The peak of Derrylahard East is perplexing. It’s on a continuation of the Eastern Mizen Ridge that runs from just west of Mount Corrin (which we visited exactly a year ago), takes in Letterlickey Cairn (ditto) and peters out close to the wind farm at Ballybane West (which we explored last October). At its highest point it overlooks Glanlough (from the Irish Gleann Locha – ‘Glen’ or ‘Meadow’ of the lake). We must not be confused or misled by another Glanlough nearby – on the Sheep’s Head peninsula, nor yet another in Co Kerry.
On the map above I have indicated Glanlough, which is central to our most recent peregrination. It is a mountain lake which has been virtually hidden over the last decades by thick commercial pine forests. Very recently, much of the forest has been felled, and views from the top of the ridge are now revealed: they are magnificent and far-reaching. In fact, from the high point we found we could see the 12 arched bridge at Ballydehob – which means. of course, that we can also see Derrylahard East from our own village.
The upper picture was taken from the Derrylahard East Peak with a lens stretched well beyond its limit, but you can see the 12 arched bridge and the sandboat quay house just below the centre of the view: Cape Clear is on the horizon. The lower picture was taken a while ago from the 12 arched bridge in Ballydehob, looking north towards the Derrylahard East Peak, which is swathed in cloud to the left of the rainbow.
We started the walk at the western end of the loop: we accessed it from a road that runs through the forestry from Barnageehy down to Durrus. As we gained the higher ground we could see the ridge path that would lead west through to Mount Corrin – currently closed due to storm damage. We turned uphill and kept close to the townland boundary. Below – Finola is correctly negotiating the stile by going backwards down the steps!
We followed the Sheep’s Head Barnageehy Loop Walk in an anti clockwise direction, circling the lake of Glanlough and looking out for the summit, which is known as Derrylahard East Peak, even though it appears to be within the townland of Glanlough. According to the 6″ OS map, which dates from the 1840s, there was once a trig point at this summit: a height of 990ft – 302 metres.
At the peak: Finola looking back towards Gabriel – always dominating the landscapes in West Cork – with the islands and ocean in the distance; Dunmanus Bay and the Sheep’s Head to the west, with the Beara Peninsula visible beyond; the view east encompassing the Ballybane West turbines and Mount Kidd.
Upper map: the 1904 OS showing Glanlough lake in context with the wider topography of West Cork. Above – the Down Survey, made between 1656 and 1658: this section covers the area shown in the OS above it, and is at a comparable scale. The red asterisk shows the position of the lake at Glanlough: I had hoped there might be some notation on the Down Survey that would give some insight into the name of Glanlough, but the old map is fascinating for the fact that very few of the names are familiar to us and barely a scattering of them can be easily equated with place names today.
I said at the outset that the peak of Derrylahard East is perplexing. For one thing, it is clearly in the townland of Glanlough, yet bears the name of the neighbouring townland. Then there is the altitude of the summit: mountainviews.ie shows two figures for the height above sea level: 301m (which I would – almost – agree with), but also the figure of 353.9m, which must be a mistake. Unless, of course, there is something preternatural in this small patch of West Cork territory: I’m thinking of the legend of the ‘floating’ islands in the lake on Mount Gabriel. According to John Abraham Jagoe, Vicar of Cape Clear – from the Church of Ireland Magazine 1826 – they ‘…float about up and down, east and north and south; but every Lady-day they come floating to the western point, and there they lie fixed under the crag that holds the track of the Angel’s foot…’ Perhaps our peak fluctuates at will to confuse us? The shape of the summit is also intriguing: we sensed there are traces of a circular platform and a number of loosely scattered stones – could there have been a megalithic structure here?
The views from this peak would justify it being marked out as a special site, and we could expect to find some stories recorded in the folklore archives, but no: the Duchas Schools Collections reveals nothing of the peak, the lake, nor the townland.
