2 historic sites 0 scheduled monuments 4 listed buildings 1 archaeological periods

LOUGH ROAD covers 5.8 km² in Northern Ireland. With 2 historic sites and 0 scheduled monuments on record, the ward sits at the 14th percentile across all 462 NI wards for combined archaeological heritage. It also records 4 listed buildings (HED Historic Buildings Record), the 18th percentile for listed-building density across NI wards. Per 1,000 residents, this works out at 1.1 recorded sites — the 10th percentile across NI wards (a measure of heritage density relative to current population). All dated archaeological evidence falls within the Mesolithic period. The recorded total is low relative to the ward's area. In Northern Ireland this typically reflects limits of survey coverage rather than a genuine absence of past activity.

Detailed boundary map of LOUGH ROAD ward, Armagh City, Banbridge and Craigavon
LOUGH ROAD boundary detail
Regional context map showing LOUGH ROAD ward within Armagh City, Banbridge and Craigavon
LOUGH ROAD in regional context

Heritage at a glance

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

2
Historic sites
19th percentile
0
Scheduled monuments
17th percentile
4
Listed buildings
18th percentile
1.04
Sites per km²

Population context

974
Persons per km²
81st percentile
1.1
Sites per 1,000 residents
10th percentile
5,601
Total residents (2021)

The recorded heritage of LOUGH ROAD

Of the 2 historic sites recorded, the most common are Standing Stone (Unlocated) (1, 50% of historic sites) and House & Bawn: Woodville House (1). For Standing Stone (Unlocated)s, this is the 0th percentile across NI wards that record this type. For House & Bawn: Woodville Houses, this is the 0th percentile across NI wards that record this type. Across the ward's 5.8 km², this gives a recorded density of 1.03 sites per km² (all heritage types combined).

Most common monument types

TypeCountDescription
Standing Stone (unlocated) 1
House & Bawn: Woodville House 1

Chronological distribution

Mesolithic
2

Terrain and environment

Mean elevation of 36m sits around the NI median (27th percentile). The terrain is broadly flat, with a mean slope of 3.1° (19th percentile across NI). The Topographic Wetness Index of 10.9 (77th NI percentile) indicates moderate drainage, balanced between upland shedding and lowland accumulation. The land-cover mosaic combines urban land (36%), improved grassland (36%), and woodland (27%), giving a mixed agricultural and semi-natural landscape. In overall character, this is low-lying, gently-sloping terrain — characteristic of NI's lowland basins and coastal plains, with land use dominated by urban land.

Terrain measurements

Mean elevation35.6 m 28th pct
Max elevation51.6 m 15th pct
Mean slope3.1° 19th pct
Wetness index (TWI)10.91 77th pct
Grassland36.0% 36th pct
Woodland26.9% 73rd pct
Cropland1.1% 51st pct
Urban land36.1% 72nd pct

Where this ward sits in NI

Elevation
28th
Slope
19th
Drainage
77th
Grassland
36th
Woodland
73rd

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

The placename record for this ward is small — 4 names in total — but it does include 1 ecclesiastical placename. With this few records, the count should be treated as indicative rather than a firm characterisation.

Placename categories

Ecclesiastical (kil-, temple-, monaster-)1 name

Recorded historic sites

NamePeriodType
HOUSE & BAWN: WOODVILLE HOUSEMesolithicDefence
STANDING STONE (unlocated)MesolithicRitual/Funerary

Listed buildings in LOUGH ROAD

Address / NameGradePeriod
WOODVILLE HOUSE LOUGH ROAD LURGAN CO.ARMAGHB
DERRY LODGE 29 LOUGH ROAD LURGAN CO.ARMAGHB1
LURGAN COLLEGE COLLEGE WALK LURGAN CO.ARMAGHB1
FALLOWFIELD SCHOOL LOUGH ROAD LURGAN CO.ARMAGHB1

Discover more in Armagh City, Banbridge and Craigavon

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.