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Skeleton in Cnoc nan Deiligeanan
When they were building the ROC hut at Cnoc nan Deilgeanan they found a body with its feet crossed inside a circle of stones with another stone on top. They gave it to Dr Bonner who sent it away somewhere. John George MacLean, Scarinish, 1/1994 -
An Carnan Liath ‘the gray cairns’
A green dome in a wet field in Heylipol, measuring 30 m in diameter and about 3 m maximum height. GPS is NL97050 43509. The dome has a central depression, and there appears to be a structure to it. The centre and east of the dome has a different vegetation with a lot of nettles and Rumex. There are the stony footings of a 10 x 5 m rectangular building to the east, which may be on the 1768 Turnbull map. -
Elizabeth Gibb Collection
Evelyn Elizabeth Balfour Gibb (née Milne) (1914–2000) was the daughter of Lady Frances Balfour, herself the daughter of the 8th Duke of Argyll. She married and lived in Sussex, but was a frequent visitor to the island, usually staying at The Lodge. She developed an interest in archaeology, and spent a lot of time in the 1970s and 80s roaming Tiree, particularly its Iron Age forts. She donated some material to the National Museum of Scotland, but this collection from 16 find spots was donated to An Iodhlann by her granddaughter Stephanie Clarke.
Dun, Caolas (which one is not described): 1983; 4 small sherds, 2 large pieces of slag.
Dun Mor Vaul: 13 thick sherds (2 rims, one of which is everted; 1 comb decoration), 1 possible lug.
Dunes between Brock and Ruaig Post Office: 11 small sherds.
Kirkapol: 1 sherd.
Dùn an t-Sìthein, Gott: 13 sherds (1 flat base).
Old Manse garden, Gott: 2 sherds.
Island House (possible location): hammer/smoothing stone (see photo).
Stream on boundary of Heylipol and Balinoe (NL 98686 42460): 9 sherds, 1 glazed pottery piece, 1 piece of slate, 1 of 3cm tapered nail, 1 hammer stone, whelk, limpet, scallop shells, animal bones and teeth, 4 bits of hard dark unidentified material.
Barradhu, Hynish: 1 piece of pumice, 2 small smoothing stones, 1 piece of slag, 1 limpet shell, 3 pieces of iron (possible cartspring).
Barradhu, Hynish (rock shelter): around 60 worked flints, 15 sherds (1 with comb decoration).
Dunes between Hynish Farm and Dùn nan Cleite: 1 worked flint (awl), 3 sherds, 1 3-cm iron cylinder with two notches (see photo).
Dùn na Cleite: 1972; 8 sherds (2 with everted rims and 1 with comb decoration), 1 worked flint, 3 animal teeth.
Dùn Hiader: 1972. 5 sherds (1 decorated, 1 with an indented, raised cordon), 1 smoothing stone, 1 hammerstone, 1 piece of iron 2 cm long, 1 piece of burnt bone.
Balephuil: 2 worked flints, 14 thick sherds, 1 small bone awl, 1 small pointed bone tool. ‘Sand dunes below Balephuil – just over the fence, not in the field you go down to the shore from, but the next along to the NW. 1982 May. Dr Brown knew this was an old settlement. Jean has a finger bone!’
Balephetrish: 1 hammerstone.
Sorisdale, Coll: 1 large fine sherd, 6 small sherds, 3 worked flints, 12 cowrie shells, 3 large pieces of bloom.
Included was a note [about possible rock art]: ‘I’m sure I found some [cup marks] on the non-seaward side of Dun Moor Vaul above the well/spring. I have a photograph somewhere. Quite small depressions in a circle about 12 of them. [?] “votive” holes in rock in Crete. 1994. EG’ -
Saddle quern
A saddle quern used as a coping stone in Fang a’ Bhàird ‘the sheepfold of the poet’ on Ben Hynish. A nearby cobble has been placed in it as a rubbing stone. These are prehistoric and are evidence that there was cereal grains were processed nearby. A number of saddle querns were found prominently in the sheepfold in Happy Valley. There may have been some superstition behind this.
