Archaeological Report - Ballinglanna North 6, Co. Cork (Ireland)

Eachtra Journal

Issue 10 [ISSN 2009-2237]

Archaeological Excavation Report
E3972 - Ballinglanna North 6, Co. Cork
Fulacht Fiadh and Pit

EACHTRA
Archaeological Projects

Ballinglanna North 6
Co Cork
May 2011

Client: Cork County Council

Project: N8 Fermoy to Mitchelstown
E No: E3972

Excavation Director: John Tierney

Written by: John Tierney

Co Cork

Excavation Director

John Tierney

Written By

John Tierney

EACHTRA
Archaeological Projects

CORK GALWAY
The Forge, Innishannon, Co. Cork Unit 10, Kilkerrin Park, Liosbain Industrial Estate, Galway
tel: 021 4701616 | web: www.eachtra.ie | email: info@eachtra.ie tel: 091 763673 | web: www.eachtra.ie | email: galway@eachtra.ie

© 2011
The Forge, Innishannon, Co Cork

Set in 12pt Garamond
Printed in Ireland

Table of Contents
Summary��iii
Acknowledgements��iii
1 Scope of the project ��iii
2 Route location�� iv
3 Receiving environment �� 1
4 Archaeological and historical background �� 3
Mesolithic(c�8000to4000BC)�� 3
Neolithic(c�4000to2000BC)�� 3
�
BronzeAge(c�2000to500BC)�� 4
IronAge(c�500BCtoAD500)�� 6
Earlymedievalperiod(c�AD500to1100)�� 7
Highandlatermedievalperiods(c�AD1100to1650)�� 8
Post-medievalperiod(c�1650tothepresent)�� 8
5 Site Location and Topography �� 9
6 Excavation methodology �� 9
7 Excavation results �� 11
Area1�� 11
Area2��12
Plantremains��18
�
Lithics��18
Charcoal��18
Radiocarbondate��22
8 Discussion ��23
9 References �� 27
Appendix 1 Stratigraphic Index ��30
Appendix 2 Site matrix �� 42
Appendix 3 Groups and Subgroups ��44
Appendix 4 Finds register ��48
Appendix 5 Plant remains �� 49
Appendix 6 Lithics report �� 52

i

List of Figures
Figure 1: The route of the N8 Fermoy to Mitchelstown Bypass overlain on the Ordnance
Survey Discovery Series map� �� 2
Figure 2: The route of the N8 Fermoy to Mitchelstown Bypass overlain on the first edition
Ordnance Survey map CO010, 011, 019, 020, 027 and 028� �� 5
Figure 3: The route of the N8 Fermoy to Mitchelstown Bypass overlain on the RMP map
CO010, 011, 019, 020, 027 and 028� The map is based on the second edition Ord-
nance Survey maps� ��10
Figure 4: Post-excavation plan of Ballinglanna North 6� �� 13
Figure 5: Post-excavation plan of Area 1 Ballinglanna North 6� �� 14
Figure 6: Post-excavation plan of Area 2 Ballinglanna North 6� �� 17
Figure 7: Section of trough C�79 and pit C�80� �� 19
Figure 8: Section of hearth C�24 and section of pit C�32� ��20
Figure 9: Early Bronze Age sites on and in the environs of the N8 Fermoy Mitchelstown� ��26

List of Plates
Plate 1: Pre-excavation view of burnt mound deposit C�2 facing south� �� 12
Plate 2: Post-excavation of re-cut trough C�79 and pit C�80 from south� �� 15
Plate 3: Post-excavation of hearth C�24 and stake-holes C�34, C�69-C�72 from south� �� 15
Plate 4: Post-excavation of pit C�22 from south� �� 18
Plate 6: Post-excavation of pit C�74 from north� ��21
Plate 5: Post-excavation of pit C�32 from east� ��21
Plate 8: Early Mesolithic flint blade E3972:1:1 ��22
Plate 7: Quartzite quernstone E3972:21:1 ��22

List of Tables
Table 1 Dimensions of troughs and pit �� 11
Table 2 Dimensions of stake-holes �� 16
Table 3 Dimensions of pits �� 16
Table 4 Radiocarbon dates from Ballinglanna North 6� ��22
Table 5 radiocarbon dates from the burnt mound sites on the N8 Fermoy to Mitchelstown��24

ii

Ballinglanna north 6-E3972 http://eachtra.ie/index.php/journal/e3972-ballinglanna-north6-co-cork/

Summary
The site at Ballinglanna North 6 was divided into two areas. An early Mesolithic flint
blade (E3972:1:1) was recovered from the topsoil. Area 1 comprised a burnt mound/
fulacht fiadh that extended beyond the limit of the excavation to the west. The mound
overlay a trough that had been re-cut. An Early Bronze Age date was returned for the
mound. Area 2 was located 65 m to the north of Area 1. A pit was located on the northern
edge of the area of excavation and extended beyond the baulk. A flint blade (E3972:21:2),
dating to the first half of the Neolithic and a fragment of a quern stone (E3972:21:1) were
recovered from the fill of the pit. Two hearths and associated stake-holes and two pits
dating to the early modern period were also excavated in Area 2. An early modern date
was returned for one of the hearths. The entire area of excavation was truncated by land
drains, furrows and field ditches.

