Lewis, Eoropie
Settlement (Prehistoric)(Possible), Unidentified Pottery (Period Unassigned)
Site Name Lewis, Eoropie
Classification Settlement (Prehistoric)(Possible), Unidentified Pottery (Period Unassigned)
Alternative Name(s) Druim A' Sgeir; Taigh Jack Alasdair Bhig
Canmore ID 4421
Site Number NB56NW 5
NGR NB 5152 6507
Datum OSGB36 - NGR
Permalink http://canmore.org.uk/site/4421
- Council Western Isles
- Parish Barvas
- Former Region Western Isles Islands Area
- Former District Western Isles
- Former County Ross And Cromarty
NB56NW 5 5152 6507.
OS 6"record sheet held in the Royal Museum of Scotland (RMS).
Excavation (1977)
NB 515650 150m NW telephone kiosk. Stone slabs and bones were uncovered during the preparation of house foundations. Excavation was limited. Finds included large quantities of animal bones (cow, sheep, deer, pig) and of pottery fragments, hammer stones, pot boilers, a bone pin. Some of the pottery has been provisonally dated to the early Iron Age. Structures found included dry-stone walls; a paved area; an under-floor 'drain' covered by lintel-like slabs, leading to a stone-lined pit; a rough mound of flattened stones. Stone structures at this depth have been found on other occassions in this vicinity.
Ponting, M and G 1977
Excavation (1978)
Stonework of several structures overlain by midden material containing shellfish and animal remains were found during building operations. Apparently part of a complex of structures. Sherds of pottery of Iron Age type were found.
Hedges, M, Ponting, M and G 1978
Soil Sampling (4 March 2003 - 12 March 2003)
AOC Archaeology were grant aided by Historic Scotland for a second successive season of fieldwork related to a partnership project to assist a PhD studentship investigating the Marine Reservoir Effect, as well as a further project which includes analyses of Plaggan Soils. A total of 25 potential sites were visited to ascertain their potential for sample retrieval relating to the two projects described above.
None of the ecofactual or artefactual material noted at any of the sites visited could be described as being in secure contexts. The material was either within what appeared to be deposits interpreted as topsoil, in unstratified spreads, which were eroding out of the overlying eroding windblown sands, or in the case of Galston within deposits which appeared to have slumped down from above. In light of this no samples were taken for the PhD studentship concerned with the Marine Resevoir Effect. Some soil micromorphological samples were, however, taken in the connection with the study into Plaggan soils. These samples will be reported on at a later date.
AOC Archaeology - Alan Duffy (2003)
