Irish Landscape

Extreme Green – Castlehaven

There are many places in West Cork that deserve more than one visit. Our enforced confinement close to home focusses us on that thought. March went out like a lamb and – on the first day of April – we went off to enjoy the stirrings of spring in one of our favourite spots: Castlehaven.

Here’s that spot seen from above. It’s accessed from a boreen that goes nowhere else, and is to the south west of Drishane, just outside Castletownshend. In the view you can see the little cove and an old burial ground which surrounds the ruin of the original church of St Barrahane, probably built on medieval foundations but disused by the 1600s. This benign place has bathed in some momentous historical events but is now forever peaceful and seems far removed from our material world.

The 25″ OS map – dating from the late nineteenth century – marks the main features of Castlehaven: the ‘Grave Yard’, Rectory (based on an older house) and ‘Toberbarahane’ – a holy well. One of our favourite walks begins just to the south of the graveyard and wends its way up to the well, – and beyond – following a small stream which has ferociously gouged a channel through the rock formations in ancient glacial times. Today I can only describe the experience as ‘Extreme Green’ because our eyes are drawn to a riot of spring growth and exotic flora. In fact, Finola described it as a rainforest path when we first visited a few years ago.

The Holy Well is still revered, evidently, especially by sailors who need protection while at sea. The saint was known as Bearchán, and most likely came from the Corca Laoighde family  (the Annals describe the O’Driscolls as kings of the Corca Laoighde in the twelfth century), although we can find very little of his life. According to Pádraig Ó Riain’s A Dictionary of Irish Saints, Bearchán’s pattern day is not known, but Amanda gives it as 3rd December in Holy Wells of Cork & Kerry, something which she must have gleaned from local knowledge.

The Holy Well is easy to find and involves crossing a stout timber bridge to the left of the path. On our previous visit, three years ago, a tree had fallen across the path and the bridge was damaged, but this has now been put right.

Finola is coming back along the holy well path, and the bay of Castlehaven is immediately beyond her. The colour of the sea is stunning azure at this time of the year. Just beyond the gate, and sited right above the strand, is all that is left of Castle Haven, a strategic tower house which saw action on 6 December 1601, during the Nine Years’ War between Gaelic Irish lords and the English. The O’Driscolls, who held the castle then, had welcomed in a small convoy of Spanish munition ships. The commander of the English naval forces based at Kinsale, Admiral Leveson, was ordered to “. . . seeke the Spanish fleete at Castlehaven, to take them if he could, or otherwise to distresse them as much as he might . . .” I’ll leave the rest of this story as a cliff-hanger, to be completed in a future post, but we will return to the castle which gave Castlehaven its name.

The old photograph dates from the late 1800s and is from the Lawrence Collection, courtesy of the National Library of Ireland. My photo shows all that remains of the castle today: a section of stone walling close to the cliff face. Its downfall occurred in 1926 and we know this because:

. . . Edith Somerville recorded that while taking a walk on 26 February 1926 she heard a loud rumble and in looking towards the direction of the old tower found that it had collapsed. Nowadays only a mere stump remains, and that covered with briars and weeds. The castle stood on the side of the harbour of Castlehaven, to the immediate south of the stony grey beach, and the decayed church, graveyard and holy well of St Barrahane, the local patron saint who gives his name to the nearby glen and castle. The castle and haven was known as Cuan-an-Chaisleán to the Irish, as Castlehaven to the English, and El Puerto Castello to the Spanish, but they all mean the same thing . . .

The Castles of County Cork by James N Healey, The Mercier Press, 1988

In the next post I’ll be telling you more about the pivotal sea-battle at Castlehaven between the Irish – Spanish alliance and the English forces; and setting out a case of mistaken identity. We will also be exploring another Castlehaven Castle, and looking into a salacious scandal that led to a beheading or two in 1631. There’s much to look forward to…!

Following the Cascades (Sweet Ilen – Part 7)

There’s a walk that goes down from Castledonovan to Drimoleague: it follows an ancient mass path and much of it is right alongside the Ilen River. At its northern end there is a section known as the Deelish Cascades: this is geologically fascinating, and gives us some insights into how our West Cork landscape was formed thousands of years ago.