Project Details
Road project name N8 Fermoy to Mitchelstown Bypass
Site name Ballinglanna North 6
Ministerial Order no. A040
E no. E3972
Site director John Tierney
Townland Ballinglanna North
Parish Kilcrumper
Barony Condons Clangibbon
OS Map Sheet No. CO027
National Grid Reference 181394 104453
Chainage 3300-3400

Acknowledgements
The senior archaeologist was John Tierney and the post-excavation managers were Penny
Johnston and Jacinta Kiely. Administration of the project was by Choryna Kiely and Fio-
na Greene. Illustrations are by Ben Blakeman and Maurizio Toscano. Photographs are by
John Sunderland, Hawkeye and Eachtra Archaeological Projects. Specialist analysis was
carried out by Mary Dillon, Penny Johnston, Farina Sternke and the 14 Chrono Centre
at Queen’s University Belfast. The project was funded by the Irish Government under the
National Development Plan 2007-2013 and was commissioned by Cork County Council
on behalf of the National Roads Authority. The project archaeologist was Ken Hanley.

1 Scope of the project
The archaeological works associated with the N8 Fermoy to Mitchelstown Bypass was
carried out on behalf of Cork County Council, National Road Design Office, Rich-
mond, Glanmire, Co. Cork. The project was funded by the Irish Government under the

iii

iSSUE 10: Eachtra JoUrnal - iSSn 2009-2237 archaEological Excavation rEport

National Development Plan 2007-2013. The total archaeological cost was administered
by the National Roads Authority through Cork County Council as part of the Author-
ity’s commitment to protecting our cultural heritage. The purpose of the archaeological
services project was to conduct archaeological site investigations within the lands made
available, to assess the nature and extent of any potential new sites uncovered and to
preserve by record those sites of agreed archaeological significance, as approved by the
Department of Environment, Heritage and Local Government in consultation with the
National Museum of Ireland.
Phase 1 of the project (archaeological testing of the route) was carried out in October
2005 under licence 05E1150 issued by Department of the Environment Heritage and Lo-
cal Government (DoEHLG). The principal aim of this phase of the project was to test for
any previously unknown sites by a programme of centreline and offset testing and to test
sites of archaeological potential identified in the EIS and geophysical surveying. Five Cul-
tural Heritage Sites were tested under individual excavation licences 05E1122-05E1126.
Phase 2 of the project (resolution) involved the resolution of all archaeological sites
identified within the proposed road corridor prior to commencement of the construction
of the bypass. This phase of the project was carried out from September 2006 to Septem-
ber 2007 and excavations were conducted under the management of a Senior Archaeolo-
gist. A total of 28 sites were excavated during this phase of works under separate licences
issued by DoEHLG.
A post-excavation assessment and strategy document was prepared in Phase 3 of the
project to present a management strategy for dealing with post-excavation work arising
from archaeological works along the route of the new N8 Fermoy to Mitchelstown By-
pass. It included a proposal for post-excavation and archiving work and a budget for the
works. The document detailed the location of the route, the receiving environment, the
archaeological and historical background, the scope of the project and the circumstances
and scope of fieldwork. The document presented a scheme-wide summary of the archaeo-
logical findings, a research framework within which the findings were dealt with and a
publication plan and dissemination strategy for the end results.

2 Route location
The route of the N8 Fermoy to Mitchelstown road is located in the rich pastureland of
North Cork (Figure 1). The project involves the construction of c. 16 km of the N8 from
Gortore north of Fermoy to Carrigane north-east of Mitchelstown. The N8 Fermoy to
Mitchelstown road passes through the townlands of Gortore, Ballynacarriga, Glenwood,
Ballinglanna North, Ballinrush, Caherdrinny, Gortnahown, Ballybeg, Turbeagh, Glena-
tlucky, Ballynamona, Kilshanny, Corracunna, Kildrum, Garryleagh, and Carrigane. The
townlands are located in the parishes of Kilcrumper, Glanworth and Brigown and Barony
of Condons Clangibbon, with the exception of Gortore, and Glenwood, which are
located in the Barony of Fermoy.

iv


The route begins at the northern end of the Fermoy Bypass at Gortore, c. 2km north
of Fermoy, and continues northwards across the River Funshion, and to the west of the
Glencorra Stream, a tributary of the Funshion, for 4 km. At Caherdrinny, it crosses over
the western extremities of the Kilworth Mountains. From there it descends north-east-
wards onto the broad plain that extends east and north-eastwards from Mitchelstown. It
crosses the existing N8 at Gortnahown and passes to the east of Mitchelstown, crossing
the R665 Mitchelstown-Ballyporeen road and links up with the N8 Cashel Mitchelstown
Road at Carrigane south of Kilbeheny and 2 km west of where the borders of the Cork,
Limerick and Tipperary counties meet.

