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Tillydrone, Mote Hill

Mound (Period Unassigned)

Site Name Tillydrone, Mote Hill

Classification Mound (Period Unassigned)

Alternative Name(s) Seaton Park, Mote Hill; Aberdeen Cathedral Grounds; Tillydrone Motte

Canmore ID 20205

Site Number NJ90NW 8

NGR NJ 93665 08870

Datum OSGB36 - NGR

C14 Radiocarbon Dating

Permalink http://canmore.org.uk/site/20205

Ordnance Survey licence number AC0000807262. All rights reserved.
Canmore Disclaimer. © Bluesky International Limited 2025. Public Sector Viewing Terms

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Digital Images

Administrative Areas

  • Council Aberdeen, City Of
  • Parish Aberdeen
  • Former Region Grampian
  • Former District City Of Aberdeen
  • Former County Aberdeenshire

Archaeology Notes

NJ90NW 8 93665 08870

(NJ 9366 0886) Mote Hill (NR)

OS 1:10,000 map, (1974).

Location formerly entered as NJ 9366 0886.

See also NJ90NW 332.

For Seaton Park (centred NJ 9390 0910), see NJ90NW 407.00.

'Tillydrone', 'an ancient, artificial, earthen mound' (Ordnance Survey Name Book [ONB] 1867), is probably a motte (Simpson and Webster 1972). It is tree-covered and conical, 30 metres diameter at base, with a flat, oval top 9 metres by 5 metres. In height it is c.7 metres on the east and 5 metres on the west due to the slope of the ground.

Dr Simpson (Dr W D Simpson, Librarian, Aberdeen University), reported an encircling ditch, but this was not visible at the time of field visit. It is composed of fine, sandy soil containing very little stone (OS Field Surveyor JLD). Local tradition says it was erected as a beacon site.

Visited by OS (JLD) 12 September 1952.

Name Book 1867; C G Simpson and B Webster 1972.

This monument is situated on a NE-facing slope near the edge of a steep, high terrace and at an altitude of about 32m OD. It is within the area of a public park and may have had an encircling ditch.

NMRS, MS/712/83.

NJ 936 088 Six trenches were excavated on and around the mound known as Tillydrone Motte in October and November 2001. The excavation revealed that there had been a wooden palisade and stone revetment around the mound, but no dating evidence was found for any of the associated layers. A saddle quern reused in the stone revetment suggested a prehistoric site in the area. Charcoal layers were excavated from adjacent to the revetment, from a layer through which the defensive structure had been cut. A radiocarbon date of AD 170?45 was obtained for one of these layers. Trenches through the base of the mound revealed that there had been no surrounding ditch, and that small amounts of quarrying and reinstatement had taken place in the 19th or early 20th century.

Archive deposited in Aberdeen City SMR and the NMRS.

Sponsor: HS

A Cameron 2002.

(Classification changed to Mound). There is no evidence that this rounded hillock at Tillydrone, which lies in parkland 250m W of Aberdeen Cathedral (NJ 90NW 9), is a motte. The mound stands 7m in height, but it measures less than 10m across the top. As such, it is too small to provide sufficient space for a manorial establishment, though this does not preclude a purely military function as the site of a tower, like that excavated at Abinger in England, and noted by Kenyon.

Recent excavations have revealed that the lower part of the mound is natural, but no ditch was located around the base of the mound, only a stone revetment. A palisade cut into the natural mound overlay an Iron Age structure which was radiocarbon dated to 170 + 45 AD. Since no definitive medieval finds or features that would support a tower have been recovered, there is no conclusive evidence for it being used as a motte in the medieval period. However, the tradition of its use as a beacon cannot be discounted.

Visited by RCAHMS (PJD) 27 September 2001.

J R Kenyon 1993; A Cameron 2002.

Scheduled as 'Mote Hill, palisaded settlement and cairn... a prominent conical mound situated within Seaton Park... The mound stands on the edge of a steep, NE-facing slope running down to the River Dee, while the remaining approaches to the mound are open and relatively flat. The base of the mound is 30m in diameter while the summit is flat and oval-shapwed measuring 9m by 5m. The mound is 7m high on the easy and 5m on the west owing to the sloping ground.'

Information from Historic Scotland, scheduling document dated 6 January 2009.

Activities

Resistivity (May 1999)

The Motte is approximately 30 metres in diameter and stands about 9 metre high. The slope height is approximately 30 degrees except on the north face, which has eroded down a steep scarp. The ground East and West is park lawn with a serpentine pathway. The motte slope was surveyed by two traverses at right angles N to S and W to E plus a 5m top square.