. . . The oldest rocks exposed in West Cork are of Devonian age (410 – 355 million years ago) . . . These mostly red and green sandstones, siltstones and mudstones were deposited on a continental landmass in a low latitude desert or semi-arid environment. The sediments were deposited from rivers, whose flow was dominated by flash-floods fed by episodic rainfall, which originated predominantly from mountainous areas lying to the north which were were formed during the Caledonian Orogeny (mountain building event) in latest Silurian and early Devonian times. The environment was perhaps similar to the present day Arabian desert. This “Old Red Sandstone” continent extended over what is now northwest Europe. In Cork and Kerry these sediments accumulated in a large subsiding trough (the Munster Basin), resulting in one of the thickest sequences of Old Red Sandstone encountered anywhere in the world (at least 6km thick) . . .

Geology of West Cork, M Pracht and A G Sleeman, geological Survey of Ireland 2002

I have marked on this Geology Map the course of the Ilen River from its source on Mullagmesha Mountain to the tidal estuary which begins at Skibbereen. The map shows the ‘grain’ of the various faults which run SW to NE over the terrain: the river generally flows perpendicular to these faults, and the ‘grain’ is clearly seen in the exposed river bed running over the Deelish Cascades.

Praeger usefully simplifies the geological definition of the landscapes (for more on Praeger see Finola’s complementary post today):

. . . The story which geology tells as to how West Cork and Kerry got its present form is interesting, and I shall try to tell it in non-geological language. Towards the close of Carboniferous times – that is, after the familiar grey limestone which covers so much of Ireland and the beds of sandstone and shale which succeeded it were laid down on an ancient sea-bottom, but long before the beginning of the Mesozoic period, when the New Red Sandstone and white Chalk were formed – the crust of the Earth in Ireland and beyond it was subjected to intense lateral squeezing from a north-south direction. This forced it into a series of great east-west folds, thousands of feet high from base to summit – the Carboniferous beds on top, and below them and following their ridges and hollows the massive strata of Devonian time, and other deeper-buried systems. A series of pieces of corrugated iron laid one over the other will illustrate what happened. The folding was developed particularly conspicuously in the Cork-Kerry area. What we see is the result of this ancient crumpling, now greatly modified by the effect of millions of years’ exposure to sun and frost, rain and rivers . . . The more resistant slates, carved into a wilderness of mountains, still tower up, forming long rugged leathery ridges. A sinking of the land has enhanced the effect by allowing the sea to flow far up the troughs. That the ridges were longer is shown by the high craggy islands that lie off the extremities, and continue their direction out into the Atlantic . . .

The Way That I Went, Robert Lloyd Praeger, Methuen & Co London, 1937

While the upheavals of far-off eras reaching back millions of decades certainly laid the foundations of our landscape, the geological events which actually honed the shaping of the terrain as we see it today are far more recent – the ‘Ice Ages’ which developed only 30,000 years ago and had receded by about 10,000 BC. During that time sea levels fell and then rose again, and the topography and shoreline of the island with which we are familiar today was established. The ice sheets covered most of the land and were up to 1,000 metres thick. As they melted, glaciers fell away from the highest points and carved fissures into the slopes, creating valleys and rivers. One of the most extensive ‘local’ ice-caps was in south-west Munster where a ‘Cork-Kerry’ glaciation, centred on or close to the Kenmare river, developed independent of the general ice sheet. Our own ‘Sweet Ilen’ was a consequence of the ice movement, and the rock formations that we see in the Deelish Cascades are good evidence of these modern geological events.

All the way down the Cascades you will see evidence of the scouring of the rocky river bed, and huge ‘erratic’ boulders that have been carried from the mountain-top on the ice flow, to be deposited randomly – and picturesquely – in the torrent. Of course, you don’t have to know about geology to appreciate the walk: you are free to explore the well kept path and delight in this West Cork experience which has been laid out for us all through the mighty efforts of the Drimoleague Heritage Walkways and the Sheep’s Head Way.

