Iceland review - 2015, Síða 33

Iceland review - 2015, Síða 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.
Síða 1
Síða 2
Síða 3
Síða 4
Síða 5
Síða 6
Síða 7
Síða 8
Síða 9
Síða 10
Síða 11
Síða 12
Síða 13
Síða 14
Síða 15
Síða 16
Síða 17
Síða 18
Síða 19
Síða 20
Síða 21
Síða 22
Síða 23
Síða 24
Síða 25
Síða 26
Síða 27
Síða 28
Síða 29
Síða 30
Síða 31
Síða 32
Síða 33
Síða 34
Síða 35
Síða 36
Síða 37
Síða 38
Síða 39
Síða 40
Síða 41
Síða 42
Síða 43
Síða 44
Síða 45
Síða 46
Síða 47
Síða 48
Síða 49
Síða 50
Síða 51
Síða 52
Síða 53
Síða 54
Síða 55
Síða 56
Síða 57
Síða 58
Síða 59
Síða 60
Síða 61
Síða 62
Síða 63
Síða 64
Síða 65
Síða 66
Síða 67
Síða 68
Síða 69
Síða 70
Síða 71
Síða 72
Síða 73
Síða 74
Síða 75
Síða 76
Síða 77
Síða 78
Síða 79
Síða 80
Síða 81
Síða 82
Síða 83
Síða 84
Síða 85
Síða 86
Síða 87
Síða 88
Síða 89
Síða 90
Síða 91
Síða 92
Síða 93
Síða 94
Síða 95
Síða 96
Síða 97
Síða 98
Síða 99
Síða 100
Síða 101
Síða 102
Síða 103
Síða 104
Síða 105
Síða 106
Síða 107
Síða 108
Síða 109
Síða 110
Síða 111
Síða 112
Síða 113
Síða 114
Síða 115
Síða 116
Síða 117
Síða 118
Síða 119
Síða 120
Síða 121
Síða 122
Síða 123
Síða 124
Síða 125
Síða 126
Síða 127
Síða 128
Síða 129
Síða 130
Síða 131
Síða 132

x

Iceland review

Beinleiðis leinki

Hvis du vil linke til denne avis/magasin, skal du bruge disse links:

Link til denne avis/magasin: Iceland review
https://timarit.is/publication/1842

Link til dette eksemplar:

Link til denne side:

Link til denne artikel:

Venligst ikke link direkte til billeder eller PDfs på Timarit.is, da sådanne webadresser kan ændres uden advarsel. Brug venligst de angivne webadresser for at linke til sitet.