Throughout last week, evaluative excavation was undertaken at Castle Island, Loch Kinord which was building on the underwater survey work conducted earlier this month (read about that HERE). The aim of the excavation was to establish the nature of this island, which has shown evidence below the water-line for being substantially artificial. The history of the island’s occupation stretches back at least as far as the first half of the 14th century, and radiocarbon dating has suggested occupation from as early as the 10th century. The excavation hoped to reveal evidence for even earlier use of the site.
The first discovery made was that the topsoil across the island is full of charcoal. It is presumed this is related to the destruction of the castle in 1649 by Act of Parliament and/or the final phases of occupation at Castle Island. It also appears that the Castle Island is at its core a natural deposit of material, almost certainly glacial in origin. However, it was also clear from the excavations (and submerged survey) that this island has been substantially modified, probably including levelling the top and scarping the sides to create the defences of the castle. This kind of construction has numerous parallels to medieval mottes and moated sites. Interestingly here though, is that this kind of construction is taking place on an island. While not a crannog in the classic sense, this modification of the island on such a complete scale would satisfy a number of criteria for classifying it as a crannog.
In addition to identifying the make-up of the island, the excavation also uncovered evidence for some structures on the island including an alignment of postholes, a very large pit (1.45m deep) and charred in situ timbers. The limited scale of the excavation make understanding these features’ purpose somewhat speculative, so an interpretation of the features will be reserved for a future post after further thought.
The excavation did not reveal that the island is wholly or mostly artificial as initially thought (and hoped) nor do we as yet have clear evidence for the construction and occupation of the site before the 10th century AD. Radiocarbon dating of some of the features identified in the excavation may yet indicate earlier activity, with results from C14 dating expected in the coming months. Regardless, Castle Island is an intriguing site, not least for its contemporaneous occupation to the classic style crannog 500m away, Prison Island, which has radiocarbon dates from the 9th and 12th centuries AD. Additionally, given that the site has not seen any disturbance other that the removal of timber from the surrounding loch bed in the 18th and 19th centuries, the preservation of this site should be considered outstanding with significant further potential.
This work was made possible by the help of volunteer excavators John Witold, Juliette Mitchell, Tessa Poller and my supervisor Gordon Noble. Thanks go to the Society of Antiquaries of Scotland who have provided funding for this excavation. Finally, thank you to Catriona Reid and the Muir of Dinnet Nature Reserve who have kindly granted permission for this work to take place.