Cairnduff | |
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Stewarton, East Ayrshire, Scotland | |
Cairnduff Bronze Age Burial Mound | |
Coordinates | 55°40′26″N4°30′45″W / 55.673995°N 4.5126024°W Coordinates: 55°40′26″N4°30′45″W / 55.673995°N 4.5126024°W |
Grid reference | grid reference NS42094514 |
Type | Burial Cairn |
Height | 0.7 metres |
Site information | |
Owner | Private land |
Open to the public | Yes |
Condition | Extensive robbing damage |
Site history | |
Built | Unknown |
Materials | Boulder banks |
Cairnduff,Cairn Duff or Carn Duff [1] is a roughly circular Bronze Age burial cairn, [2] located on the lands of High Peacockbank Farm near the town of Stewarton in East Ayrshire, Scotland. It was built around 3000 years ago.
Cairnduff is situated on the summit of Cairnduff Hill [2] at 114m [3] and Smith points out its prominence and that it is visible from the possible moot hill or watchtower site near High Castleton in the vicinity of Lainshaw House. [2] The position gives clear views of Strathannick and the surrounding hills to the north and south-west.
Cairnduff is a type of tumulus, barrow or burial mound dating within the time period approximately 1300–700 BC, the Bronze Age. The term cairn is typically given to such structures in Scotland and refers to a stone pile, built and not of natural origin. The descriptive term cairn in this context is itself derived from the Scottish Gaelic : càrn [ˈkʰaːrˠn̪ˠ] (plural càirn [ˈkʰaːrˠɲ] ). [4]
The centre of this once circular cairn has been entirely removed due to the robbing of stones and only a low, roughly circular stoney bank around a 1.0m wide and a maximum of 0.7m high remains. Turf-covered, the cairn is located within a rectangular field bank. A significant quantity of rounded stones are still present and some are exposed to view in situ or spread around the site. A few larger boulders, possibly perimeter stones are present and the indications are that the diameter of the cairn may originally have been over 20m. [5] The stones are whinstone and mostly large. [6] No hammer or chisel marks were found on any of the stones. [6]
The three urns found were buried in pits that were close to the original ground level. One urn was around a foot in diameter and the other two were 5½ inches in diameter and six inches in height, [7] with zig-zag lines around the rim. [6] In 1820 it was recorded that other urns might be present "as not more than a fourth part of it has yet been examined". [6] A height of 5 to 6 feet measured in 1820 with stones possibly removed previously for road building, etc. [6]
The site was wooded in 1779 as shown on the Lainshaw Estate map. The cairn with its contents of three cinerary urns was exposed when trees were being removed by uprooting them from this small plantation in around 1810 [2] to 1826. [8] These urns or beakers are recorded to have contained bones. [8]
The Black Hill Cairn is a Bronze Age burial site near Kirkfieldbank in the Clyde Valley and is set in a similar location to Cairnduff at the highest point in the area.
The Lainshaw Estate map of 1779 shows a Cairnduff Park and below it a Bonfire Park running down to the Annick Water. The cairn itself is not named or indicated and only a small clump of trees is shown in its location, lying just outside the Lainshaw Estate on the lands of High Peacockbank. [9]
Circa 1810 [2] or 1826 [8] Mr John Deans of Peacock Bank (sic) decided to extract some small trees from his plantation on Carnduff Brae when he exposed three urns or beakers that contained bones. The position of the urns within the cairn was covered with a considerable quantity of stones and earth. [8] The stones would have had to be collected and carried to the site, probably from the river as many are rounded and river worn. No detailed description of the urns survives other than some details of the size and their present location is not recorded.
By 1857 Mr. James Neilson Provan of Peacockbank was the landowner. The urns contained bones and relics and these vessels were found enclosed in small excavations that were close to the original ground level. One urn, around a foot in diameter, was broken whilst being removed. The remaining two urns had a diameter of 5½ inches and were six inches in height. They were made from coarse clay. [7]
The field name 'Bonfire Park' suggests that the cairn, located at the highest point of ground overlooking Stewarton, may have been the site of traditional bonfires, such as those related to Halloween.
The typical burial ritual of the time involved the corpse being laid under a funeral pyre and burnt, together with any artefacts. Once cremated the surviving bones were carefully separated from the ashes and placed inside an urn that was inverted and buried in a pit. The ashes, charcoal and other remains of the pyre may have been buried in a pit nearby. The whole was covered in stones and earth to form a cairn. [10]
Cairnpapple Hill is a hill with a dominating position in central lowland Scotland with views from coast to coast. It was used and re-used as a major ritual site over about 4000 years, and in its day would have been comparable to better known sites like the Standing Stones of Stenness. The summit lies 312 m above sea level, and is about 2 miles (3 km) north of Bathgate. In the 19th century the site was completely concealed by trees, then in 1947–1948 excavations by Stuart Piggott found a series of ritual monuments from successive prehistoric periods. In 1998, Gordon Barclay re-interpreted the site for Historic Scotland. It is designated a scheduled ancient monument.