See Joanna Close-Brooks (1983) Proc Soc Antiq Scot, 113, pp. 282–289:
‘Not much can be said about early prehistoric querns in Scotland since so few are published. There is no well-defined typology; some flat querns can readily be classified as saddle querns, and some deep ones as trough querns, but others hover between the two extremes. One must assume that early Neolithic querns were flattish saddle querns, and that later on trough querns came into fashion. These apparently flourished in the Bronze Age especially in northern Scotland. There are now radiocarbon dates of 1564 be ± 120 (BM-441) and 1760 be ± 55 (GrN-6168) from carbonized barley associated with part of a trough quern in the wall of a house at Ness of Grating, Shetland (Calder 1956, 353; Barcham 1980). In the Iron Age flat saddle querns reappear. This change is demonstrated at Jarlshof (Hamilton 1957, 49, 50), and Clickhimin (Hamilton 1968, 30, 64, 78), though the exact date at which it happens is not altogether clear. The preponderance of flat saddle querns on Iron Age sites is also shown by old excavations such as Duntroon, Argyll (Caulfield 1978, pi 8a). There seems to be a general, though not exclusive, tendency for earlier saddle querns to be a shallow scoop with a rim round the grinding area on some or all sides (fig 1, 2; fig 2, 4), whereas Iron Age querns are almost flat and worn right out to all edges, as can be seen in the photograph of the Duntroon querns mentioned above. This is also true of the large collections of saddle querns recently excavated at Broxmouth, East Lothian, and at Douglas- muir, Angus. On this basis the quern from Kilcoy III (fig 3) is likely to be of Iron Age date. The geographical extent of trough querns is unclear at present. Curie (1934, 301) coined the term ‘trough quern’ for the deep querns he found at Jarlshof. Though this type of quern is best known in Shetland, the type is also common in northern mainland Scotland, and a number of trough querns from Ross-shire and Inverness-shire are noted below. Beyond this, trough querns may occur even in southern Scotland.’ -
Trough quern
This trough quern was dug up in an old stackyard from the foundations of a shed in The Sliabh, Balephuil in 2010. It was broken when it was found. It was put as a coping stone in a drystone wall. It was made from a block of gneiss.
NL 97060 40793
Dimensions of stone: L50 x W50 x D24cm
Trough: L 40 x W 20 x D13 cm
It is prehistoric in date and was used for grinding grain.
See See Joanna Close-Brooks (1983) Proc Soc Antiq Scot, 113, pp. 282–289:
‘Not much can be said about early prehistoric querns in Scotland since so few are published. There is no well-defined typology; some flat querns can readily be classified as saddle querns, and some deep ones as trough querns, but others hover between the two extremes. One must assume that early Neolithic querns were flattish saddle querns, and that later on trough querns came into fashion. These apparently flourished in the Bronze Age especially in northern Scotland. There are now radiocarbon dates of 1564 be ± 120 (BM-441) and 1760 be ± 55 (GrN-6168) from carbonized barley associated with part of a trough quern in the wall of a house at Ness of Grating, Shetland (Calder 1956, 353; Barcham 1980). In the Iron Age flat saddle querns reappear. This change is demonstrated at Jarlshof (Hamilton 1957, 49, 50), and Clickhimin (Hamilton 1968, 30, 64, 78), though the exact date at which it happens is not altogether clear. The preponderance of flat saddle querns on Iron Age sites is also shown by old excavations such as Duntroon, Argyll (Caulfield 1978, pi 8a). There seems to be a general, though not exclusive, tendency for earlier saddle querns to be a shallow scoop with a rim round the grinding area on some or all sides (fig 1, 2; fig 2, 4), whereas Iron Age querns are almost flat and worn right out to all edges, as can be seen in the photograph of the Duntroon querns mentioned above. This is also true of the large collections of saddle querns recently excavated at Broxmouth, East Lothian, and at Douglas- muir, Angus. On this basis the quern from Kilcoy III (fig 3) is likely to be of Iron Age date. The geographical extent of trough querns is unclear at present. Curie (1934, 301) coined the term ‘trough quern’ for the deep querns he found at Jarlshof. Though this type of quern is best known in Shetland, the type is also common in northern mainland Scotland, and a number of trough querns from Ross-shire and Inverness-shire are noted below. Beyond this, trough querns may occur even in southern Scotland.’
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Sherd (rim)
‘Rim potsherd and a small part which has broken off of it. A fine, light grey/brown clay with a micaceous content. From the same vessel as A.1978.34.d.[2].’ -
Two sherds (rim)
‘Two potsherds comprising a large section of rim. Flat rim, of a fine, light grey/brown clay with a micaceous content. Dimples from shaping visible on exterior. Well-fired.’ Photo -
Four body sherds
‘Two large conjoining body sherds, and two small fragments, from a sizeable vessel. Exterior of light brown clay, containing heavy, dark brown grits.’ -
Five sherds
‘Five small potsherds of coarse orange fabric. Badly damaged. All A.1978.34.f potsherds are from the same vessel.’ -
Sherd (rim)
‘Rim potsherd of coarse orange fabric. Flat rim. Badly damaged. Conjoins with A.1978.34.f.[3]. All A.1978.34.f potsherds are from the same vessel.’