3 Receiving environment
The topography of East Cork and Waterford consists of east/west valleys separated by in-
tervening ridges. The ridges consist of sandstones and mudstones of the Devonian Period
(Old Red Sandstone) laid down 355-410 million years ago and the valleys of Carbonifer-
ous limestones laid down 290-355 million years ago. The sediments covering many of the
rocks are mainly of glacial origin deposited by glacial ice or meltwater (Sleeman et al.
1995, 1).
The landscape of the area is dominated by the Galtee Mountains to the north, the
Ballyhoura Mountains to the north-west, the Kilworth Mountains to the east and the
Nagles to the south. The landscape is drained by the Blackwater River, the Funshion
River (which flows into the Blackwater River c. 2 km north-east of Fermoy), and the
Glencorra Stream, a tributary of the Funshion River. The largest population centres in
the area, Fermoy and Mitchelstown, have developed on the banks of the River Blackwater
and Gradoge (a tributary of the Funshion), respectively.
The route begins at Gortore, c. 2 km north of Fermoy, at an elevation of c. 40 m OD.
At Caherdrinny, it rises to its maximum elevation of c. 180 m OD as it crosses over the
western extremities of the Kilworth Mountains, before descending onto the broad plain
that that extends east and north-eastwards from Mitchelstown, at an elevation of 100-120
m OD.
The soils on the southern portion of the route are characterised by acid brown earths
derived from mixed sandstone and limestone glacial till. These soils occur generally in
the valleys of Cork and Waterford (Gardiner and Radford 1980, 61), and have a wide use
range, being suitable for tillage and grass production. The soils on the western limits of
Kilworth Mountains are characterised by brown podzolics derived from sandstone. The
soils on the northern portion of the route are characterised by brown podzolics derived
from sandstone and shale glacial till. They have a wide range of potential uses and are well
suited to arable and pastoral farming (ibid., 67). Land use along the route was almost en-
tirely grassland devoted to intensive dairying and cattle-rearing, with only an occasional
tillage field.

1


N

Derry
Donegal Antrim

Tyrone

Leitrim Fermanagh Armagh Down

Sligo

Cavan
Garryleagh 1 Carrigane 1
Louth
Mayo
Roscommon Longford E2433 E2434
Meath

Westmeath Dublin
Gal ay
w
Oﬀaly
Kildare

Clare
Laois Wicklow Kildrum 1
Carlow E3971
Tippeary
r
Kilkenny
Limerick Wexford
Kilshanny 3
Kerry N8 Waterford E2432
Cork

Kilshanny 2
E2431

Ballynamona 2 Kilshanny 1
E2429 E2430

Ballynamona 1
Glenatluckly 1 E2428
E2427

Gortnahown 2
E2426

Gortnahown 1 Gortnahown 3
E2423 E2477

Gortnahown 4
E3832

Caherdrinny 3
E2422

Caherdrinny 2
E2421

Caherdrinny 1
E2420
Ballinrush 1
E2419

E2418
E2417

E2416
E3972
E3972

E2415

E2414
Ballynacarriga 3
E2412
Ballynacarriga 2
E2413

Ballynacarriga 1
Key E2411
Post Medieval Gortore 1B
Early Medieval E2410
Gortore 2
Prehistoric Site
E3973
Prehistoric Settlement Site
Burnt Mound
Non-archaeological
0km 2km
Townland Boundaries

Figure 1: The route of the N8 Fermoy to Mitchelstown Bypass overlain on the Ordnance Survey Discovery Series map�

2


4 Archaeological and historical background
Archaeological sites of numerous periods were discovered along the route of the new
road (Figure 2). The periods are referred to as follows: Mesolithic (c. 8000 to 4000 BC),
Neolithic (c. 4000 to 2000 BC), Chalcolithic (Beaker) (c. 2500-2000 BC), Bronze Age
(c. 2000 to 500 BC), and Iron Age (c. 500 BC to AD 500), early medieval period (c. AD
500 to 1100), medieval period (c. AD 1100 to 1650), post-medieval period (c. AD 1650 to
the present).
A number of Giant Irish Deer (Megaloceros giganteus) skulls, large antlers, antler frag-
ments and various long-bones were retrieved from the clay sediments, c. 1.5 m below the
peat stratum at Ballyoran Bog (04E1014) on the route of the N8 Rathcormac Fermoy.
A radiocarbon date of cal BC 11201-10962 was returned for the Giant Irish Deer. Gi-
ant Irish Deer are extinct but are known to have inhabited Ireland during two separate
periods in the Pleistocene (from 37,000-32,000 BP and 11,750-10,950 BP), with examples
from lake deposits beneath peat bogs frequently dating to the period between 11,750 BP
and 10,950 BP (Woodman et al. 1997). The Ballyoran Bog examples were found in this
typical location of lacustrine (lake) sediments beneath peat and they therefore pre-date
the beginnings of bog formation and the first human settlement of the area.

Mesolithic (c. 8000 to 4000 BC)
The earliest known human settlement in Ireland dates from the Mesolithic period (c.
8000 BC - 4000 BC). In Munster, the majority of the evidence (flint scatters) for Meso-
lithic occupation has ‘come from the Blackwater valley in Co. Cork’ (Woodman 1989,
116). Flint scatters were recorded in the townlands of Kilcummer Lower (CO034-060)
on the northern bank of the Blackwater c. 13 km to the south-west of the route and in
Ballynamona (CO018-099) and Wallstown (CO018-100) on the northern and southern
sides of the Awbeg river respectively c. 20 km to the west of the route (Power et al. 2000,
2). Mesolithic sites and find spots were recorded on other road schemes in Co. Cork, these
included; Rath-healy 3 03E1678 and Curraghprevin 3 03E1138 (N8 Rathcormac Fermoy
Bypass), Ballynacarriaga 1 01E0567 (N25 Youghal Bypass), Ballinaspig More 5 01E0546
(N22 Ballincollig Bypass) and Carrigrohane 3 02E0431 (N22 BG).
Mesolithic activity was recorded on the route of the N8 Fermoy-Mitchelstown at
Gortore E2410 and at Caherdrinny 3 E2422 and Mesolithic stone tools were recovered
from Ballinglanna North 1 E2414, Ballinglanna North 3 E2416 and Ballinglanna North
6 E3972.