Stewarton is a town in East Ayrshire, Scotland. In comparison to the neighbouring towns of Kilmaurs, Fenwick, Dunlop and Lugton, it is a relatively large town, with a population estimated at over 7,400. It is 300 feet above sea level. The town is served by Stewarton railway station.
There are many large stones of Scotland of cultural and historical interest, notably the distinctive Pictish stones, but also the other types discussed below.
Chapeltoun is an estate on the banks of the Annick Water in East Ayrshire, Scotland. This is a rural area famous for its milk and cheese production and the Ayrshire or Dunlop breed of cattle.
Lambroughton is a village in the old Barony of Kilmaurs, Scotland. This is a rural area famous for its milk and cheese production and the Ayrshire or Dunlop breed of cattle.
The old Barony and castle of Corsehill lay within the feudal Baillerie of Cunninghame, near Stewarton, now East Ayrshire, Scotland.
Carlin Stone or Carlin Stane is the name given to a number of prehistoric standing stones and natural stone or landscape features in Scotland. The significance of the name is unclear, other than its association with old hags, witches, and the legends of the Cailleach.
The Barony of Peacockbank was in the old feudal Baillerie of Cunninghame, near Stewarton in what is now East Ayrshire, Scotland.
The Lochridge estate was in the old feudal Baillerie of Cunninghame, near Stewarton in what is now East Ayrshire, Scotland.
The Barony of Aiket with its castle, lay within the old feudal bailiary of Cunninghame. The barony lands equate to the extant Parish of Dunlop, East Ayrshire, Scotland.
The Barony of Ladyland was in the old feudal Baillerie of Cunninghame, near Kilbirnie in what is now North Ayrshire, Scotland.
The Castle and Barony of Robertland is located near Stewarton, off the B769 road, in the old district of Cunninghame, Parish of Stewarton, and now part of East Ayrshire, Scotland.
The Lands of Lainshaw lie in Strathannick and were part of the Lordship of Stewarton, in East Ayrshire, Scotland. Lainshaw House is a category B listed mansion, lying in a prominent position above the Annick Water and its holm in the Parish of Stewarton, Scotland. Part of the much older Lainshaw Castle is contained within the several later building phases of the present day Lainshaw House. The names 'Langshaw' or 'Langschaw' were used in historic times. Law Mount near the High and Laigh Castleton farms has been suggested as the site of the original castle, granted in the 12th century to Godfrey de Ross by Hugo de Morville.
Bloak was a hamlet or clachan in East Ayrshire, Parish of Stewarton, Scotland. The habitation was situated between Auchentiber and Stewarton on the B778. It was originally built as a row of housing for crofters and farm workers. A small school remained open for some years after the hamlet ceased to exist.
Kingsford is a hamlet or clachan in Strathannick, East Ayrshire, Parish of Stewarton, Scotland. The habitation is situated on the B769, two miles north of Stewarton and fourteen miles from Glasgow.
The lands of Broomlands or Broumlands formed a small country estate about a mile to the east of Irvine, North Ayrshire, Scotland situated on the east bank of the Annick Water in the Parishes of Dreghorn and Irvine.
The Murder of Hugh Montgomerie, 4th Earl of Eglinton at the Annick Ford in Stewarton, East Ayrshire, Scotland, took place in 1586 as a consequence of a long running feud between the Montgomeries, Earls of Eglinton and the Cunninghames, Earls of Glencairn, families who were competing for power and influence locally and nationally. The significant repercussions of this act were felt throughout the county of Ayrshire and beyond. The spelling 'Montgomerie' is used throughout for both the family and Montgomery for the clan and clan and district names 'Cunninghame' in the same fashion.
Lainshaw Castle was a 15th century castle about 1.0 mile (1.6 km) south-west of Stewarton, East Ayrshire, Scotland, to the north of Annick Water. The castle was incorporated into Lainshaw House over the course of the 17th and 18th centuries.
Lawthorn is a hamlet near Perceton in Strathannick, Irvine, North Ayrshire, Scotland. The settlement lies on the old Irvine to Stewarton toll road.
Kemp Law Dun is a vitrified fort dating from the Iron Age situated near the town of Dundonald in South Ayrshire, Scotland. The remains of the Iron Age fort or dun lie on the old Auchans Estate in the Dundonald Woods near the site of the old Hallyards Farm and the quarry of that name. The footpath route known as the Smugglers' Trail through the Clavin Hills from Troon to Dundonald runs passed the ruins of the dun. Kemps Law is in the order of two thousand years old.
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