Scottish Archaeological Internet Reports (SAIR)

Society of Antiquaries of Scotland, 2012. (updated 2023) https://doi.org/10.5284/1017938. How to cite using this DOI

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Society of Antiquaries of Scotland (2023) Scottish Archaeological Internet Reports (SAIR) [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1017938

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Digital Object Identifiers

Digital Object Identifiers (DOIs) are persistent identifiers which can be used to consistently and accurately reference digital objects and/or content. The DOIs provide a way for the ADS resources to be cited in a similar fashion to traditional scholarly materials. More information on DOIs at the ADS can be found on our help page.

Citing this DOI

The updated Crossref DOI Display guidelines recommend that DOIs should be displayed in the following format:

https://doi.org/10.5284/1017938
Sample Citation for this DOI

Society of Antiquaries of Scotland (2023) Scottish Archaeological Internet Reports (SAIR) [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1017938

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The Excavation of an Early Bronze Age Burnt Mound at Arisaig, Lochaber, Highland

Suddaby, Ian

with contributions by Torben Ballin, Michael Cressey and Clare Ellis; and illustrations by Karen Clarke and Leeanne Whitelaw

Scottish Archaeological Internet Reports 39 (2009)

0903903592

Abstract: During the upgrading of the A830(T), the 'Road to the Isles', the remains of a disturbed burnt mound deposit were discovered and later excavated during September and October 2005 by CFA Archaeology Ltd. This is the first such feature to have been excavated in this part of the Highlands.

The burnt mound was discovered lying partly below a modern field bank on the edge of Arisaig during a trial trenching evaluation. Excavation demonstrated that the feature was formed in an active fluvial environment and that, despite the rural and boggy location, it had suffered considerable damage since its formation, caused by both the fluvial action of the adjacent stream and by a field drain. No evidence was found for either a hearth or a formal trough. The implication of a small assemblage of local quartz from within the burnt material is discussed. The charcoal assemblage is compared to spectra of pollen from contemporary deposits of peat in the area. Studies of the nature and origin of the burnt material via the results of soil magnetic susceptibility and thin-section analyses are presented. Six radiocarbon dates from three associated contexts span the period from 2550 to 1900 BC and suggest the burnt mound accumulated during the Early Bronze Age.


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