode 58 produced “rootless shields” south of Pu‘u ‘Ō‘ō. These broad, gently sloped accumulations (shields) of lava are called “rootless” because they are not situated over primary eruptive vents. Some of the rootless shields collapsed over time, providing new insights into the formation and destruction of these structures. Similar structures and related lava flows have also been reported in Iceland and recognized in satellite images of Mars.
Lava from episode 58 eventually formed a stable tube system that extended to the southeast and reached the ocean on March 5, 2008. This ocean entry was called Waikupanaha, which was about 2.4 miles east of today’s Kamokuna ocean entry.
Episode 58 endured until March 5, 2011. It was significant in several ways, primarily for increasing our understanding of Kīlauea and its volcanic processes.
It was also the first East Rift Zone eruption episode to occur simultaneously with an eruption at the summit of Kīlauea—the Overlook vent and lava lake within Halemaʻumaʻu, which opened in March 2008. Such synchronous eruptive vents separated by 12 miles continue today. The two ongoing eruptions offer tremendous opportunities to study the hydraulics of the magma plumbing and transport system between the summit and east rift of Kīlauea.
Episode 58 ended when the shallow conduit carrying lava from the main reservoir beneath Pu‘u ‘Ō‘ō to the Fissure D vent became plugged. This caused a back-up between Pu‘u ‘Ō‘ō and the summit magma reservoir, providing another data point in how the two parts of Kīlauea Volcano’s plumbing system influence each other.
Time-lapse images obtained by remote HVO cameras prior to and during episode 58 were compiled in a series of movies to illustrate Kīlauea in action. These short Quicktime files can be freely downloaded from the U.S. Geological Survey.
As the episode 61g lava flow enters its second year, HVO continues to track and study the dynamic processes of Kīlauea, one of the world’s most active volcanoes. Only time will tell what the next decade will bring.
Volcano Watch is a weekly article written by U.S. Geological Survey`s Hawaiian Volcano Observatory scientists and colleagues.