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Balbridie

Balbridie
Jielbeaumadier asnapio maison neolithique vda 2010.jpg
Reconstruction of a Neolithic long house of the type discovered at Balbridie
Location Banchory, Aberdeenshire
Coordinates 57°03′13″N 2°26′36″W / 57.05356°N 2.44325°W / 57.05356; -2.44325
Type Neolithic long house
Length 26 m (85 ft)
Width 13 m (43 ft)
Area 329.6 m2 (3,548 sq ft)
History
Founded Early to mid 4th millennium BC
Periods Neolithic
Site notes
Excavation dates 1977-1980
Archaeologists Nicholas Reynolds and Ian Ralston
Condition No extant remains
Ownership Historic Scotland
Management RCAHMS
Public access Yes
Designated 1978
Reference no. (CANMORE) 36669

Balbridie is the site of a Neolithic long house in Aberdeenshire, Scotland, situated on the south bank of the River Dee, east of Banchory. The site is one of the earliest known permanent Neolithic settlements in Scotland, dating from 3400—4000 BC, and the largest Neolithic long house to be excavated in Britain. In a European context, Whittle has indicated the rarity of such large Neolithic timber houses, citing Balbridie, a hall in Cambridgeshire and Fengate as a small set of such finds. Neolithic features found in a later excavations at Dreghorn included post holes indicating a large rectangular structure comparable to Balbridie.

The Balbridie site was discovered in 1976 by aerial photography carried out by the Royal Commission on the Ancient and Historical Monuments of Scotland. The unusually dry summer revealed previously undetected cropmarks suggesting a very large structure. Subsequent archaeological work on site allowed the conceptual reconstruction of an enormous timber structure including the identification of large timber postholes.

The vicinity of Balbridie includes a number of other notable archaeological features including the Neolithic site of Bucharn. Watt has pointed out that this local area attracted an unusual density of very early settlement in Scotland. Balbridie is not only close to the River Dee but also to the Elsick Mounth trackway, the route of early crossings inland through the lower Grampian Mountains.



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