Neolithic (c. 4000 to 2000 BC)
The Neolithic Period is characterised by the introduction of agriculture and the begin-
nings of the clearance of the woodlands. The population increased and became more
sedentary in nature. A substantial Neolithic settlement site has been recorded at Lough
Gur, Co. Limerick. Previously the nearest known Neolithic house was located in Pepper-

3


hill (CO016-226/01) c. 30 km to the northwest of the route. It was recorded during the
construction of the Bruff-Mallow gas pipeline (Gowen 1988, 44-51).
The material culture includes the manufacture of pottery, flint and stone arrowheads,
scrapers, axes etc. The range of monuments types includes Megalithic tombs, single burial
graves and stone circles. Megalithic tombs can be sub-divided into court tombs, portal
tombs, passage tombs and wedge tombs. There are few wedge tombs or stone circles
known from north or east Cork. Two of the exceptions are wedge tombs located at Lab-
bacallee (CO027-086), which is one of the largest wedge tombs in the country, and at
Manning (CO027-091) both located c. 4 km west of the N8.
Recent infrastructural work on the N8 Rathcormac to Fermoy and the Ballincollig
Bypass have added significantly to the number of Neolithic sites in the county. A Neo-
lithic house was excavated at Gortore (E2119), on the N8 Rathcormac to Fermoy road
and another Neolithic house was excavated at Barnagore (02E0384), along the route of
the Ballincollig Bypass. Both of these Cork examples produced essentially the same ra-
diocarbon results (cal BC 3940-3620 at Barnagore and cal BC 3928-3655 from Gortore)
and they represent the oldest known houses in the county. A single pit at Fermoy town-
land (05E0078), located c. 3 km to the south of Gortore, produced 12 sherds of a Middle
Neolithic Globular bowl, and another site at Curraghprevin (c.12 km south of Gortore)
produced Western Neolithic (Early Neolithic) pottery and a radiocarbon date of 3090-
2580 BC (Late Neolithic).
Rectangular Neolithic houses were recorded on the route of the N8 FM at Gortore
1b (E2410), Ballinglanna North 3 (E2416) and Caherdrinny 3 (E2422). A large enclosure
containing several structures associated with Late Neolithic pottery was excavated at Bal-
lynacarriaga 3 (E2412). Activity dating to the Neolithic was also recorded at Ballynamona
1 (E2428), Ballynamona 2 (E2429), and Gortnahown 2 (E2426) and Gortore 2 (E3973).

Bronze Age (c. 2000 to 500 BC)
The Bronze Age is characterised by the introduction of metallurgy and an increase in
settlement and burial sites. Copper ores were mined and copper, bronze and gold items
manufactured. The range of burial site types includes cist graves, pit and urn burials,
cremation cemeteries, barrows, ring-ditches and wedge tombs. Stone circles and stand-
ing stones also date to the Bronze Age. Both enclosed and unenclosed settlement sites are
known. The most prolific Bronze Age site type is the fulacht fiadh; over 2,000 examples
have been recorded in County Cork alone. These monuments survive as low mounds of
charcoal rich black silt, packed with heat-shattered stones, and generally situated close to
a water source. Fulachta fiadh are generally classified as ‘cooking places’, whereby stones
were heated in a hearth and subsequently placed in a trough of water, the water continued
to boil with the addition of hot stones and wrapped food was cooked within the hot wa-
ter. The trough eventually filled with small stones, ash and charcoal that were removed,
forming the basis of the familiar mound.

4


N

Derry
Donegal Antrim

Tyrone


Sligo

Cavan
Louth
Mayo
Meath

Westmeath Dublin
Gal ay
w
Oﬀaly
Kildare

Clare
Carlow E3971
Tippeary
r
Kilkenny
Limerick Wexford
Kilshanny 3
Cork

Kilshanny 2
E2431

E2429 E2430

Ballynamona 1
E2427

Gortnahown 2
E2426

E2423 E2477

Gortnahown 4
E3832

Caherdrinny 3
E2422

Caherdrinny 2
E2421

Caherdrinny 1
E2420
Ballinrush 1
E2419

E2418
E2417

E2416
E3972
E3972

E2415

E2414
Ballynacarriga 3
E2412
Ballynacarriga 2
E2413

Ballynacarriga 1
Key E2411
Gortore 2
Prehistoric Site
E3973
Burnt Mound
Non-archaeological
0km 2km
Townland Boundaries

Figure 2: The route of the N8 Fermoy to Mitchelstown Bypass overlain on the first edition Ordnance Survey map
CO010, 011, 019, 020, 027 and 028�
5


The Bronze Age cemetery site at Mitchelstowndown West, c. 16 km to the north of
Mitchelstown, contains 53 small barrows. The Discovery Programme Report 1 (Daly and
Grogan 1992, 44) selected four of this group for excavation.
Until recently, Bronze Age settlement sites were a rarity in North Cork. A Bronze Age
occupation site was recorded underlying the medieval ringfort Lisleagh I (CO027-158)
c. 2.5 km to the west of the N8 (Power et al. 2000, 210). A house site was excavated at
Killydonoghoe on the route of the N8 Glanmire-Watergrasshill Bypass (Sherlock 2003).
Three circular houses dating to the Middle Bronze Age were excavated at Mitchelstown
(04E1072) on the N8 Mitchelstown Relief Road. A large Bronze Age settlement site con-
sisting of three circular enclosures and three circular houses was excavated in 2003 at
Ballybrowney (03E1058), on the route of the N8 Rathcormac-Fermoy (Cotter 2005, 40).
Bronze Age round houses were recorded on the route of the N8 Fermoy – Mitchel-
stown at Kilshanny 1 (E2432) and Ballynamona 2 (E2429). Burnt mounds/fulachta fiadh
sites were recorded at Ballinglanna North 1 (E2414), Ballinglanna North 3 (E2416), Ball-
inglanna North 6 (E3972), Ballynamona 2 (E2429), Caherdrinny 1 (E2420), Kilshanny
3 (E2432) and Kildrum 1 (E3971). Two ring ditches and associated cists and pits burials
were recorded at Ballynacarriga 3 (E2412). Portions of several encrusted urns and food
vessels dating to the Early Bronze Age were recorded in association with the burials. A
cremation burial and associated Early Bronze Age urn were also recorded at Glenatlucky
(E2427).