As we descended the track we were grateful that the recent forestry removal has opened up the extensive views to the south, over Roaringwater Bay, but we are also reminded of the devastation that this type of monoculture creates. The scarring of the landscape will last for years, until eventually covered by further spruce planting: then the views will vanish again.
As we left behind the havoc of the ravaged hillsides it was good to find some pastoral prospects, reminding us that West Cork always has unfolding delights and juxtapositions, wherever we wander.
It rises on a remote mountain-top in the wilds of Mullaghmesha townland and falls 500 metres from there to the Atlantic, over a length of 34 kilometres. I think it’s time to establish exactly where the river ends, and the ocean begins. As you can see from the photo above, the lower reaches are wide and shallow, and the estuarial waters are dotted with islands and islets, some of which are only revealed at the ebb of the tide.
Below Skibbereen, the river is fully tidal – and its character is constantly changing. The history of the waterway has also seen an evolution, from a busy highway carrying lighters filled with cargoes to the wharves in the town (in the 19th century there were five of them – and a Customs House), to the present day where it is a tranquil scene, only busy – in normal times – with the skiffs and light craft based at the Rowing Club (above): that establishment has produced some celebrated champions!
Oldcourt (above) was the transhipment point where laden ships from distant shores would leave their loads into the shallow draft barges that would take them upstream into the town. Today it is still a busy hub where vessels are stored, built and repaired – and also left to decay. The disorder of the place has a picturesque informality, and there is medieval history also: a rickety tower house stump stands guard over the apparent chaos. We have written about the boatyard (and the castle – and a ketch named Ilen) in a previous post.
You can cross a bywater of the Ilen by bridges at Inishbeg (above) and Ringarogy. Exploration of those two islands will reveal a number of view points over the main channel of the river to the north. The marked aerial map below shows the lie of the land, while the photos following show the wide views of the river in both directions from Inishbeg.
(Upper) looking upstream from Inishbeg, and (lower) a close view of The Glebe Burial Ground, also seen from across the main river at Inishbeg.
Downstream from Inishbeg: at the east end of the island we found an unusual large rock which appears to have a worked surface and a possible cup-mark. Below that rock is the lonely ruin of a structure which must have had a remarkable aspect over the whole width of the river. It would be easy to suppose that this ruin could have been part of a defence system, but there is no mention in the archaeological records of this, or of the rock. For now, they remain enigmas – but perhaps there is an alert reader out there who can shed some light?
Ringarogy has fewer accessible viewpoints than Inishbeg, but the long causeway and some prospects from high land indicate how the lower course of the river is punctuated with small, barren landfalls (above).
I have made up my mind that the Ilen proper must ‘end’ at Turk Head – the pier, above, is looking towards the main channel of the river. It is also a small but substantially built harbour – partly hewn out of the low cliffs – which can shelter a few light fishing craft.
But the reality of the downstream ‘end’ of the river seems to be defined on the 6″ OS map above, which dates from the early 19th century and shows the townland names and boundaries as they were recognised at that time. There, a clear line is drawn between the island of Inishleigh to the north, and Spanish Island to the south. To the east of that line, apparently, is the Ilen, while to the west is the edge of Roaringwater bay, which leads into the ocean, but first skirting a myriad of rocks and small islands, only some of which have names.
There may be traditions – unknown to me – that define where the river mouth lies. Perhaps it doesn’t really matter. If you are a seafarer carrying goods bound for Skibbereen you will have to negotiate your way safely through a fairly convoluted channel before entering a contrasting world of wide, calm water and rich, smooth meadowlands: Sweet Ilen.
I’m remembering back to a warm summer evening spent on the Barley Cove dunes with the bunnies.
How many can you see?
We wanted to just sit and observe, so we found a comfortable spot where we had a view over the warren. They were everywhere! They weren’t unduly perturbed by humans, although they disappeared quickly when dogs came sniffing around. In the face of all the challenges rabbits face in Ireland, it felt good to be in a place where they seemed to be in a long-term relationship with their habitat.
