Tag Archives: Lough Ree

Cupid at Athlone

Aquatic Excursion (from a correspondent)

Athlone (2003)

September 17, 1846 — The Amateur Band of St Peter’s, who deserve so much from the inhabitants of Athlone for the many opportunities they seize upon, to amuse them, having provided — on a large scale — for themselves and guests a sumptuous and plentiful feast, with the necessary teetotal drinks, sailed up the lake on last Sunday in the Cupid Steamer. The day was beautiful and inviting and the placid stream of the noble Shannon — as if in harmony with the circumstance — opening wide its expansive bosom to receive them, displayed in gorgeous grandeur, the verdant beauties of its multitudinous islands and grove-covered promontories of its indented coasts.

I never saw the lake to such advantage as on that occasion. We had about eighty persons on board, amongst whom were the Rev Mr Philips CC and RW, Mr Keating and family, and other pic-nic parties, with viands and refreshments in abundance. As the steamer made the lake and swept through an Archipelago of islands — namely, Carbery, Kid, the Wren, and Crow Islands, &c, having the wood-embosomed Hare Island, the present insulated residence of my Lord Castlemaine, on the right and the grove-crested cape of the Yeu or, as some call it, the Loo Point on the left — then it was that she breasted the serene bosom of this inland ocean not as Byron says, “walking the waters like a thing of life”, but bounding over its mirrored surface like an impetuous courser she seemed to devour the distance, while she tossed a road of foaming surges from her heels.

On each side appeared emerging from wood and grove beautiful villas and noble ruins, towers and antiquated telegraphs, with their declivous lawns sweeping to the water’s edge. As we passed between Inchmore, Innisbofin, the Nun’s Island, the cultivated and rich callows of the Longford coasts, and Warren’s Point, St John’s and Mount Plunket on the Roscommon side, hill and dale land and water reverbrated with the dulcet tones of our excellent band under their inimitable instructor, Mr Keating, while at intervals the gay and cheerful dance on deck, to the music of the violin, enlivened the enjoyment of the exhilirating prospects that accumulated around us.

One or two objects which I observed, struck me very forcibly, and reminded me of the left-handed, nay, monopolising policy of former days, and the state of vassalage under which we yet groan and which “Ireland for the Irish” would never tolerate. In a beautiful valley, and modestly peeping from the clustering foliage of circumnambient trees and in accommodating contiguity to the “big house” stood the snug and aristocratic church of the minority, styled in legal parlance “the Established”, while at a distance on the bleak hill of Newtown, exposed to wind and weather, a chapel dedicated to the worship of the millions, displayed all the frigid isolation of a step-mother’s care.

We now arrived at Quaker’s Island, and having tacked about, we made for Warren’s Point, on our way home, and went on shore at St John’s Castle. With feelings of deep melancholy mingled with admiration, we viewed the venerable ruins of this once majestic pile (huge masses of which lay scattered here and there), its dismantled bastions, deep fosse, and the roofless walls of its antiquated chapel, while on a neighbouring hill stands the shell of its watch-tower to give timely warning of the approach of the feudal rival who would dare contest sovereignity with its lord. We then warmly and eagerly discussed the viands abundantly spread on the verdant sward at the base of

These ivy crowned turrets, the pride of past ages,
Tho’ mould’ring in ruins still grandeur impart.

After which the merry dance commenced, unconstrained laughter and encouraging shouts accompanying the performers, bringing the memory back to the times of rural felicity; when under the fostering tutelage of a domestic legislature, every family had its own quern to grind its own grain, every peasant could drink his own beer and the daily toil of virtuous industry being over, the children of simplicity, to the sounds of the oaten reed or the violin, or the more national bag-pipes, tripped it gaily on the “light fantastic toe”. And this was the happy and tranquil state of “Old Ireland” before the importation into it of such exotic materials as Sir Walter Raleigh and his rotten potatoes. To return to the ruins. I wish Lever, Carlton, or some one of those compilers of Irish legendary lore, had visited Lough Ree, he would find there more traditionary facts connected with the pristine magnificence of the different localities, than very many of those which have been already noticed in Magazines.

Having embarked once more we soon arrived home, and thus ended to the satisfaction of all parties, one of the most amusing days I, at least, ever spent in my life. To Bernard Mullins Esq, the young men composing the band return their sincere acknowledgements, for his kindness in accommodating them with the Cupid for this very pleasant excursion.

