3 historic sites 0 scheduled monuments 0 listed buildings 1 archaeological periods

BALLYKEEL covers 4.4 km² in Northern Ireland. With 3 historic sites and 0 scheduled monuments on record, the ward sits at the 6th percentile across all 462 NI wards for combined archaeological heritage. Per 1,000 residents, this works out at 1.0 recorded sites — the 8th percentile across NI wards (a measure of heritage density relative to current population). All dated archaeological evidence falls within the Medieval period. Note: 67% of historic site records have unresolved period attribution; chronological figures reflect only the dated subset.

Detailed boundary map of BALLYKEEL ward, Mid and East Antrim
BALLYKEEL boundary detail
Regional context map showing BALLYKEEL ward within Mid and East Antrim
BALLYKEEL in regional context

Heritage at a glance

Percentile rankings throughout this profile compare each ward only against the other 461 Northern Ireland wards.

3
Historic sites
25th percentile
0
Scheduled monuments
17th percentile
0
Listed buildings
2nd percentile
0.69
Sites per km²

Population context

694
Persons per km²
71st percentile
1.0
Sites per 1,000 residents
8th percentile
3,026
Total residents (2021)

The recorded heritage of BALLYKEEL

Of the 3 historic sites recorded, the most common are Non-Antiquity – Drainage Feature (1, 33% of historic sites), A.P. Site – Circular Cropmark (1), and Motte And Bailey: Harryville Motte (1). For Non-Antiquity – Drainage Features, this is the 0th percentile across NI wards that record this type. For A.P. Site – Circular Cropmarks, this is the 0th percentile across NI wards that record this type. Across the ward's 4.4 km², this gives a recorded density of 0.68 sites per km² (all heritage types combined). Note: 67% of historic site records carry an 'Unknown' period attribution and cannot be placed chronologically; the chronological breakdown reported below reflects only the dated subset.

Most common monument types

TypeCountDescription
Non-antiquity – Drainage Feature 1
A.p. Site – Circular Cropmark 1
Motte And Bailey: Harryville Motte 1

Chronological distribution

Medieval
1
Unknown
2

Note: 67% of historic site records carry an ‘Unknown’ period attribution. The chronological breakdown above reflects only the dated subset.

Terrain and environment

Mean elevation of 56m sits around the NI median (45th percentile). Mean slope is 3.4° (30th percentile across NI), giving moderately undulating terrain. The Topographic Wetness Index of 10.8 (69th NI percentile) indicates moderate drainage, balanced between upland shedding and lowland accumulation. The land-cover mosaic combines urban land (40%), improved grassland (38%), and woodland (21%), giving a mixed agricultural and semi-natural landscape.

Terrain measurements

Mean elevation56.1 m 45th pct
Max elevation74.4 m 30th pct
Mean slope3.4° 30th pct
Wetness index (TWI)10.78 70th pct
Grassland38.1% 38th pct
Woodland20.8% 60th pct
Urban land40.3% 75th pct

Where this ward sits in NI

Elevation
45th
Slope
30th
Drainage
70th
Grassland
38th
Woodland
60th

Geology and preservation

The dominant bedrock formed during the Cainozoic era (Palaeogene period). Relatively young rock formed in the last 66 million years. In Ulster, Cainozoic basalt — the lava that created the Antrim Plateau and Giant's Causeway — dominates much of the eastern landscape. Bedrock composition is uniform (complexity index 0.00), with a single dominant geological unit underlying most of the ward. A uniform geology narrows the natural lithic-resource base available to past inhabitants.

Bedrock eraCainozoic
Bedrock periodPalaeogene
Surface depositsTill
Peat coverage0.0%
Bedrock complexity0.00

Placename evidence

Just two placenames are recorded for this ward in the combined OSNI, Logainm NI, and GeoNames sources. That is too few to support any meaningful characterisation of the linguistic heritage layers — diagnostic categories such as ecclesiastical, defensive, or Plantation-era names need a larger sample to be reliably distinguished from the generic Gaelic landscape vocabulary that is common throughout Ireland.

Recorded historic sites

NamePeriodType
A.P. SITE – circular cropmarkUnknownUnknown
MOTTE AND BAILEY: HARRYVILLE MOTTEMedievalDefence
NON-ANTIQUITY – drainage featureUnknownUnknown
Grounding History report mockup

Want a deeper view?

Grounding History: 10 Maps of Northern Ireland’s Past

A spatial history report bringing together analysis of all 462 wards into one place through 10 high-quality maps — covering monument density, archaeological periods, placename heritage, terrain, wetland, and the historic landscape at first survey.

About this profile

What is a ward?

A ward is the smallest electoral and statistical geography used by the Northern Ireland Statistics and Research Agency (NISRA). The boundaries used here are the 2014 NISRA / OSNI Wards (462 across Northern Ireland), each typically covering 1-700 km² and a population of a few thousand. Wards do not align with parishes, townlands, or any historic administrative unit — they are a modern statistical convenience, used here only as a fixed spatial frame within which to summarise heritage records.

What counts as a site?

Three distinct heritage record types are reported separately, not combined: (1) Historic Sites — entries in the Northern Ireland Sites and Monuments Record (NISMR), the inventory of recorded archaeological sites and findspots, dated from prehistoric to early-modern; (2) Scheduled Monuments — sites legally protected under the Historic Monuments and Archaeological Objects (NI) Order 1995 and maintained by the Historic Environment Division (HED); (3) Listed Buildings — buildings of architectural or historic interest protected under the Planning Act (NI) 2011 and graded A, B+, B1, B2, or Record-Only by HED. A site appearing in more than one register is counted in each register independently.

Editorial principles

These ward profiles describe evidence, not history. They report what is recorded, not what occurred. Where the data is ambiguous, we say so. We do not infer historical processes — population movements, settlement expansion, periods of decline — from patterns in the record. Absence of evidence is not evidence of absence: in Northern Ireland, where antiquarian survey was uneven and modern excavation is geographically biased, a gap in the record almost always reflects the limits of recording rather than a genuine historical absence. We mark such gaps explicitly where they appear in the data.

Limits of coverage and known caveats

Several caveats apply to every ward profile: (1) NISMR coverage is uneven across NI — some areas (notably parts of the south-east and the Belfast urban fringe) have been more intensively surveyed than others, so a low recorded site count does not reliably indicate a low past density of activity; (2) period attributions in NISMR are often 'Unknown', and chronological breakdowns reported here reflect only the dated subset; (3) placename classification depends on the Irish-language form (name_ga), which is recorded for approximately 50% of NI placenames in the combined sources, so ecclesiastical and pre-Christian counts may be understated where anglicised forms remain unparsed; (4) terrain percentile ranks compare each ward only to the other 461 NI wards; they are not absolute thresholds. For absence-dominant land cover categories (wetland, water, cropland), percentile ranks are suppressed below 1% raw value, since the ranking of zero-value wards is not meaningful.

Data sources (11)
Spotted an error? This dataset is updated continuously. Email contact@danielkirkpatrick.co.uk with corrections, missing records, or suggestions for improvement.