European rabbits (Oryctolagus cuniculus to the biologists, coinín, pronounced cunneen, in Irish) were introduced to Britain by the Normans in the 11th century. They called them coneys and kept them in coney garths as a food source. Niall Mac Coitir, in his marvellous Ireland’s Animals: Myths, Legends and Folklore, tells us
The ‘coney garth’ consisted of a small enclosed field surrounded by a deep ditch, and a huge turf mound planted with gorse and blackberry to keep the rabbits in. Escape was easy, however, and the rabbit soon became free game for yeoman and serfs, even though it was illegal. . .
The Barley Cove dunes – rabbit country
A hundred years later, they brought their rabbits to Ireland, with the same predictable results. When you think that an adult female (a doe) can have up to seven litters a year, each one yielding up to ten kittens, the proliferation rate is explosive. They are kept somewhat in check in the wild by natural predators and a high mortality rate. Left totally undisturbed, rabbit populations probably undergo the same cyclical variations that other mammals do, with numbers increasing for about ten years and then declining due to over-population, before building up again.
Ears back – what’s he listening for?
But rabbits have never been left undisturbed for two main reasons – first they are a natural source of food and fur and second they can be a significant agricultural and horticultural pest. Exporting rabbit skins was big business in medieval Ireland and as late as the 1940s rabbit meat was still being processed and eaten at a great rate. But pity the organic gardener who comes out in the morning to find his patch stripped and desolate, or the farmer who loses a portion of her hard-won crop. The solution for the agricultural sector was disastrous – in the 1950s farmers introduced the disease myxomatosis into the rabbit population with devastating results. As I was growing up in 1950s Ireland I never saw a rabbit – the population had been virtually wiped out.
Since then, they have recovered somewhat (although now threatened with a new disease in the wild) but in this part of the world it’s still not commonplace to see a rabbit. That’s why it’s such a treat to be able to sit and watch them at Barley Cove. The best time to do this is in the evening, since they are naturally nocturnal creatures.
The warrens are obvious and sizeable – those big hind legs are effective digging machines! The tunnels have several entrances and contain passages and chambers where kittens can spend their first few days. Chris Packham, the British naturalist, has an amazing clip from his BBC program “The Burrowers” where a rabbit warren is filled with concrete, creating a model of its extent and complexity. Just click on the photo below and then on the picture again when you get to the site.
To get closer to the Barley Cove rabbits in order to photograph them I had to crawl through long grass and try not to spook them. Once they and I were at eye level, it felt like a real communication – being regarded by those deep pools of age-old knowledge, gentle and wise, was lovely. At the same time, the ears were on high alert, and I knew that one false move and he was gone.
It certainly does! But this post is – literally – about rock: the hard, knobbly kind that is underneath us, surrounds us, and which has historically built our environment. In the picture above, taken on a clear February day during the most severe Covid lockdown, Finola is walking through beautiful West Cork. Beyond her is the great, gaunt outcrop of Mount Gabriel. Beside her is a traditional stone wall: its design unchanged over centuries. In the landscape all around her are rocks – large and small – scattered in the rough pasture.
In the distance, of course, is the coast: there are very few places in West Cork where you cannot, at least, catch a glimpse of the sea – and so many where you can immerse yourself in it, or stand on its shore and admire the infinite textures which those same rocks display. It’s mostly Old Red Sandstone: that’s the correct geological term. It was laid down in the Devonian period – a while ago now: between 400 and 300 million years, in fact. This followed an era during which our mountains were built, known as the Silurian times. Continents were shifting and separating, and what was to become Ireland was a great arid desert – deserted: there was no-one around to see it!
Old Red Sandstone: in fact it varies in colour depending on its local history. Broadly, some of the mountain rocks are purple-grey, while those closer to the sea could be greeny-red, but that is probably far too wide a generalisation. The sheer beauty is in the infinite shapes and colours. What artist needs any finer palette?