On the Motte itself only two traverses were carried out, plus a small square on the summit. The traverses rose from the level ground at 30 degrees to the horizontal. At each 1.16-m step up the slope (i.e. 1-m horizontally) the readings rose very significantly, from about 400 ohms at the base to 2000 ohms at the 9-m summit. The rise in resistance readings moving west to east matched the rise in height, except at readings 9,10 and 11 where there was a slight inversion of this pattern. The same was noted in the cross traverse, moving from the summit north to south. The square on the summit shows several high resistance blocks that suggest archaeological anomalies. I would suggest that the inversion in the traverses are suggestive of encircling wall or revetment some two to three metres below the summit. (An excavation in Oct 2001 has uncovered what may have been a palisade and boulder revetment as here suggested.)

The 20-m square to the west of the Motte shows two, perhaps three dark areas of high resistance measuring 1 or two metres across. The shape is not distinct, but given that high pass filtering should have removed geological background, then it is likely that these are archaeological sources. There are trees in the vicinity and here again roots may be having an influence. Maps of the area suggest that vegetation in the recent past may have been altered, perhaps from more extensive wooding.

The 40x100-sq metre area east of the Motte shows several areas of potential archaeological interest. At the base of the Motte are two significant high resistance dark marks, which lie along a west to north curve of low resistance that could denote wall and a ditch encircling this side of the Motte. Moving east there are a few dark, high resistance patches, but the area is well treed and the roots may well be having an effect. From about 60 metres east there are some significant anomalies both very high and very low and of a non-natural appearance that suggests archaeological activity. The intensity in this region would suggest that minimal trial trenching should confirm this hypothesis. The white band across the plots is of course the existing 2-3-m wide pathway.

Watching Brief (15 November 2011 - 1 May 2012)

A watching brief was carried out from 15 November 2011- 1 May 2012 on trenches excavated for the City Centre Heating Phase 1 (Aberdeen City Council Planning references P110789, P111251 and change of route P120455). The trench for laying the pipes starts at The Beach Ballroom, Links Road (AB24 5NR), runs SW along Links Road, along Constitution Street, around Constitution Court, along Wales Street, across Park Street, along Frederick Street, north along King Street, Mealmarket Street, West North Street to Mitchell Hall (AB24 5AS) and also SW along Longacre and Queen Street to Grampian Police HQ and Aberdeen City Council Town House (AB10 1BS).

Information from Oasis (camerona1-125584) 24 July 2012

NJ 95273 07178 (Beach Ballroom) – NJ 94325 06603 (West North Street) – NJ 94325 06405 A watching brief was maintained, 17 November 2011 – 1 May 2012, during the excavation of trenches for new heating pipes. The trenches running from The Town House, Broad Street to Aberdeen Leisure Centre, Beach Boulevard were 1.5m wide and 1.2m deep. The foundations of 19th-century tenements were recorded in Broad Street and garden soils in Mealmarket Street.

Archive: RCAHMS

Funder: Aberdeen Heat and Power

Alison Cameron (Cameron Archaeology) July 2012

Note (March 2017)

Appearances can be deceptive – the motte that never was

Hidden in plain sight in Seaton Park, Aberdeen, Tillydrone Mote is a great example of how difficult it can be to accurately identify archaeological sites – even for those of us who are meant to be experts!

For most of its life, Tillydrone was declared to be a motte or castle mound, with its origins in the medieval period. And at first glance, there is no reason to doubt this interpretation. It bears all the hallmarks of a motte – a conical, flat topped mound, its base circa 30m in diameter, standing prominently in an elevated position in the landscape, in an area where other medieval sites have been recorded.

However, excavations carried out in the early 2000s at the behest of Historic Scotland, turned this interpretation on its head. The excavation revealed that far from being a mere 1000 years old, the mound was in fact closer to around 4000 years old.

While the lower part of the mound was seen to be natural, at its core was a large man-made stone structure which appears to have marked out an area used for burials during the Bronze Age.

An Iron Age site

The mound was reused in the Iron Age for an altogether different purpose, something more akin to that of a medieval motte. It appears to have been used as a small defended occupation site or “fortlet”, a palisade (wooden fence) having been built on one side of the mound with a stone revetment (which included a saddle quern) on the south east side. Within this defended area, multiple layers of occupation and demolition were recorded; one feature was radiocarbon dated to 170 +/- 45 AD while in another feature a sherd of mid-2nd Century AD Samian ware was found, definitively placing the use of this site in the Iron Age period.

Other artefacts found include a number of flint tools and a copper alloy ring, possibly part of a horse harness. Tellingly, no medieval artefacts were recovered.

No doubt there are more secrets buried within Tillydrone Mote. If there’s one thing this site teaches us it’s that you should not be afraid to question what’s gone before you - there is always more to learn!

Claire Herbert - Regional Archaeologist, Archaeology Service for Aberdeenshire, Moray, Angus and Aberdeen City Councils

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