2008:065 - A1 Scheme 1, Newry, Glassdrummond – Site 10, Armagh

NMI Burial Excavation Records

County: Armagh Site name: A1 Scheme 1, Newry, Glassdrummond – Site 10

Sites and Monuments Record No.: N/A Licence number: AE/08/19

Author: Peter Bowen and E. Moore, ADS Ltd Unit 6, 21 Old Channel Road, Belfast, BT3 9DE.

Site type: Early Christian and post-medieval activity

Period/Dating:

ITM: E 706908m, N 828705m

Latitude, Longitude (decimal degrees): 54.196124, -6.361623

Excavation was carried out at Site 10 as part of the archaeological mitigation strategy for the A1 road improvement scheme, Beech Hill to Cloghogue, Carnbane, Co. Armagh. The pattern of cultural history for the region shows there has been intensive occupation right through from early times, with known archaeological sites ranging from the Neolithic (over 5000 years old) to mills that remained in use until only 100 years ago. The desktop assessment undertaken by Scott Wilson Scotland Ltd/Fergus McIlveen LLP revealed that the proposed development would impact directly on four archaeological sites: two standing stones, DOW040–036 and DOW046–44; two possible rectangular houses, DOW040–024; and a motte, DOW046–002, at Mount Hill. From records held by the Northern Ireland Environment Agency and additional aerial photographs, a further 25 potential archaeological sites were identified in the study area.
Site 10 was located on a rise on the north-facing slope. The site was divided into five excavation areas, A–E. The archaeological investigation took place between January and June 2008. The key features investigated include a substantial flat-bottomed ditch in Area A, a possible enclosure ditch, with a further three ditches, albeit less substantial, also excavated in Area B.
Evidence of pitting activity was also apparent throughout the site and several of the pits displayed signs of in situ burning, particularly in Area A. In addition, several isolated post-holes, a large post-medieval field boundary ditch and several field furrows were also excavated, some of which represent later agricultural land use. The natural subsoil on-site consisted of mid-brownish-orange silty sand and coarse decayed granite. Outcrops of granite were also observed.