Archaeologia Islandica - 01.01.2011, Side 23

Archaeologia Islandica - 01.01.2011, Side 23
ARCHAEOLOGICAL ASSESSMENT OF SELECTED SUBMERGED SITES IN VESTFIRÐIR sonar (Olavius, O. 1964). The side-scan sonar survey showed that the seabed in Paradís was similar to Hveravík, i.e. got deeper towards the east and was deepest along a cliff on the east side, about 30 - 40 meters. The sonar survey in Paradís showed only one site that was probably not a natural feature and could be a large man-made object. This site was positioned with a gps and will be examined in more detail at a later stage. One dive was carried out in Paradís bay to get an idea about the vegetation and the composition of the seabed. There is not much marine vegetation on the seabed in the bay and it is heavily silted, similar to Hveravík. The cliff on the east side was partially examined and it showed that the cliff face had collapsed in places through time, leaving large pieces of rocks and boulders on the seabed. The main reason for the deep sediments in Hveravík and Paradís is the river that runs into the bay, carrying with it considerable amounts of river sediments annually. Hveravík and Paradís are sheltered with little evidence of wave perturbation and currents are almost non-existent. These conditions cause the river sediments to accumulate on the seabed in the bays instead of being carried further out into the sea. Reykjarfjörður (Skrímslaíjörður) The Reykjarfjörður fjord is situated in the southern part of Ámeshreppur in Strandasýsla. The íjord is fairly large and lies in an east to west direction. The fjord has been occupied from the settlement to the present and farms are situated on the coastline. In the bottom of the fjord is a small settlement, Djúpavík, where a herring factory was built in the early 20th century. The factory has been abandoned for a long time but a small summer settlement has grown around the tourist industry at Djúpavík (Lámsdóttir, Bima et al. 2005). In 1615 three Basque whaling ships got caught in drift-ice where they were anchored on the north shore of the Reykjarfjörður fjord and were wrecked. Most of the crews managed to get ashore and sailed in their small whaling boats north along the coast of the Vestfirðir peninsula into the Isafjarðardjúp fjord. There they hoped to find other whaling ships and get a passage back home. However, the whalers were murdered by a band of armed men sent by local magistrate for some minor offence. The reasons behind this horrible crime are not fully known but it seems that the magistrate believed that the whalers had committed some crime that warranted such harsh measures (Kristjánsson, Jónas ed. 1950). The wrecking of the three whaling ships was documented in detail by the Icelander Jón Guðmundsson the leamed. In late September 1615 the three whaling ships were anchored just of shore by a farm called Naustavík (fig. 8). During the days before, ice had drifted into the fjord on the south side but on the 21st of September a sudden gale from the southwest pushed the ice to the northeast towards the whalers. The ice smashed into the ships and two of them immediately broke from their moorings. One was thrown against another ship and broke up 21
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Archaeologia Islandica

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