Previous episodes in this series: Sweet Ilen : Sweet Ilen – Part 2 : Sweet Ilen – Part 3 : Sweet Ilen – Part 4 : Sweet Ilen – Part 5 : Sweet Ilen – Part 6

Winter Light in West Cork: Lockdown Edition

We’ve both been dipping in to Robert LLoyd Praeger recently – Robert for this week’s post on the Ilen Cascades and me for pleasure. Praeger’s classic book The Way That I Went, was published first in 1937 and has never been out of print (this is the edition we have). My browsing reminded me that I tried a Praeger approach to explaining our West Cork landscape a few years ago, in a post post titled Wild Atlantic Light – the West Cork Winter Edition. I am having another go at it now with edited text and new photographs, all taken in the winter months. Mostly what I was trying to do then and now is to explain the West Cork landscape – what gives it its form and shape and colour and startling beauty. Being in lockdown since Christmas has forced us (even more than usual) to engage with our territory on a deeper level, seeking to understand what makes it the way it is.

Of this area, Praeger says,

At the Southern end of this land of great mountain promontories, in West Cork, you find yourself in a little-known and tourist-free region of much charm. You stay on Sherkin Island . . . or Cape Clear island . . . , at Schull or far out at Crookhaven: and you walk and boat and fish and lounge and bathe, and enjoy the glorious air and sea; towns and trams and telephones seem like bad dreams, or like fugitive glimpses of an earlier and inferior existence. A meandering railway penetrates to Schull, and the roads are as good as you could expect them to be in so lonely a country. All is furzy heath and rocky knolls, little fields and white cottages and illimitable sea, foam-rimmed where it meets the land, its horizon broken only by the fantastic fragment of rock crowned by a tall lighthouse which is the famous Fastnet.

Things have changed quite a bit since the 1930s, of course – how we wish that little railway was still running or that the ‘our’ part of Ireland had remained ‘little-known.’ But while it may seem that Praeger is describing a whole other world, enjoyed in the summer, the fundamentals remain. For example, as Praeger pointed out, West Cork is a maritime area and that affects our weather. It means that clouds are plentiful at all times of the year and that the weather can be highly variable and unpredictable. But the ocean, and the Gulf Stream it carries all the way from the Gulf of Mexico, ensure that we have a slightly milder climate than the rest of Ireland. Beside the sea, the air is full of negative ions. That’s a good thing. Negative ions stimulate our senses and lead to a heightened sense of wellbeing.

Sure, we can have rainy days and bitter winds in the winter, but there are lots of sunny days too. When the sun shines in the winter, it is filtered through those drifting clouds to produce those marvellous effects of light and shade that lend such drama to the landscape.

In winter too, the colours are highly contrasting – the green of the fields change abruptly to the blondes and golds of the higher mountains. The bracken turns the colour of amber and the fionán grasses provide an expansive sea of rippling heath on higher ground.

We don’t get snow very often, but it’s certainly visible on the high points, such as on the Caha Pass between Glengarriff and Kenmare. Praeger loved this dramatic geology with its crags and folds.

Under a blue sky the sea in West Cork turns the colour of the Mediterranean or the Caribbean. and this is particularly striking in the winter, perhaps because it’s so unexpected. They tell me it has to do with having a sandy bottom and I am sure there are other scientific explanations, but really, you have to see it yourself to believe it.

Our underlying geology (see Robert’s post again for Praeger’s explanation) provides the ruggedness, the exposed sandstone ridges, and the deep coastal indentations that characterise the landscape.

The end result of it all – the sunshine, the clouds, the mountains, the sea, the contours and colours of the land – is the kind of light that artists dream of. The sheer clarity of it is startling – you can see from one end of the peninsula to the other in a way that city dwellers have forgotten it’s possible to do. That clarity brings out every hue and allows all the colours to sparkle against each other.

The photographs in this post were all taken from the depths of winter to the first glimmerings of spring. Robert Lloyd Praeger found this area entrancing in the summer – he should have come in the winter! The last light of a winter evening would have set his heart aflutter.

Mizen Mountains 6 – Derrylahard East

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.

Previous posts in this series:

Knockaphuca, Corrin, Letterlicky Cairn, Lisheennacreagh, Knockatassonig

What The Forest Was Hiding

There are new forests going in all around us here in West Cork. While Ireland desperately need more trees, mostly in this area they seem to be sitka spruce – a species we have come to dislike intensely since it creates an ecological zone which does not appear to support much biodiversity; it covers, hides and damages much of our historical and archaeological heritage; and it creates dense dark patches on the landscape.

