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Latitude: 55.8757 / 55°52'32"N
Longitude: -4.856 / 4°51'21"W
OS Eastings: 221426
OS Northings: 668419
OS Grid: NS214684
Mapcode National: GBR 31.2T9C
Mapcode Global: WH2MN.CKVY
Entry Name: Kelly Bank Cottage, cairn 750m E of
Scheduled Date: 25 March 2011
Source: Historic Environment Scotland
Source ID: SM12840
Schedule Class: Cultural
Category: Prehistoric ritual and funerary: cairn (type uncertain)
Location: Inverkip
County: Inverclyde
Electoral Ward: Inverclyde South West
Traditional County: Renfrewshire
The monument comprises the remains of a cairn, built probably between 3000 and 1000 BC in the late Neolithic period or Bronze Age. It is visible as a low mound of turf-covered stones and lies in moorland at about 165m above sea level. The cairn lies on the W slopes of Berry Hill and is sited on a low hill above the N side of the Kelly Glen. There are extensive views to the west.
The upstanding remains of the cairn measure around 8m in diameter and stand to about 1m in height. The cairn is generally well-preserved, but there are two areas of localised robbing on the S and W sides.
The area to be scheduled is circular on plan, to include the remains described above and an area around them within which evidence relating to the monument's construction, use and abandonment may survive, as shown in red on the accompanying map.
Source: Historic Environment Scotland
Cultural Significance
The monument's cultural significance can be expressed as follows:
Intrinsic characteristics
Excavation suggests that many round cairns were used to cover and mark human burials in the late Neolithic or Bronze Age and date most commonly from the late third millennium BC to the early second millennium BC. This cairn appears to be largely undisturbed suggesting that archaeological information is likely to survive beneath its surface. The excavation of similar mounds elsewhere in SW Scotland shows that cairns often incorporate or overlie graves or pits containing cist settings, skeletal remains in the form of cremations or inhumations, pottery and flint work; comparable remains may exist beneath this cairn. These deposits can help us understand more about the practice and significance of burial and commemorating the dead at specific points in prehistory. They may also help us to understand the changing structure of society in the area. In addition, the cairn is likely to overlie and seal a buried land surface that could provide evidence of the immediate environment before the monument was constructed. Botanical remains, including pollen or charred plant material, may survive within archaeological deposits deriving from the construction and use of the cairn. This evidence can help us build up a picture of climate, vegetation and agriculture in the area.
Contextual characteristics
This monument belongs to a diverse group of up to 86 known or possible cairns in the former county of Renfrewshire, including some that have been destroyed by modern land use since they were recorded. The majority lie between 200m and 300m above sea level on the NE fringe of the uplands that define the southern edge of the Clyde Valley, but this example is part of a small group of cairns and cist graves that look west over the Firth of Clyde to southern Argyll and the Isle of Bute. The intensive use of the lowlands for agriculture, housing and industry, as well as the activities of archaeological researchers, have influenced the distribution pattern we see today and it seems certain that cairns would originally have been a feature of the lowlands as well as the uplands. Cairns seem to be positioned for visibility both to and from the site, tending to be located on hill tops, false crests and ridges, and are generally inter-visible. In this area, their position and significance in relation to contemporary agricultural land and settlement merits future detailed analysis.
This monument can be compared with three other cairns that lie to the north within a distance of 2.5km and with nine cairns that lie 6.5 km to the north-east, around Gryfe Reservoir. Survey work around the reservoir has revealed concentrations of late Neolithic or early Bronze Age pottery, as well as several hut circles, and similar remains may exist in the vicinity of this cairn. The monument can also be compared with excavated examples further afield, such as the cairn at East Green Farm, Kilmacolm, where at least two Bronze Age funerary urns were found, and that at South Mound of Houston, where the cairn covered a cist grave containing cremated human bone, a flint knife and a Bronze Age food vessel. Cairns were often long-lived foci of religious or funerary activity and have the potential to contain secondary burials. This longevity is demonstrated at South Mound of Houston, where the cairn re-used the location of a group of Neolithic pits and lay close to a probable cist cemetery. Cairns have the potential to further our understanding not just of funerary site location and practice, but also of the structure of early prehistoric society and economy. This cairn is smaller than the excavated examples in the vicinity and is therefore also important because it may represent a slightly different monument type.
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, particularly the design and construction of burial monuments, the nature of burial practices and their significance in prehistoric and later society. Skeletal remains and artefacts from cairns can also enhance our knowledge about wider prehistoric society, how people lived, where they came from and who they had contact with. This monument is particularly valuable because it is largely undisturbed and lies close to several other cairns and settlement sites. The loss of the monument would significantly diminish our future ability to appreciate and understand the placing of such monuments within the landscape and the meaning and importance of death and burial in prehistoric life.
Source: Historic Environment Scotland
Bibliography
The monument lies within the Renfrewshire Heights SSSI and SPA.
RCAHMS record the site as NS26NW8. The WoSAS SMR records the site as WoSASPIN 5855.
References
Alexander, D (ed) 1996, Prehistoric Renfrewshire; Papers in Honour of Frank Newall, Renfrewshire Local History Forum.
Newall, F 1962, 'Early open settlement in Renfrewshire', Proc Soc Antiq Scot 95 (1961-2), 159-70.
Source: Historic Environment Scotland
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