O’B

Athlone Sentinel 18 September 1846

Garryowen and the Royal Canal

The shortage of water for the Royal Canal has been covered a few times on these pages with pieces about its feeders in general, the Lough Owel feeder in particular and the proposed replacement supply from Lough Ennell.  Last I heard, the Lough Ennell proposal had become a matter for Irish Water rather than for the local authority, which sent the whole thing back to the drawing-board but if, Gentle Reader, you have more recent information, do please leave a Comment below.

A recent post about the inadequacy of back-pumping from the Inny led to a discussion in the Comments, from which it became plain that the Lough Owel feeder was well below normal levels and that the water supply to Mullingar, never mind that to the canal, was seriously inadequate. I was prompted to suggest that one of these might be the best type of boat for the Royal.

But I see from the blatts that the seventh cavalry, in the shape of Irish Water (whistling Garryowen, of course), intends to take water from Lough Ree to supply Athlone, Mullingar and Moate.

Perhaps there will be some to spare for the Royal Canal.

The current at Killaloe

I have been known to complain about the absence [on the interweb] of information about the state of the Shannon downstream of Banagher and Meelick.

Waterways Ireland

On the Waterways Ireland website, on the “About Us” menu, there’s a “Water Levels” option which takes you to this OTT Hydromet page. Perhaps my security settings are too high (or too eccentric), but at the top of the page all I see is

Alternate HTML content should be placed here. This content requires the Adobe Flash Player. Get Flash

At the bottom I read

Click here to obtain list of todays 9am Values. Please Note – Levels are recorded in meters to MSL Malin Head.

There is also a disclaimer.

The link goes to this page where the locations of various gauges are categorised by waterway. The furthest south [on the Shannon] I can find is …

Meelick Weir Gauge SS_MEELICK Water level 0001 32.62m 2018-07-07 07:30:00 5400

… from which I deduce that the water level at Meelick Weir is 32.62 metres above mean sea level at Malin Head. From that, of course, I can deduce the depth of the water at Meelick, or I could if I knew how far the bed of the river was above MSL Malin Head, and by charting the daily returns I could see whether the level was increasing or decreasing.

OPW

Alternatively, I could use the OPW’s gauge at Banagher, only a little way upstream, which shows me the depth, the change over 35 days and the level in relation to various percentiles of previous levels. That is a lot easier to read and a lot more useful: although a measure of flow would be more useful still, I can assume that a high level will be accompanied by a faster flow.

ESB

I have recently discovered that the ESB has a page with (admittedly for a small number of sites) information in a more user-friendly format than either WI or the OPW. To find it from the home page, select “Our Businesses”, then “Generation & Energy Trading”, then “Hydrometric Information”, then “River Shannon”, then “Beware of the leopard”. Alternatively, try www.esbhydro.ie/shannon for a list of PDFs.

Either way, the files available include

  • a hydrometric forecast for the Shannon
  • one-year charts showing levels at each of five locations: Bellantra sluices, Lough Ree; Thatch, Lough Ree; Athlone Weir downstream; Portumna Bridge; Pier Head, Killaloe
  • even more useful for anyone going near Killaloe Bridge, the total flow [in cubic metres per second] at Parteen Villa Weir and at Ardnacrusha.

Here, in flagrant breach of the ESB’s copyright, is the chart for Parteen Villa Weir:

The flow at Parteen Villa Weir

The flow has been pretty well flat, at 0, for some time. The Parteen and Ardnacrusha charts have accompanying tables giving the figures for the last 30 days; here are those for Ardnacrusha:

The flow at Ardnacrusha

Each of Ardnacrusha’s four turbines uses about 100 cubic metres per second [cumec]. The flow through Parteen Villa Weir is divided between the old course of the Shannon [which must get 10 cumec] and the new channel through Ardnacrusha. The combined flow through Parteen has been 11 cumec for the past week, and Ardnacrusha has been getting nothing (except a tiny amount on 3 July). That explains why the level of water at Castleconnell, on the old course, is slightly higher than normal summer levels (11 rather than 10 cumec).

And with no water going through Ardnacrusha, the level of Lough Derg is normal (see the chart for Killaloe) and there is no strong current at Killaloe.

Note, by the way, that the levels shown by the ESB are referenced to the older Poolbeg ordnance datum, not the Malin Head used since 1970: “Poolbeg OD was about 2.7 metres lower than Malin OD.”

Other sites?

If, Gentle Reader, you know of any other accessible web pages with user-friendly information on flows or depths on the waterways, do please leave a Comment below.

