Jökull


Jökull - 01.01.2021, Síða 78

Jökull - 01.01.2021, Síða 78
Gísladóttir et al. The herders knew the area very well and had often been herding there either on foot or horseback. The annual sheep roundup took place according to a tra- ditional plan, with the first roundup for this season completed three weeks earlier (personal communica- tion, Þórarinn Eggersson, 13 August 2020). On 10 October, the three areas of Merkigil, Axlir and Sand- fell were herded to Atlaey (Figure 3). In the evening the herders went with their horses to the shepherd hut near the river Hólmsá (Figure 3) where they spent the night. On 11 October, the four areas of Brytalækir, Háfjöll, Utanundir and Öldufell were herded, on foot and horseback. By the end of the day all sheep were rounded and kept overnight be- tween Hólmsá and Leirá rivers. The sheep herders again stayed overnight with their horses at the shep- herd hut near Atlaey. It was a mild autumn day on 12 October 1918, and the sky was clear except for a greyish mist shroud- ing the Mýrdalsjökull ice cap, hiding it from view. The herders left Atlaey together and herded the flock south of the river Leirá. There the men separated: one group herded the sheep onwards to the Fossarétt sort- ing pens, while the other went off to round up sheep on the mountain Rjúpnafell. The Rjúpnafell group split in two, one group going west of the mountain to the pastures closest to Mýrdalsjökull, while the other went east of Rjúpnafell and worked the pastures to the east and south. Two men herded the so called Sandar (Figure 3) east of Rjúpnafell and the remaining group herded on the outwash plain area further to the east. The roundup went well, and by around 3pm on 12 October, the herders and sorters were in various loca- tions on the outwash plain in the Upphagar pastures between Rjúpnafell and the Skálm river, the northern part of Selhólmur and just south of Hrísneshólmur. Then, events unfolded rapidly. On Selhólmur, the men had taken a short break, and from one hillock there was a view to the west. One herder, Vilhjálmur Bjarnason from Herjólfsstaðir, noticed a commotion in the west and realised that an eruption had begun in Katla. Vilhjálmur (Bjarnason 1985, pages 159– 160) described what he saw: “I looked across the area around us and over towards the waterfall Hrúthálsa- foss (Figure 4). Although it was now some distance away, its sound reached us quite loudly, fluctuating with the wind. [I thought] [n]othing interesting about that, it was just the waterfall. But the waterfall was tricking my ears now. Of course, the sound of the flood had begun to merge with the noise of the wa- terfall, although we did not realise it. I looked further along the Hrútháls ridge, where the southernmost tip reached the outwash plain as a series of quite high sandy knolls that I knew well. But now I sensed a change there, something unexpected. A bank of fog was moving across, caused by the outburst flood of course, so that visibility was not good at this distance. I can hardly believe my eyes. Inside the fog every- thing seems to be in motion. What on earth is hap- pening? I wonder. I watched for a while, stunned by this terrifying sight. The flood that emerged east of the mountain Hafursey (Figure 3) raced across there and had barely begun to spread out. So it looked like a mountain side that hurtled forwards with a shifting surface on which dark icebergs towered and the flood- wave sprayed water in all directions, depending on how the crest of ice rolled forward. Katla! I immedi- ately thought.” After experiencing this, the companions hurried off, one to warn the men herding in the Upphagar pastures, others towards the sorting pen to warn the sorters. Bjarnason (1985, page 161) describes the flood in this area in more detail: “When we first saw the main flood, I estimated that it was about 5 km away from us, but on the outwash plain glacial water was flooding out, filling the Skálm [river] and several of its tributaries. This pre-flood, as you might call it, didn’t carry any ice to slow its progress, and was much closer than the main flood which rolled a mass of ice ahead of it, including towering icebergs. When we noticed this pre-flood, which was scarily close, it was obvious that it was more than enough to make the Skálm impassable once it reached its main course.” The sheep sorters were now becoming concerned. They had heard a strange hum and thudding that seemed to come from Mýrdalsjökull. One of the sorters, Sigurður Jónsson from Þykkvabæjarklaustur in Álftaver, rode along the Ljósavatnaháls ridge (Fig- ure 4), which commanded a good view of the sheep- sorting pen towards the northwest, and there he met 76 JÖKULL No. 71, 2021
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