Contrast the biodiversity of a forest of sitka spruce with a planting of deciduous trees

At the end of their growing cycle – 30 to 50 years – the forest is clear-felled, creating an ugly and hazardous environment into which new seedlings are planted. Best practice forestry nowadays is supposed to mix in broad-leaves species, leave nurse logs and open spaces, keep streams clear and accommodate natural habitat throughout the planting.

In our recent walk through a clear-felled forest we saw little evidence of best practice – indeed the seedlings were already in place, in serried ranks and all one species (above). 

In this forest, explored last year, a clearing has been left for a ruined cottage

While an identified and recorded national monument is given a clearing (usually inadequate) in a plantation, other parts of our heritage are simply hidden, destroyed or damaged by the heavy equipment. Alerted by a friend (thank you, Lydia!) we took a walk yesterday on a clear-felled stretch of hillside, to see what the forest had been hiding.

The townland is Derryconnell, between Schull and Ballydehob so it’s within our 5K travel limit. We parked by the gate and walked up the well-maintained forestry road, with the clear-felled landscape all around us. It’s hard not be emotionally impacted by how devastated a landscape like this appears. Clear-cutting is highly controversial, with its proponents arguing that it can be done in an environmentally-positive and sustainable way. I have no idea, because I have no expertise in this area, if this particular patch has been cut using good science – perhaps others can comment.

The trees had been cut after 30 years of growth – I counted the tree rings

We soon saw what we were looking for – the end walls of old stone buildings. We walked up to each in turn, marvelling that they were still to be seen where they had once been completely hidden by trees. There was a west building, a middle set of two (below), and an east building.

It’s hard to know when stone structures like this were last lived in or used and it’s tempting to call something like this the remains of a famine village. However, some of them had cement detailing that indicated they may have been abandoned more recently than their ruinous appearance suggested. Lydia had noticed some late nineteenth or early twentieth century delph – in her photograph some bits looked hand-painted and some looked like transfer ware. 

I went back to early OS maps and Griffith’s Valuation to see if I could put a date on what I was looking at. The earliest map, the Historic 6 inch, dates from 1829 to 1841. It clearly shows (above, on the right, near the red townland boundary) the middle two side-by-side buildings, so we can say for certain that whoever was living in the side-by-side set at the time the map was made, lived through the Famine. The house showed signs of later renovation (cement rendering around a window) so it may have been occupied or used into the twentieth century. 

Above: The two buildings, house (closer) and barn, showing the cement rendering outside the window

These two middle buildings formed a smallholding, with a clearly defined haggard outside the right-hand building. Along this haggard and leading to the house was an old green road (below). We’d like to go back sometime and trace how far this goes – it looked very inviting. 

The right-hand building of the two (below) had two doors but no fireplaces and therefore was most likely in use as a barn. It’s a substantial building but with few features except for a ledge along one wall.

The left-hand building (below) was clearly a house, with a fireplace at each end. The larger fireplace had fallen and the collapse indicated that it had been a tall chimney. This was the principal room of the house, where most of the living and all of the cooking took place.

The other room also had a fireplace and this was a curious small affair, with the flue accommodated entirely within the thickness of the end wall.

Top: the end wall with its small fireplace; Middle: the flue within the walls; Bottom: the top of the wall showing the flue exiting

The easternmost building was very broken down and overgrown and it was hard to make out its features, but we did manage to establish that it had the same kind of small in-the-wall fireplace as the previous cottage, as well as some concrete detailing.

This is the latest of the structures, only showing up on the map that dates from the late 1880s to 1913. The map shows a longish building, with two projections at the rear, neither of which have survived. Given that it’s the newest building, it’s perhaps surprising that it hasn’t fared any better than the others.

The east building on the Historic 25″ map, showing that it was constructed after the 1840s but before 1913. On this map you can also make out the green road that runs behind the middle set of buildings

Finally, the westernmost building, which may or may not appear on any of the maps, has two distinct ‘rooms,’ neither of which has a fireplace, although outwardly it bears the appearance of a house/barn combination (below). There’s a small black dot on the earliest map (the Historic 6”) about where this structure is now, but it doesn’t seem substantial enough for what’s on the ground. Therefore, it seems that this building, or most of it, is also later in date and may even post-date the map from the turn of the 20th century.

