Iceland review - 2015, Qupperneq 33

Iceland review - 2015, Qupperneq 33
ICELAND REVIEW 31 Jónsdóttir, coordinator of the Icelandic Met Office’s natural hazards division. The Met Office monitors 70 seismographs and 70 GPS sensors located on volcanoes and in seismically-active areas in Iceland and its staff were quick to put up more meters in the Bárðarbunga area. Kristín adds that because of the EU-funded research project Futurevolc, which had been launched prior to the eruption, important instruments had already been installed in the field, stream- ing data real-time, so the developments in the volcano could be followed closely. “The earthquakes moved away from the caldera, to the northeast and north,” Kristín describes of the development. The pattern indicated that magma was channeling its way underground, creating a 48-km (29- mile) long intrusive dike, which ended in the already existing Holuhraun lava field, north of the glacier. “It was a relief,” Kristín admits. “A minor sub-glacial erup- tion did occur but it was extremely lucky that magma didn’t surface through the ice. There was no ash, no floods.” After an eruption which lasted a few hours on August 29, a 1.5-km (1-mile) long fissure opened up, spewing 1,175°C (2,150°F) hot lava from three craters, Suðri, Baugur and Norðri, as high as 100 meters (328 feet) into the air. Lava flowed over the old lava field, onto the sands around it and into the riverbed of glacial river Jökulsá á Fjöllum, which retreated. “The lava spread out over a plain of fine sand in an area called Flæðurnar, north of Dyngjujökull [outlet glacier], which gets whirled up by the wind, causing sand- storms—an annoyance for people in East Iceland. Now the lava binds a large part of the dust,” Kristín reveals. Eventually, the new lava field stopped expanding and start- ed thickening, while the edges around the craters grew taller. The eruption remained fairly stable until mid-January. One month later it was reported that the eruption was likely to be in its final days. BIGGEST AND HOTTEST The Holuhraun eruption is the largest lava eruption in Iceland since the 1783- 1784 Laki eruption. During the Holuhraun eruption, 1.5 cubic km (0.36 cubic miles) of lava were emitted, covering 85 square km (33 square miles), which is the same size as Iceland’s largest lake, Þórisvatn in the south- ern highlands. For comparison, Manhattan measures 59 square km. Holuhraun is also the ‘hottest’ eruption the world has seen this century, at one point releasing one third more energy than Russian volcano Tolbachik, which erupted in 2012-2013 and placed second on the list, as concluded in a study led by Robert Wright of the Hawaii Institute of Geophysics and Planetology. The lava is approximately 40 meters (131 feet) thick at the lava field’s highest points. The crater is 70 meters tall, 100 meters wide and 600-700 meters long. The average thickness of the lava is 15 meters, or similar to a five-story building. GAS, GAS, GAS Even though Holuhraun was the biggest eruption Iceland has seen in centuries, it occurred in a favorable location in the remote northeastern highlands, pos- ing no direct threat to inhabited areas. Nevertheless, toxic volcanic gases, primar- ily sulfur dioxide (SO2), have proven a hazard with Holuhraun being the most gas-intensive eruption in Iceland since the 18th century. At the eruption site, where gas masks and gas meters are a requirement, SO2 levels have reached 130,000 µg/m3, while 21,000 µg/m3 is the highest level recorded in an inhabited area, in Höfn, Southeast Iceland, in late October. At lev- els above 2,000 µg/m3—which have been recorded across the country—warnings are issued and people advised to stay inside with the windows closed and heaters on. As a reference, an hourly concentration of 350 µg/m3 is the maximum safe limit for human exposure. While SO2 hasn’t been picked up in inhabited areas since the eruption ended, gas is still being released at the eruption site as it takes months or years for the lava to degas. “During a recent fieldtrip we measured high levels of gas, even with the strong wind. There was still a distinct haze over the lava field,” describes Sara Barsotti, coordinator for volcanic hazard at the Icelandic Met Office, of the scene in mid-March. “It will not be safe to walk on the lava for several months to come.” Samples taken in all regions have indi- cated that snow has turned acidic as a result of the volcanic gases. “A research project is ongoing. Samples from fishing rivers and water reservoirs will be taken in spring but all this changeable weather has helped—some of the toxins have already been washed away,” Víðir Reynisson, direc- tor of the Department of Civil Protection and Emergency Management, states. “The levels will peak immediately after spring thaw but this will not be a lasting problem.” Víðir is confident that come summer, it will be safe to release sheep to the highlands, as is customary in Iceland, and for hikers to drink water from brooks. RISING AGAIN Bárðarbunga is one of the biggest volcanoes in Iceland and has produced massive erup- tions in the past. Scientists disagree wheth- er it will erupt again in the near future.
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