 

 

The Hind

The River Hind Navigation is not well known, which may be attributable to its non-existence. There were several proposals to make the Hind navigable, to link the town of Roscommon to Lough Ree on the Shannon, but none of them were implemented. One of them almost made it, though, and such interest as the topic has is the result of the Hind’s inclusion (or semi-inclusion) on the list of navigations for which W T Mulvany, Commissioner for Drainage, was responsible in the late 1840s and early 1850s.

Mulvany was responsible for five drainage-cum-navigation projects (and many drainage projects), whereof the Hind was the least important. The other four were

  • the Lough Oughter navigation, upstream on Lough Erne from Belturbet, which was never completed: various (mostly Fianna Fáil) insane politicians in the area are still trying to have it completed
  • the Cong and Belturbet Canals, which were abandoned before they were finished
  • the Junction Canal in the Ballinamore and Ballyconnell Drainage District, later known as the Ballinamore and Ballyconnell Canal, which had a brief and notoriously unprofitable existence, but which was later transformed into the Shannon—Erne Waterway, which was a good investment for Ireland because the Germans [or someone] paid for it
  • the Lower Bann navigation, linking Lough Neagh (which already had two links to coastal ports) with the North Atlantic in the middle of a beach near Coleraine. This was the only one of Mulvany’s navigations that was completed and that remained open, despite its complete uselessness, as the railways got to the area before the navigation did.

In this catalogue of commercial nitwittedness, the Hind had the advantage that it was delayed: an even more insane proposal, to drain the Suck into the Hind, meant that the Hind navigation scheme was deferred long enough to be abandoned altogether, which was just as well as the railway soon made any navigation unnecessary.

However, the proposal was there and, if you are very bored, you might like to read about it. But this is for anoraks: the subject is unimportant, the detail [163 endnotes] outweighing what little interest the scheme possesses. There are no photos of boats or of locks, because there weren’t any; there aren’t even any cat videos.

 

The Traveller’s Map of the River Shannon (1830)

The Traveller’s Map of the River Shannon. Arranged as a Guide to its Lakes and the Several Towns, Gentlemens’ Seats, Ancient Castles, Ruins, Mines, Quarries, Trading Stations, and General Scenery on Its Banks, Source in Lough Allen to the Sea, Leitrim, Longford, Roscommon, Westmeath, King’s County, Tipperary, Galway, Limerick, Kerry and Clare, Accurately Taken from the Survey made by J. Grantham, by order of the Irish Government, under the direction of the late J. Rennie. Printed and published for the Irish Inland Steam Navigation Company, 1830.

Oblong folio, 15 numbered maps printed in black with river and water features coloured in light blue. Original quarter calf green cloth boards, russet title to centre of upper boards, stamped in gilt with gilt fillet boarder. Repair to rear of plate 15, otherwise all maps in very good to fine condition.

Contents: 1. Map of Ireland, 2. Index Map. Lough Derg to the sea, 3. Index Map. Lough Derg to Lough Allen., 4. Kilrush to Tarbert and Foynes Island, 5. Foynes Island to Grass Island, 6. Grass Island to Limerick and O’Brien’s Bridge. 7. O’Briens Bridge to Killaloe and Dromineer. 8. Dromineer to Portumna and Redwood Castle. 9. Redwood Castle to Banagher, and Seven [Churches (Clonmacnoise)], 10. Seven Churches to Athlone and Lough Ree, 11. Lough Ree to Lough Forbes. 12 Lough Forbes to near Leitrim. 13. Leitrim to Head of Lough Allen. 14. map of Limerick, 15. Map of Killaloe.

Map 1 shows Ireland and its waterways at scale of 1″ equals 20 miles, Maps 2 and 3 show the key for 4-13, with table of falls of water along the route on former and table of distances on latter; Maps 4-14 each have a short descriptive panel; Map 14 shows Limerick from the north of King’s Island to the New Barrack in the south with key Map 15 from the town at left to Beal Boru at right.

Yours for only €1800 at Ulysses Rare Books in Dublin.

Up the Inny

The navigation of the River Inny from Ballynacarrow upriver to Lough Sheelin.

Mr Mullins’s steamer

Here is a little information about the steamer Cupid, which was owned or used by the contractor Bernard Mullins on the Shannon in the 1840s.