Who lived on this section of land? To answer this question we can turn to Griffith’s Valuation. This was a survey of Irish land that took place between 1848 and 1864, to establish the value of property for taxation purposes. The results are online and searchable by townland. The map tells us that the land we are looking at was parcel number 2 in the townland of Derryconnell (below). It was occupied by several tenants, despite the fact that only the side-by-side set of houses are on Griffith’s map. Perhaps the other tenancies refer to the renting of fields. 

What Griffith’s Valuation shows for parcel 2 is that William, Michael and Jeremiah Coghlan rented land from Thomas Cave, and in turn rented land (probably single fields) to Patrick Tuohy, Denis Driscoll, Ellen Spillane, Thomas Sheahan and Michael Sheehan. The Coghlans therefore acted as middlemen between Cave and their renters, illustrating one of the problems with the land systems at the time with the poorest having to pay enough so that a middleman (sometimes a series of them) could get their cut. 

We don’t know much about Thomas S Cave, but he owned extensive property around this area much of which had previously been part of Lord Audley’s mining interests. Beside the Derryconnell lands, he also owned plots in Rossbrin, Cappaghglass and Foilnamuck – all areas associated with mining – and he owned and may have lived in Cappagh House, a beautiful period property we featured in our post on the mine chimney that blew down and now lived in by our lovely neighbours Mark and Terri O’Mahoney and their family. Below is an old photograph of that house and the chimney as it stood then.

This has turned to be a little meander though history, geography and ecology and all the more enjoyable as I didn’t expect to be so stimulated when we set out for a simple walk within our 5K limit. Once again, thanks to Lydia, friend and fellow history buff, for the information on where to go, how to get there, and what to look out for.

Back to the Irish Canals

Our readers with good memories may remember a long-running series I penned five years ago, about the canals of Ireland. I revisited that series recently – for a Trasna na Tíre talk* – and realised that I had left it incomplete back in 2017! What better time to finish off the journey than now – when we can only travel outside our lockdown limits through virtual technology?

In 2016 Finola and I explored part of the Irish canal system, following in the footsteps of Tom and Angela Rolt who had voyaged the same way exactly 70 years before, in 1946. They were pioneers in their day, as boating for ‘pleasure’ on the canals was rare. In their book Green & Silver they also managed to capture, in words and photographs, the essence of a decaying transport system in Ireland immediately following WWII, and our travels tried to give an impression of the considerable transformation of inland waterways in Ireland since their time. We traversed, on road and on foot, their voyage around the Shannon Navigation, and the Grand and Royal Canals.

The upper photograph was taken by Angela Rolt in 1946: it shows the Rolt’s boat moored up in sleepy Robertstown (Grand Canal), receiving the attentions of a crowd of small children who had never seen a pleasure cruiser before. Below that is the photo of Robertstown we took in 2016, seventy years later. Our own travels in that year, however, omitted the Rolt’s journey through Dublin, when they had to pass across the Liffey and Dublin Port to get from the Grand Canal to the Royal Canal. The header is an extract from a 19th century map of the docks area in Dublin.

That’s the ‘Green & Silver’ route, above, which the Rolts travelled in 1946. Starting from Athlone they went anti-clockwise around the triangle formed by the Shannon Navigation, Grand Canal; and Royal Canal. This involved crossing the Liffey in Dublin

We have visited Dublin many times in recent years, and I managed to take photographs to complement those of the Rolts, in order to finally complete the ‘Green & Silver’ series today. First, however, let’s try to get an idea of the scale of Dublin Port by comparing aerial views, like by like, of that district and our own Rossbrin Cove in West Cork. The scale and area of each of these two photographs is exactly the same (1600 hectares): the demography (population and land use) couldn’t be more different.

. . . After tea we journeyed on through Landestown and Digby Bridge Locks to the Leinster aqueduct over the River Liffey. It was an attractive pound, the canal skirting a ridge of high ground on our right with a view over the valley to the left until it turned to cross the river. As there was little traffic about, we stopped for a few moments on the aqueduct, an impressive structure of four arches, to look down at the swift flowing peat-stained waters which we next should see, and enter, in the heart of Dublin . . .