In those deserted times, an ‘Old Red Sandstone Continent’ extended over what is now northwest Europe, but it is worth noting that in ‘our’ part of it – the Munster Basin, covering today’s Kerry and Cork – we have one of the densest masses of this rock in the world: at least 6 kilometres thick. And we have to appreciate what it has given to us – high mountain spines sweeping steeply down to an indented shoreline of coves, creeks and inlets, with the myriad mottled islands that we oversee. An unparalleled, unfolded world.
After the ‘desert’ period, but much later – only about a million and a half years ago – came the Pleistocene Epoch. the word is from the Greek polys and cene – meaning ‘most recent’ – and that brings us almost up to date. That was a time of great climate events: deserts were inundated and then covered in ice sheets 3 kilometres thick, while moving glaciers tore up the rock surfaces, advancing and retreating several times. Eventually, what had been desert became arctic tundra. It is supposed that the ancestors of our present day life forms happened along during this epoch, and managed to survive. But we don’t find any traces of them until after the last ice sheet retreated in our part of the world – only about 12,000 years ago. The landscape that was left behind was inundated by rising sea levels, and the very last land bridge (between Cornwall and the eastern tip of Wexford) was washed away after that, but not before the Giant Elk and its mammal relations had got a foothold on the western side. The snakes, however, didn’t make it. And what of the humans?
Well, the humans embraced the rocky landscape. They made their marks on the outcrops; then they moved the rocks about, and made architecture from them. We can still see their efforts, some 5,000 years later.
These Neolithic carved motifs could be the earliest human interventions on the natural Irish landscape: they might date from 3,000 BC. These examples are from West Cork, and were only discovered a few years ago. Finola wrote the definitive thesis on Rock Art when she studied at UCC in the 1970s, and we have staged exhibitions and given talks on the topic.
A couple of thousand years later, Irish people started to build things with the stones they found around them. This wedge tomb under the backdrop textures of Mount Gabriel at Ratooragh has rested here since the Bronze Age. Finola’s post today uncovers the fascinating folklore stories that generations have told about such artefacts. But restlessly working the fabric of the landscape – Old Red Sandstone – into walls, shelters, tower houses, temples and towns has never ceased.
In honour of World Wetlands Day, which we celebrate on Feb 2 every year, here is a selection of beautiful, weird and wonderful native plants from one small bog soak in West Cork.
Bogs are unique environments, highly acidic and with low nutrients. Nevertheless, some plants have adapted to thrive in them. It’s important we safeguard these diminishing natural habitats.
That’s Castle Island, above, beyond Gaelic Lord Finnin O’Mahony’s dilapidated realm at the entrance to Rossbrin Cove, in Roaringwater Bay. In the fifteenth century there would have been a hive of activity at Rossbrin: quays alive with fishing activity, boats being repaired and prepared, houses, stores and cellars – all full. Castle Island itself would also have been inhabited in those days, as were many of Carbery’s Hundred Isles. Skeam West – to the east of Castle, and roughly in the centre of all the islands of Roaringwater Bay, has the remnants of a church said to date from the ninth century (Fahy – Journal of the Cork Historical and Archaeological Society, Volume 67, 1962).
Upper – Castle island with its close neighbours in Roaringwater Bay; lower – the ancient church on nearby Skeam West, drawn by Fahy in 1962 (courtesy Cork Historical and Archaeological Society). Fahy suggested a ninth century date for this structure, although other commentators have suggested an earlier origin, possibly even before St Patrick’s time
We set foot on Castle Island for the first time in August of last year – during a reprieve in the Covid lockdown measures. Those days seem halcyon now, compared to our current scourge and severe restrictions. We have not been able to return, but I am setting out to bring my reporting a bit more up to date, as I have been provided with further information from a range of sources.