Iron Age (c. 500 BC to AD 500)
Until the last decade there was little evidence of a significant Iron Age presence in the
Cork region. Settlement sites are few and far between as well as being difficult to identify
(Woodman, 2000) while the material culture of this period is limited. Linear earthworks,
believed to have marked tribal boundaries, and hillforts are two of the most visible monu-
ments of the period. Recent infrastructural work on the N22 Ballincollig Bypass, the N8
Glanmire Watergrasshill Bypass and the M8 Rathcormac Fermoy has altered the picture
considerably.
Three separate stretches of a linear boundary, the Claidh Dubh, have been recorded in
County Cork. The longest stretch, c. 24 km in length extends from the Nagle Mountains,
across the Blackwater valley and into the Ballyhoura Hills. Radiocarbon dating following
excavation of a section of it revealed it dated to some time before AD100 (Doody 1995,
23).
Two of the four hillfort sites in Cork are located in North Cork (Power et al. 2000,
205). Caherdrinny (CO019:97/0103) is located at the western end of the Kilworth
Mountains, c. 700 m to the west of the N8, Corrin (CO035:49/01) is lo cated at the
eastern end of the Nagle Mountains, overlooking a pass between the Blackwater and
Bride river valleys just south of Fermoy.
Iron Age dates were returned from a roundhouse at Ballinaspig More 5 01E0546,
a possible bowl furnace at Curraheen 1 01E1209 and the fulacht fiadh at Curraheen 4

6


02E1297 on the N22 Ballincollig Bypass; the Iron Age structure at Muckridge 1 01E0429
on the N25 Youghal Bypass; iron working sites at Kilrussane 01E0701 and Trabstown
01E0501 on the N8 Glanmire Watergrasshill Bypass; the iron working site at Lisnagar De-
mesne 1 03E1510, the pit at Maulane East 1 03E1286, the pit at Scartbarry 3 03E1800, the
corn-drying kiln at Rath-healy 1 03E1139, the burnt mound at Fermoy Wood 04E1014
and the ring ditch at Ballybrowney Lower 3 05E0233 all on the M8 Rathcormac Fermoy.
Activity dating to the Iron Age was recorded on the route of the N8 Fermoy – Mitch-
elstown at Ballinglanna North 3 E2416, Ballinglanna North 4 E2417, Ballynacarriaga
3 E2412, Gortnahown 1 E2423, Gortnahown 3 E2477 and Caherdrinny 3 E2422. The
sites, with the exception of a single fire pit at Ballinglanna North 4 E2417, did not date
exclusively to the Iron Age.

Early medieval period (c. AD 500 to 1100)
The early medieval period is characterised by the arrival of Christianity to Ireland. The
characteristic monument type of the period is the ringfort. Ringforts are the most nu-
merous archaeological monument found in Ireland, with estimates of between 30,000
and 50,000 illustrated on the first edition of the Ordnance Survey 6” maps of the 1840’s
(Barry 1987). As a result of continued research, the construction of these monuments has
a narrow date range during the early medieval period between the 7th and 9th centuries
AD. Although there are some very elaborate examples of ringforts, they often take the
form of a simple earth or stone enclosure functioning as settlements for all classes of secu-
lar society (Stout 1997).
A major research excavation of two ringforts was undertaken at Lisleagh, c. 2.5 km to
the west of the N8 route, in the late 1980s/early1990s. Structural, domestic and industrial
evidence was recorded at both sites. A number of stake and wattle round houses, and
ironworking were recorded in Lisleagh I, which had two phases of occupation, ranging
from the early 7th century to the 9th century AD (Monk 1995, 105-116).
Souterrains, frequently associated with ringforts and enclosures, are man made un-
derground chambers linked by narrow passageways. The concealed entrance is located
at ground level. It is thought souterrains were used for storage or places of refuge during
times of trouble (Clinton 2001). It has also been hypothesised that some may have been
used for housing slaves.
The monastery of Brigown (which gave the name to the modern parish in Mitchel-
stown) was founded in the 7th century by Fanahan. Fanahan is reputed to have com-
missioned seven smiths to make seven sickles which were used by him for self-mortifica-
tion. The new monastery was named, Brí Gabhann, for the smiths (Power 1996, 3). The
ecclesiastical remains comprise a church, graveyard, holy well and site of round tower
(CO019:30/01-05). A possible enclosure site with evidence of metalworking was excavated
by John Purcell in Brigown. This was possibly the enclosure of Brigown. No dates were
obtained from the site (John Purcell personal communication).

