Archaeologia Islandica - 01.01.2002, Qupperneq 30

Archaeologia Islandica - 01.01.2002, Qupperneq 30
Timothy J. Horsley & Stephen J. Dockrill Figure 7 reveals that many of these anomalies have a regular form, with some linear and rectilinear features visi- ble. These are interpreted as being the responses to buried stone foundations for structures originally in these locations. As stated above, one of the aims of the surveys in this area was to locate any features associated with a church, and this has been achieved. A high resistance anomaly has been detected to the east of the main cluster, and in the area where the church was expected. Almost rectilin- ear, this anomaly could be structural in origin, but with anomalies only detected on three of the four sides. Although ori- ented east-west and about 6m x 4m, on its own this rather amorphous anomaly cannot be confidently identifíed as a church. However this anomaly is seen to be situated at the centre of a circular anomaly of low resistance, about 30m in diameter. This ring of low resistance might be due to an infilled boundary ditch or bank, and is consistent with a medieval Icelandic church. This was later confirmed by excavation when a number of graves were discovered within the area (Gestsdóttir 1999, 44). It does not appear that either method has detected these graves. A very subtle positive linear anomaly can be made out in the northeastem cor- ner of the survey area, and might be due to the buried remains of a bank, possibly a field boundary. Two linear low resistance anomalies have been detected to the west of the track, which could be interpreted as infilled ditches. However, these coincide with the positions of the ferrous pipe anomalies seen in the gradiometer sur- vey, and can be positively identified as the response to these modern pipe trench- es. Within the survey area to the east of the track, a number of linear high and low resistance stripes are visible. These are real anomalies, not survey defects, and can be seen to be on a slightly differ- ent orientation to the survey grid. During the data collection, a number of linear depressions were noticed on the farm mound, probably be caused by tread marks of a bulldozer employed to level buildings on the farm in the 1970s. These would certainly produce anomalies like those detected. When the results of both geophysical surveys over the farm mound are com- pared, it can be seen that the gradiometer survey has successfully detected the church anomaly as one of the areas of intense dipole anomalies. Other anom- alous areas can then also be confidently interpreted as being due to buried struc- tural remains, as they too coincide with areas of high resistance. Geophysical surveys within the farm of Hofstaðir have proved successful not only for the detection of anomalies, but also for the interpretation and assessment of buried remains at the site, therefore improving the archaeological under- standing of the site. Anomalies detected during the earth resistance surveys and subsequently con- firmed by excavation indicate that this technique has the potential to Iocate and identify cut features into sediments, in 28
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Archaeologia Islandica

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