May 27, 2010
A weekly feature provided by scientists at the Hawaiian Volcano Observatory.
Petrologic Monitoring of Kīlauea Volcano: An update for "Rockhounds"
Petrology is literally the "study of rocks," and looking carefully at the rocks coming out of a volcano is necessary in order to understand what's happening on the inside.
Erupting lava, including liquid and crystals, records the journey that magma takes from the mantle into the heart of the volcano and on to the surface.
Based on patterns of earthquakes and swelling and contracting of the summit, scientists have inferred the existence of a 2-3 cubic kilometer (0.5-0.7 cubic mile) reservoir of magma that is around 4 km (2.5 mile) below Halema`uma`u Crater. Because these patterns at the summit also correlate with events on Kīlauea's rift zones, a magmatic connection must exist between the summit magma reservoir and the rift zones.
What scientists have long speculated about, however, is the residence time of magma in the summit reservoir. Many assumed that the reservoir contains stagnant magma left over from past summit eruptions in 1982, 1974, or perhaps even decades earlier. In March 2008, when a new vent erupted at the summit, speculation about the age of the summit magma reservoir was laid to rest.
Like forensic scientists who identify carefully extracted DNA, petrologists can identify the "genetic signature" of magma from deep within the mantle by determining concentrations of specific elements that are present in trace amounts. By analyzing these trace elements in older lava, we know that the "mantle DNA" of magma feeding Kīlauea has evolved over time, even since the previous summit eruption in 1982.
Our analyses of Kīlauea's new summit lava confirm it to be a genetic match to lava erupting on the east rift zone. This petrologic evidence for summit-to-rift magma continuity is a milestone on our road to understanding the most studied volcano on earth. It shows us that the active magma pathways from Halema`uma`u to Pu`u `Ō `ō have been flushed of remnant magma and are now filled by a burgeoning supply of new magma from depth!
So, aside from having the same "mantle DNA," how does summit lava compare with lava erupting 21 km (13 miles) away on the east rift zone, and what does that comparison tell us about what's happening in the magma system from the Kīlauea's summit to its east rift zone?
At the summit, lava is erupted at about 1,170 degrees Celsius (2,140 degrees Fahrenheit) and often contains small, amber-green olivine crystals. Out on the rift zone, though, lava is erupting at about 1150 degrees Celsius (2,100 degrees Fahrenheit) and contains a mixed-up assemblage of crystals.
As magma or lava cools under normal circumstances, olivine crystallizes first, followed by pyroxene. "Rockhounds" detect the subtle mixture of amber-green olivine and forest-green pyroxene crystals in the majority of recent rift lava flows. However, some pyroxene crystals are found with scalloped and embayed edges indicating that they were dissolving in a higher-temperature magma in which olivine crystals are more likely to grow. In fact, some olivines have even crystallized around tiny remnants of dissolved pyroxene crystals!
These microscopic crystal relationships provide clear evidence for mixing between hotter, gas-rich "new" magma and cooler, degassed, pyroxene-bearing magma mush, before it is erupted on the east rift. We know that this pyroxene-bearing magma mush is recently derived from the mantle because it, too, has the same genetic signature.
The persistence of this mixed-crystal assemblage in east rift zone lava attests to the presence of magma mush along cooler margins of the active magma pathways, as well as in cavities and cracks within the shallow volcanic edifice. The hotter magma that recharges the edifice could also be mixing with the cooler magma in the summit reservoir, adjacent to the east rift conduit.
Petrology suggests that we have a lot to learn about the complexities of shallow magma storage and transport. The entire Pu`u `Ō `ō eruptive sequence, a prolonged period of magma replenishment, has allowed petrologists a unique view of happenings within and on Kīlauea volcano.
Kīlauea Activity Update
Reduced coastal plain surface flow activity and ocean entry vigor has been countered by an increase in activity upslope. As of Thursday, May 27, a large breakout high on the flow field had constructed a low shield topped by a lava pond. This breakout apparently captured much of the lava supply feeding the Ki entry.
At Kīlauea's summit, a circulating lava pond deep in the collapse pit within the floor of Halema`uma`u Crater was visible via Webcam throughout the past week. The lava level remained relatively steady most of the time, with only a few fluctuations in its depth. Volcanic gas emissions remain elevated, resulting in high concentrations of sulfur dioxide downwind.
Two earthquakes beneath Hawai`i Island were reported felt during the past week. A magnitude-3.2 earthquake occurred at 7:23 a.m. on Friday, May 21, 2010, H.s.t., and was located 5 km (3 miles) southwest of Kailua-Kona at a depth of 40 km (25 miles). A magnitude-2.4 earthquake occurred at 8:40 a.m. on Thursday, May 27, and was located 42 km (26 miles) west of Kailua-Kona, at a depth of 26 km (17 miles).
Visit our Web site (http://hvo.wr.usgs.gov) for detailed Kīlauea and Mauna Loa activity updates, recent volcano photos, recent earthquakes, and more; call (808) 967-8862 for a Kīlauea activity summary; email questions to askHVO@usgs.gov.
Updated: May 28, 2010 (pnf)