7


A horizontal-wheeled mill (CO027-108) was located on the northern side of the Glen-
corra Stream c. 120 m north of the confluence with the River Funshion.
A ringfort and associated souterrain (CO027-109) were excavated on the route of the
N8 Fermoy – Mitchelstown at Ballynacarriga 2 (E2413). Two circular houses and a com-
prehensive range of metalworking activities were excavated at Gortnahown 2 (E2426).
Sites with evidence of metalworking activities were also excavated at Ballynamona 2
(E2429) and Ballinglanna North 1 (E2412).

High and later medieval periods (c. AD 1100 to 1650)
This period is characterized by the arrival of the Anglo-Normans and the building of
tower houses. Mitchelstown was formerly known as Brigown / Mitchelstown (CO019-
149). It was listed as a market town in 1299 and was located on the southern bank of the
Gradoge River, to the east of Mitchelstown Castle (Power et al. 2000, 595). The town
developed under the patronage of the House of Desmond. It passed into the hands of the
Earls of Kingston in the 17th century (Power 1996, 23).
The Condon family controlled the barony of Condons and Clongibbon. Two of
their castles are located in close vicinity to the route of the N8 FM. Cloghleagh Castle
(CO027:113) is located on the northern bank of the Funshion River to the east of the
new route. It was built on an outcrop of limestone bedrock. It is a 5-storey tower with
associated bawn wall (Power et al. 2000, 537). Caherdrinny Castle (CO019:97/02) is lo-
cated to the west of the route. It was a 5-storey tower built within the hillfort enclosure
(CO019:97/0103). Glanworth Castle (Boherash CO027-42) is located on a sheer lime-
stone cliff overlooking the River Funshion 5 km to the west of the route. The 13th-century
hall house is associated with a four-sided walled enclosure (ibid. 516).

Post-medieval period (c. 1650 to the present).
The post-medieval period is characterised by mills, limekilns, workhouses, country hous-
es and associated demesnes, vernacular buildings and field systems (Figure 3). Three de-
mesnes associated with country houses are within the route of the N8 at Moorepark,
Ballynacarriga and Glenwood. The estate system was dismantled in Ireland in the early
20th century. Demesnes usually comprise of a large country house with associated stables,
farm buildings and gate lodges, areas of woodland and ornamental gardens etc. The de-
mesne was usually enclosed by a high stone wall such as that associated with Moorepark.
Moorepark house and demesne was the seat of the Earls Mountcashell (Lewis 1988, 312).
The Moorepark Estate covered an area around 800 acres and extended both north and
south of the river Funshion. The house was sold to the British War Office c. 1903 by
the 5th Earl’s daughter (Bence-Jones 1996, 211). It burned down in 1908 and was never
rebuilt. No trace of it now survives The demesne is clearly defined by woodland on the
1841-2 and 1906 edition Ordnance Survey maps, which was most likely enclosed by a
wall. It is likely that the demesne walls are contemporary with the mansion house and

8


therefore date to the 18th century. The Cork to Dublin mail coach road originally ran to
west of the demesne walls as it appears on the 1841-2 and 1906 Ordnance Survey maps.
The site of a workhouse (C0019-11301-) built in 1852 is located in Kilshanny townland
to the east of Mitchelstown. The complex of buildings, including a hospital chapel and
mortuary, was enclosed within a three-metre high limestone wall and could accommo-
date up to 600 people. Closed in 1916 and burned by the IRA in 1922, only the boundary
wall and main entrance way survive today (Power 2002, 48).
A late 19th century bridge of rubble limestone, approached by a causeway at either
end, carries a tertiary road from Kilworth-Glanworth over the Glencorra Stream. A road
crosses the stream at the same location on the 1841-2 Ordnance survey map, but the
bridging structure is not named. The site is named Glencorra Bridge on the 1906 edition
of the Ordnance Survey map and is of local architectural significance.

5 Site Location and Topography
The site at Ballinglanna North 6 was located west of the existing N8, and 200 m west
of the Glencorra Stream at 90 m OD. It was split into two areas. Area 1 was situated on
low-lying undulating ground and Area 2 was located on a plateau 55 m to the north-east.
Area 2 was well drained and remained dry even in heavy rain. Several pit clusters dating
to the early medieval period were excavated at Ballinglanna North 2 E2415, located 200
m to the south and Neolithic structures and burnt mounds dating to the Early Bronze
Age were excavated at Ballinglanna North 3 E2416, 350 m to the north.

6 Excavation methodology
The excavation was carried out under E-Number E3972 and complied with the meth-
od statement approved by the Department of Environment, Heritage, and Local Gov-
ernement, in consultation with the National Museum of Ireland. The site was mechani-
cally stripped of topsoil under strict archaeological supervision. Stripping was done with a
tracked machine with a flat toothless bucket. Where appropriate mini-diggers were used,
and in the larger areas to be stripped multiple large tracked machines were used; all strip-
ping operations involved the use of multiple dumpers for topsoil mounding. Topsoil strip-
ping commenced in the areas of identified archaeology and continued radially outward
until the limit of the road take was reached or until the limit of the archaeological re-
mains was fully defined. A grid was set up in the excavation area(s) and all archaeological
features were sufficiently cleaned, recorded and excavated so as to enable an accurate and
meaningful record of the site to be preserved. The excavation, environmental sampling,
site photographs, site drawings, find care and retrieval, on-site recording and site archive
was as per the Procedures for Archaeological works as attached to the licence method
statements for excavation licences.