Approaching Castle Island in 2020: upper – view of the island from the shore in Rossbrin townland; centre – proceeding to the island from Rossbrin Cove; lower – the quay on Castle Island, reportedly built in the early 20th century by the Congested Districts Board: “…the beach that it is laid upon was the best natural landing point on the island, well sheltered from the Atlantic swell …” (Mark Wycliff Samuel – The Tower House of West Cork, UCL 1998)
The history of the population of Castle Island is enigmatic and somewhat contradictory. Here is a quotation copied from the Ireland Bywayssite but uncredited and undated; I can find no other link containing the same information, but it must originally have been written when the island was still inhabited:
. . . Castle Island (Meadhon Inis – “middle island”) lies about 2km offshore, east of the mouth of Schull Harbour on the Mizen Peninsula. The island derives its English name from a ruined C14th Tower House, one of 12 built by the powerful O’Mahony clan in the area. The 1837 census recorded 89 people living on the island. At present there are fewer than 30 permanent residents, who make their living from farming . . .
quoted by ireland byways.co.uk
You will find some accounts which suggest that Castle Island was inhabited only up to the 1870s. These are incorrect: there is no doubt that the island was the home to a number of families in the 1890s as they suffered evictions then. It also seems questionable that the expense of constructing a substantial pier could have been justified only for the benefit of those who might run their cattle and sheep on a deserted island (as happens today). It is possible, therefore, that regular population of the island continued into the early years of the 20th century.
The remains of substantial houses exist on Castle island today: some do not seem to be as ruinous as would be expected if they had been unoccupied for well over 100 years
Recently, my attention was drawn to a Land Register folio recording the title for one of the parcels of land comprising Castle Island: ” . . . a burden, dated April 14, 1904, indicates that the property was transferred at that time subject to the right of . . . Jeremiah Regan to be supported clothed and maintained in the dwellinghouse on the said lands . . . ” That would imply, for sure, that there was at least one person who had the right to live on the island in the twentieth century.
Details from the ruined houses at the settlement of Wester, Castle Island: upper – brick and render chimney stack in reasonable condition; centre – elements from timber window frames still in existence; lower – traces of paint on an internal rendered wall
Accounts of the evictions which occurred on Castle Island have been well summarised in a Mizen Journal article by Liam O’Regan in Volume 6, 1998. The article is much too long to be included here, but it’s worth anyone’s while ferreting it out to get a vividly descriptive picture of the island in the 1890s.
Here’s a brief summary of the eviction story: the villain is on the left, above – he is Thomas Henry Marmion JP, principle landlord of Castle Island. He lived from 1839 to 1921 and – incidentally – his father (who had the same name) was said to have been responsible for providing the ‘soup kitchen’ at the Steam Mill, Skibbereen during the Great Famine of the 1840s. Notwithstanding this, recorded history does not have much that’s good to say about the Marmions, who in the eighteenth century had been land agents for the Bechers and Townsends. At the beginning of March 1890 (as reported, somewhat floridly, in the Cork County Eagle):
. . . A few days ago, the sheriff’s officer from Skibbereen made his appearance in Schull, surrounded by a force of police, on an evicting expedition. After a short delay, they proceeded to the water’s edge where their galleys were found to await them and the sheriff’s representative having secured himself in one of the crafts, the whole party proceeded to sea for a distance of some three miles when they landed on Castle island. This wild and sea-washed home of a few small farmers and fishermen is the property of Mr Thomas Henry Marmion . . . whose interest in recent years appears more of an incumberance or embarrassment than any advantage as the poor creatures who live in it (misnamed farmers) and on the many islands surrounding it, have to live chiefly on the profits of the sea. The fortification of Jerry Nugent was the first laid siege by the invading army, Jerry’s offence being that he owed a few years’ rent which he found impossible to pay and he was, therefore, sent adrift on the sea-washed rocks where he had a full view of the passing emigrant ships which will probably bear him away to seek out a livelihood in the land of the stranger . . .