Green & Silver by L T C Rolt, Chapter 6
Top – early print of the Leinster Aqueduct, Grand Canal; lower – the Rolts pause to admire the structure as they cross the Liffey on the aqueduct

. . . The day before we were due to leave our moorings at Grand Canal Dock I thought it as well to reconnoitre the entrance from the Liffey into the Royal Canal at Spencer Dock, North Wall. The channel into the tidal lock was barred by an enormous rolling lift bridge over which an endless procession of cars and lorries was rattling and thundering. To my eyes it appeared as though this formidable barrier was seldom or never moved. In any case it seemed optimistic to suppose that this ponderous mechanism would be operated, and the traffic along North Wall suspended, merely to allow the passage of our small craft. Looking up at the dock I saw yet another obstacle; a drawbridge this time operated by two steel beams high overhead which looked at this distance, with their long rods linking beams to bridge, like a pair of slender, long-beaked birds. This carried Sherriff Street, another busy thoroughfare, across the dock . . .

GREEN & SILVER BY L T C ROLT, CHAPTER 8
Top – Tom Rolt surveying the Scherzer style ‘rolling lift bridge’ located at the entrance to Spencer Dock, Royal Canal, in 1946. It was erected by the firm of Spencer & Co of Melksham, Wiltshire, in 1912. The bridge was worked by an electric motor – now removed. Lower – the bridge in the present day

. . . It looked as if our passage bade fair to dislocate the traffic of Dublin. I thereupon visited the engineers department of Corus Iompair Eireann at Westland Row Station where I tactfully suggested that if I came up to North Wall at low tide we might just be able to get under the bridge there, but I was received with helpful courtesy and matters were quickly arranged. Of course the bridge would be lifted, that was no trouble at all. And when did I wish to come up the river. To-morrow? High tide was at noon; if I would undertake to be at the bridge at that time it would be opened at once. Arrangements were made on the spot by telephone . . .

GREEN & SILVER BY L T C ROLT, CHAPTER 8
Upper – Angela Rolt’s photograph of the Sherriff Street lift bridge at Spencer Dock, Royal Canal, in 1946; centre – the lift bridge today (courtesy  William Murphy aka Infomatique). Lower – the overhead beam lift bridge mechanism is a principle often found on canal navigations: here is a more vernacular example on the Barrow Navigation (from Ireland of the Welcomes, 1971)

. . . Next morning we crossed the waters of the outer basin and entered the tidal lock. Actually there are three locks of different sizes here, side by side, and we entered the smallest of them which was on our port side. The lower gates opened, we paid a final farewell to the Grand Canal, and were soon dancing over the little waves of the Liffey mouth. It was our one brief taste of salt water. Having made sure that no steamers were on the move to or from the quays, we headed straight across the channel and came up the river close to the North Wall side. We swung straight in and got our lines onto the quay wall precisely at the time appointed. Everything went like clockwork. The bridgeman clambered up into his overhead cabin, men appeared from nowhere armed with red flag to stop the traffic and in a few moments, with a rumble of machinery, the bridge opened remarkable swiftly. We passed through into the tidal lock, and the bridge as quickly closed behind us. While the lock was filling, I paid my dues, two pounds for the ninety-two miles and forty-seven locks to Richmond Harbour. This done, the Sherriff Street Bridge drew up with similar despatch and we sailed through to begin our journey on the Royal Canal. Probably very few of the thousands who pass over the North Wall Bridge or board the steamer for Liverpool or Glasgow at the nearby quay suspect that this is the gateway of a forgotten water road which leads through the heart of Ireland . . .

GREEN & SILVER BY L T C ROLT, CHAPTER 8

Grand Canal Dock, Dublin – photographs which we took in 2014 (above). The decline which was apparent then continues to this day. Currently there is a plan to sell much of the land for redevelopment. It goes without saying that navigable water will need to be retained to allow access from the Grand Canal itself to the Liffey. Below – another context for the Port of Dublin in the 1950s!

The Heinkel Kabine ‘bubble car’ was designed by the same company which produced German long-range heavy bombers during the Second World War: this famous micro-car was manufactured for a short time between 1956 and 1958 under licence in Dundalk’s Great Northern Railway Ireland (GNRI) works. More than 6,000 were manufactured here.

The beauty of the rural Royal Canal: Chaigneau Bridge, Ballybranigan, Co Longford in 2016

The previous series of Roaringwater Journal posts on Irish waterways can be found (in reverse order) here.

*Robert’s Trasna na Tíre talk can be reached on this link.