9


N

Derry
Donegal Antrim

Tyrone


Sligo

Cavan
Louth
Mayo
Meath

Westmeath Dublin
Gal ay
w
Oﬀaly
Kildare

Clare
Carlow E3971
Tippeary
r
Kilkenny
Limerick Wexford
Kilshanny 3
Cork

Kilshanny 2
E2431

E2429 E2430

Ballynamona 1
E2427

Gortnahown 2
E2426

E2423 E2477

Gortnahown 4
E3832

Caherdrinny 3
E2422

Caherdrinny 2
E2421

Caherdrinny 1
E2420
Ballinrush 1
E2419

E2418
E2417

E2416
E3972
E3972

E2415

E2414
Ballynacarriga 3
E2412
Ballynacarriga 2
E2413

Ballynacarriga 1
Key E2411
Gortore 2
Prehistoric Site
E3973
Burnt Mound
Non-archaeological
0km 2km
Townland Boundaries

Figure 3: The route of the N8 Fermoy to Mitchelstown Bypass overlain on the RMP map CO010, 011, 019, 020, 027 and
028� The map is based on the second edition Ordnance Survey maps�
10


The site at Ballinglanna North 6 was discovered during Phase 2 archaeological test-
ing of a severance area along the new route of the N8 Fermoy to Mitchelstown. The site
was not available for testing during Phase 1 archaeological testing. The site was excavated
from 5 June 2007 to 26 June 2007. Only areas within the CPO were resolved. The full
extent of the area of excavation measured 3052 m2.

7 Excavation results
The full record of excavated contexts is recorded in the context register (Appendix 1) and
the stratigraphic matrix (Appendix 2). Detailed stratigraphic descriptions are found in
the groups and sub-groups text (Appendix 3). Two areas of archaeological interest were
recorded Areas 1 and 2 (Figure 4). Area 2 was located 65 m north of Area 1.

Area 1
Area 1 comprised a burnt mound/fulacht fiadh that extended beyond the limit of the
excavation to the west (Figure 5). The burnt mound layer C.2 measured 11.2 m by 4.3 m
by 0.27 m in depth within the area of excavation. It was a stony dark black soft silt with
frequent charcoal (Plate 1). Some of the charcoal from this deposit was identified as hazel/
alder and it returned an Early Bronze Age date of 1902-1737 1710-1696 (UB 12973). The
deposit overlay a trough (C.77) and a linear feature (C.58).
The trough (C.77) was found at the eastern edge of the mound, partly overlain by
some of the mound deposits. The trough was re-cut to the east and the re-cut (C.79) was
not overlain by any of the burnt mound material. The troughs were rectangular, though
irregular and shallow, in plan (Plate 2). The fills of the trough were derived from the burnt
mound (Figure 7). A circular pit (C.80) and a drainage ditch (C.55) truncated the later
trough (C.79).

Context Length (m) Width (m) Depth (m) Volume (m3)
77 2 1.1 0.2 0.44
79 3 1.3 0.24 0.93
80 1.6 1.4 0.22 0.49
Table 1 Dimensions of troughs and pit

The troughs were located in the area of a rising spring. There was anecdotal evidence
from the landowner for a ground water ‘river’ flowing through this part of the site during
times of heavy rainfall.
A shallow linear feature (C.58), aligned north-south, was located 1 m north of the
trough. It measured 2.3 m in length by 0.97 m in width and 0.32 m in depth. The mound
of burnt material had overlain the southern portion of the linear but it is possible that it
was associated with land drainage rather than the burnt mound.
The area was disturbed in the modern period by a series of land drains. Several drains
(C.18, C.19, C.55 and C.76) criss-crossed this area of the site, as it was low-lying and

11


prone to water-logging. The drain C.55 was a re-cut of drain C.76. It was U-shaped in
plan and was earlier in date. The drain C.18 was part of a comprehensive series of modern
stone filled V-shaped drains.

Area 2
The archaeological features in Area 2 comprised a hearth (C.24) and associated wind
break (C.34, C.69, C.70, C.71 and C.72), three pits (C.22, C.32 and C.74) and associated
stake-holes (C.26, C.37, C.47, C.50, C.52 and C.53) and three linear features (C.42, C.61
and C.68) (Figure 6).
The hearth C.24 was located in a shallow hollow. It measured 1.1 m by 0.56 m by
0.15m (Figure 8 and plate 3). The fill C.9 was charcoal enriched and was confined to the
deeper south-eastern part of the hearth. The subsoil in vicinity, particularly to the north-
west was scorched (C.10), suggesting that the fills of the hearth were originally more
extensive. A metalled surface (C.40) overlaid the hearth (C.24) at the south-west and
extended beyond the area of the hearth to the west. There were also some possible areas of
metalling to the south of the hearth near the screen/windbreak. This metalled surface was
made up of small sub-rounded and sub-angular stones pressed into the sub-soil. Some of
the stones were heat affected and had been exposed to high temperatures.