Cork County Eagle, march 7th, 1890
There’s much more – and it’s a harrowing story – not untypical, of course, of what was happening all over Ireland during the nineteenth century. In the portrait gallery, above, the figure in the middle is a ‘hero’: he is William O’Brien MP, a founder of the National League who, in September 1890 visited West Cork and held a meeting on Middle Calf island to support the case of tenants evicted from Castle Island and the Calves. On the right is James Gilhooly, MP, Bantry, who was chairman of the ‘All for Ireland League’ and who strongly supported the Castle Island tenants and attended many official meetings on their behalf. Matters rumbled on laboriously into the mid 1890s: eventually, it seems that the introduction of new land purchase acts (benefitting tenants), enabled six tenants to return to, and continue to occupy, Castle Island. As yet I have found no further records to help us establish how long occupation of this sparse rocky outcrop in Roaringwater Bay continued into the twentieth century.
The Mizen Journal, Volume 5 1997, has published a study by Anthony Beese of the place-names on Castle Island. I have been unable to locate this article online, but here is Anthony’s excellent map, above.
When we visited the island on a brooding August day we sensed its many ghosts, perhaps including those who returned over a hundred years ago and, possibly, lived out their working lives there. I have called this post ‘Facts and Fictions’ . . . You have had the facts. After I wrote my first post, last year, I received a communication from a writer: William Wall. I was delighted to learn that he had written a book – Grace’s Day – published in 2018, part of which is set on Castle Island. I obtained the book and read it avidly: it has opened up for me a new dimension in the story of the island – and it’s thoroughly believable.
. . . A long time ago I had two sisters and we lived on an island. There was me and Jeannie and Em. They called me Grace, but I have never had much of that. I was an awkward child. I still am all these years later. Our house had two doors, one to the south, one to the north. Its garden looked towards the setting sun. It was a garden of apple trees and fuchsia and everything in it leaned away from the wind. Dry stone walls encircled it and sheep and children broke them down. My mother lived there with us. Boats came and went bringing food and sometimes sheep, and there were times when we lived by catching fish and rabbits, though we were not so good at either . . .
Grace’s Day – a novel by William Wall, published by new island books 2018
William Wall is familiar with West Cork: he has stayed here many times, and has visited Castle Island. It’s not just the island, but the whole story of 1960s West Cork that has been his inspiration. Readers of this Journal will be aware of my own interest in the days when Ballydehob became the hub of an artists’ community: I have helped to set up the Ballydehob Arts Museum, which has celebrated this era and is now in ‘suspended animation’ due to the Covid outbreak. I also look after a website for the Museum. Grace’s Day is set in this era, and follows the unconventional lives of a family who is ‘getting away from it all’ and trying to survive following the then prevalent bible of self-sufficiency. It’s perfectly feasible that an abandoned island in Roaringwater Bay could be the setting for such a romantic pursuit of ideals. I won’t give away any spoilers, but one more extract could help to persuade you that this book is for you. You should find it in all good bookshops: please support them in these tricky times.
. . . One day on our island my sister Jeannie ran in to say that she had seen a whale in the sound and I ran out after her, my mother calling me: Grace, it’s your day, take Em. But I was too excited. And there were three fin whales making their way into the rising tide. We heard their breathing. It carried perfectly in the still grey air, reflected back at us now by the low cloud. The sea was still and burnished. We ran along the rocks watching for their breaching. We decided it was a mother, a father and a calf. They were in no hurry. When we reached the beacon, a small unlit concrete marker indicating the western edge of the island, we watched them breaching and diving into the distance until we could see them no more. But they left behind their calmness and the unhurried but forceful sound of their blows . . .
GRACE’S DAY – A NOVEL BY WILLIAM WALL, PUBLISHED BY NEW ISLAND BOOKS 2018
Our own view of Castle Island in the distance, surreally shadowed by the full moon’s glimmer, while the Fastnet Lighthouse winks away on the horizon
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Roaringwater Journal 