Description

The monument comprises the remains of a dun, a prehistoric defended settlement, with an associated outwork and an adjacent enclosure and clearance cairns. The dun and its outwork are likely to date to the Iron Age (between 500 BC and AD 500) or earlier; the enclosure and clearance cairns are thought to be later additions. These features survive as earthworks on top of a natural coastal knoll, with elements of the dun wall exposed in places. The dun encloses a roughly circular space, measuring around 15m in diameter internally. The wall now appears as an overgrown bank of stony debris, standing up to 1.2m high. The entrance faces WSW and was approximately 1.5m wide. Around the base of the knoll on the S and W, there is an outwork comprising a further wall, with an entrance offset to the entrance to the dun. The enclosure lies immediately W of the dun and its outwork. It is roughly oval in shape, measuring approximately 14m by 12m internally. One of the three cairns is located within the enclosure; the other two appear to overlie its western edge. The monument lies in rough grazing at approximately 20m above sea level. It is located roughly half way along the E coast of the island of Lismore, overlooking the Lynn of Lorn and the Argyll mainland to the E. The monument was first scheduled in 1956, but the documentation does not meet modern standards: the present rescheduling rectifies this.

The area to be scheduled is irregular on plan and its boundary is the base of the rock outcrop on which the monument is sited. The scheduled area includes the remains described above, an area around them within which evidence relating to the monument's construction, use and abandonment may survive, and adjoining land essential for the monument's support and preservation, as shown in red on the accompanying map.

Source: Historic Environment Scotland

Statement of Scheduling

Cultural Significance

The monument's cultural significance can be expressed as follows:

Intrinsic characteristics

The dun occupies a site of great natural strength, on the summit of a knoll surrounded on the E, S and N sides by near vertical cliffs and a steep-sided gully. The footprint of the dun broadly covers the elongated summit, with only a small area to the N falling outside its circuit. The dun itself survives as the remains of a roughly circular wall-circuit, with an overall diameter of around 25m. The wall now appears as a stony bank spread to 5.5m wide on average, but some of the inner and outer facing stones have been recorded previously, leading researchers to suggest that the original wall-thickness was about 4.1m. The approach to the dun was from the W where a gentle slope offers relatively easy access. Within the entrance to the WSW, part of the passage-wall and an inner corner-stone were visible in 1968. Outside the entrance to the W and S, a concentric earthwork arc forms an outwork to the dun. A break in the W side of this feature is slightly offset from the dun entrance, but represents the likely access route through the outwork to the dun. The interior ground surface of the dun is uneven and is likely to contain structural remains and archaeological evidence of occupation. The enclosure to the W is situated on a level shelf immediately below the dun, but is probably later than the dun as it almost blocks the entrance through the outwork. At least two of the clearance cairns appear to overlie the enclosure and are likely to be later than both the dun and the enclosure. This evidence for a development sequence between the dun, outwork and enclosure adds to the archaeological significance and potential of the site.

Overall, the footprint of the monument is intact and it survives in reasonably good condition. Despite the relatively slight appearance of the perimeter wall today, there is high potential for the survival of buried deposits and features beneath and beyond the wall, within the dun interior, and within the outwork and enclosure. Future examination of the dun could provide detailed information about its date, form and construction, and the wider development sequence of the dun and its outwork and the enclosure. Investigation of the interior of the dun could contribute to our understanding of how it was used and how this may have changed over time. Buried artefacts and palaeoenvironmental evidence can contribute to our understanding of how people lived and worked, the extent and nature of trade and exchange, and the nature of the agricultural economy. The monument has the potential to contribute to our understanding of the nature of Iron Age settlement and the design and development of these small defended enclosures.

Contextual characteristics

This type of relatively small, defended settlement characterises much of the coastal occupation of Argyll and Atlantic Scotland in later prehistory. There are eight known duns on Lismore and almost 50 in the Lorn area. They belong to a much broader category of later prehistoric settlement, which includes brochs, forts, crannogs, duns and hut circles. Altogether, over 500 later prehistoric settlements are known in Argyll. It is believed that duns represent the remains of the living spaces of small groups or single families. They are largely a coastal phenomenon and tend to be located on locally high ground, along prominent coastal routes or within easy reach of the coast, as in this case.

The duns of Lismore are all sited on rock outcrops and take advantage of the natural prominence and defence they afford. Sean Dun has a seaward outlook and would have been clearly visible from the sea, which, combined with its prominent knoll-top position, suggest that defence and visibility were the chief factors that determined its siting here (rather than proximity to agricultural land, for instance). A series of duns and forts lines this coastline, while Dun Mor lies some 700m W and inland of Sean Dun. The relationship between the duns in the island merits further research, but it is likely that they formed part of a network of similar sites along the Lismore coast. Sean Dun is probably also broadly contemporary with the substantial broch at Tirefour and the possible broch at Loch Fiart. Sean Dun has high potential to contribute to our understanding of the Iron Age occupation of Lismore and further afield.

Associative characteristics

The site is labelled as 'Fort (Sean Dùn)' on the first edition Ordnance Survey map.

National Importance

This monument is of national importance because it has an inherent potential to make a significant addition to our understanding of the past, in particular, the design and construction of later prehistoric, small defended settlements in western Scotland, and their place in the wider economy and society. There is good potential for well-preserved archaeological remains surviving within and immediately outside the dun and its outwork. These buried remains can tell us much about the people who built and lived in the settlement and the connections they had with other groups. The loss of the monument would significantly diminish our future ability to appreciate and understand the occupation of Argyll in the later prehistoric and early historic periods.

Source: Historic Environment Scotland

Sources

Bibliography

RCAHMS records the site as CANMORE database reference 23012. West of Scotland Archaeology Service records the site as WOSASPIN 1202.

The site was considered as part of the Lismore Landscape Project in the early 2000s.

References

RCAHMS 1975, The Royal Commission on the Ancient and Historical Monuments of Scotland. Argyll: an inventory of the ancient monuments: volume 2: Lorn, p 92, no 193. Edinburgh.

Stoddart, S, 2005, Data Structure report. Version 2.0. Lismore Landscape Project, July-August, 2004. Circulated typescript report.

Stoddart, S, 2003, Lismore: Preliminary GIS work. [Draft] Circulated typescript report.

Source: Historic Environment Scotland