Plate 1: Pre-excavation view of
burnt mound deposit
C�2 facing south�

12


181376 181402

24
Hearth
69
±
72
70 71
34 22
Pit 37 53
32 68
32 50
26
61 88
47
52 39
74
42 Ditches
Area 2
104477

104477
75

O
)
101 m O.D.
104431

104431

18

58
19 Area 1
77
79 76
80
55
Burnt
mound
Drainage ditch

0 20 m
181376 181402
Figure 4: Post-excavation plan of Ballinglanna North 6�

13

181384 181400

14
±
58

104423
104423
iSSUE 10: Eachtra JoUrnal - iSSn 2009-2237

19 Trough

77
76
79
80
55

104416
104416

Drainage ditch
Burnt mound

0 10 m
181384 181400

Figure 5: Post-excavation plan of Area 1 Ballinglanna North 6�
archaEological Excavation rEport


Plate 2: Post-excavation of
re-cut trough C�79 and pit C�80
from south�

Plate 3: Post-excavation of hearth C�24 and stake-holes C�34, C�69-C�72 from south�

15


The charcoal-rich fill (C.9) contained small quantities of plant remains, including oat
and barley grains and chaff; the presence of chaff suggests that these may have been used
as kindling. A modern radiocarbon date of cal AD 1666-1952 (UB13230) was returned
from the charred grain and seeds.
The windbreak or screen was located downslope and to the south of the hearth. It
comprised five stake-holes (C.34, C.69, C.70, C.71 and C.72). The largest stake-hole was
centrally located with two stake-holes to either side C.70 and C.71 to the west and C.72
and C.69 to the east.

Context Length (m) Width (m) Depth (m)
34 0.2 0.18 0.2
69 0.08 0.07 0.07
70 0.1 0.08 0.1
71 0.06 0.06 0.12
72 0.06 0.06 0.12
Table 2 Dimensions of stake-holes

Three pits (C.22, C.32 and C.74) were located in the vicinity of the hearth, one to the
north and two to the south. Pit C.22 was located at the edge of the area of excavation and
extended beyond the baulk (Plate 4). A flint flake (E3972:21:2) and a roughed-out frag-
ment of a quern stone (E3972:21:1) were recovered from the fill. The quern stone appears
to have broken before it was ever used and as a result it was not completed. The pit cut
a layer (C.20/23) which comprised a thin lens of charcoal overlying heat-altered subsoil.
The soil from this layer was sampled but the charcoal did not survive the flotation process
which suggests that it was totally degraded. Two stake-holes (C.37 and C.53) were located
to the south of the pit. Fragments of iron nails were included in the fill of stake-hole C.37.
A large pit (C.32) was located 0.8 m south of the hearth (Figure 8 and plate 5). The fills
were a mix of sandy silts. The pit cut the two linear features (C.61 and C.68).
The third pit (C.74) was located 3 m to the south (Plate 6). It underlay a possible
hearth and associated heat altered subsoil (C.6 and C.86). The hearth C.6 measured 3.7
m by 1.55 by 0.04 m in depth. Three small stake-holes (C.47, C.50 and C.52) were located
on the northern edge of the hearth C.6. They measured 0.04 m in diameter.

Context Length (m) Width (m) Depth (m)
22 0.5 0.3 0.29
32 2.7 1.9 0.2
74 1.54 1.15 0.26
Table 3 Dimensions of pits

An isolated post-hole (C.26) was located 6 m to the east in the eastern part of Area 2.
It was the only feature recorded on the eastern side of the ditch.
Two ditches (C.39 and C.75) and three linear features (C.42, C.61 and C.68) were
located in the area of excavation. The ditch C.75 was orientated east-west and it cut C.39,
which was perpendicular to it. The fills included clay pipe fragments. The linear features
may be associated with the hearths and pits or maybe agricultural in origin.

16

181384 181398

22 ±
53
37

Hearth
24 69
Ballinglanna north 6-E3972

68 70 72
71

104488
104488

34

32
Pit
88
47 50
61 26
52

Pit

74
42

39

104480
104480

75
Ditches

0 10 m

181384 181398

Figure 6: Post-excavation plan of Area 2 Ballinglanna North 6�
http://eachtra.ie/index.php/journal/e3972-ballinglanna-north6-co-cork/

17


Plant remains
The charred remains from this site were examined by Penny Johnston (Appendix 5). A
total of 7 samples were scanned. Charred seeds were found in two samples, both from the
deposit C.9 in the hearth C.24. The identified material included hazelnut shell fragments,
barley grains and a small amount of weed seeds.

Lithics
The lithics from Ballinglanna North 6 were examined by Farina Sternke (Appendix 6).
A flint blade (E3972:1:1) was recovered from the topsoil (Plate 7). This was typologically
dated to the Early Mesolithic and could indicate that the spread of Mesolithic activity in
this area of north Cork was even more extensive than the evidence already accumulated
from sites such as Gortore 1 E2410 and Caherdrinny 3 E2422. Two objects were found
within a pit (C.22). One of these was identified as a quartzite quern stone (E3972:21:1)
that was broken and possibly stained with ochre (Plate 8). The second lithic was a flint
flake (E3972:21:2) that was burnt and was possibly Neolithic in date.

Charcoal
The charcoal from the area of burnt mound and the charcoal for radiocarbon dates was
examined by Mary Dillon (Appendix 7). The charcoal analysis suggests that hazel, alder
and oak, 47%, 33% and 20% respectively, charcoal were used in the fires at the burnt
mound. Ash, which is often quite common at burnt mound sites, was not represented in
the assemblage. It was probably not growing in the local environment at the time.

Plate 4: Post-excavation of pit C�22 from south�

18

Ballinglanna north 6-E3972

E3972
North west facing section of C.79

C.62

C.64
C.76

C.66
C.63

C.65

C.79 C.79

C.80

0 500 mm

Figure 7: Section of trough C�79 and pit C�80�
http://eachtra.ie/index.php/journal/e3972-ballinglanna-north6-co-cork/

19

Archaeological Report - Ballinglanna North 6, Co. Cork (Ireland)

Archaeological Report - Ballinglanna North 6, Co. Cork (Ireland)

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