ESB water discharge info

Here is the ESB’s Notifications page, with info on the rate of discharge from its hydroelectric dams and weirs. Today (14 December 2015) Parteen Villa Weir is discharging 440 cumecs (cubic metres per second or, roughly, ton[ne]s per second down the original course of the Shannon. That’s 44 times the 10 cumec usually discharged and more than replaces the 400 cumec diverted through the headrace to the Ardnacrusha power station. The Shannon is therefore running at its pre-Ardnacrusha levels and the Falls of Doonass have regained their power.

Of course if Ardnacrusha didn’t exist, its 400 cumec would be coming down the original course of the Shannon on top of the 440 cumec already there, which would make for interesting levels of flooding.

That ESB page has a link to this infographic, which shows the sort of information I was trying to get across here. I usually start from Leitrim [village]; the ESB starts slightly further upstream at Lough Allen. Note that the Shannon’s few locks are concentrated upstream of Lough Ree: between them and Killaloe are only two locks, at Athlone and Meelick, so the river’s fall is very slight.

Update 2018: the ESB has a new page with lots of interesting information here.

Theft on Lough Ree …

… in the National Archives of Ireland May 2015 document of the month.

Down to the sea in steps

On 28 January 1907 James Robinson Kilroe [near the bottom of the page] of H M Geological Survey read to the Royal Irish Academy a paper on “The River Shannon: its present course and geological history” [Proceedings of the Royal Irish Academy Vol XXVI Section B No 8 Hodges, Figgis & Co Ltd, Dublin; Williams & Norgate, London 1907]. I thought that Plate V was interesting.

Shannon Derg to sea

Plate V

Kilroe wrote:

It will be perceived that instead of the river being shallow over the unyielding Silurian slate-rock, set almost vertically, and striking across the river-course, it is deeper than over the limestone of Lough Derg, and much deeper than over the comparatively easily eroded Old Red Sandstone at Killaloe. The river-bed actually drops below the datum line above the town, while at the town it is 100 feet above datum.

Old Red Sandstone strata are here to be seen in the river-bank, and Silurian rocks in situ in its bed. A barrier is thus formed, partly of Silurian, and partly of Old Red Sandstone rocks, which without the artificial impounding weir would retain the waters of Lough Derg to a depth of some 104 feet opposite Derrycastle — two miles above Killaloe.

One might have expected to find a fairly level shallow bed from Killaloe northward, a sudden drop from slate-rock to the sandstone floor, and  a pronounced wide, well-formed valley in the limestone district southward to Limerick.

None of these elements exist; instead, we have the formidable barrier at Killaloe, naturally damming up a considerable depth of water in Lough Derg, and the river falling away southward by a series of rapids which correspond with drops in the canal, south of O’Briensbridge […], along an alternative course, possibly one used by a branch of the Shannon.

Here is an extract from the Plate V map, showing the steps of the (pre-Ardnacrusha) Limerick Navigation between Lough Derg and the sea.

Shannon Killaloe to Limerick

The steps of the canal (click to enlarge)

Upstream

Kilroe wrote of Lough Ree:

The waters of Lough Ree stood some 10 feet higher within recent times than they now do, as proved by evidence of solution, with under-cutting of limestone blocks, to be seen about five miles north-west of Athlone, close to the railway, in the townland of Cornaseer.

Under these conditions the lake must have been, perhaps, twice its width, and for a considerable period. Its ancient surface-level is clearly indicated by the caps of the mushroom-shaped blocks.

And of the Shannon between Lough Ree and Lough Derg:

The extreme flatness of the river between Athlone and Meelick is such that, consequent upon the completion of the Suck Drainage-works in 1892, it was found that the callows along the Shannon above the confluence of the Suck at Shannonbridge were much more liable to sudden and frequent floodings than they previously had been.

The more rapid discharge of the Suck waters into the Shannon, before ordinary extra water had time to pass away, had the effect of modifying the regimen of the main stream to an extent which resulted in an action at law [La Touche -v- The Suck Drainage Board].

I have found only one account of that case, in the Freeman’s Journal of 1 July 1893. The plaintiffs, Messrs Harrison and La Touche, owned land at Cappaleitrim, on the west bank of the Shannon above Shannonbridge. They said that the actions of the Suck Drainage Board had caused their lands to be flooded:

[…] that the defendants brought water from the Suck into the Shannon, containing a drainage of 40 miles, with such velocity and such volume that the Shannon was penned back, and that the back water caused the damage to the lands complained of.

[…] The jury disagreed and were discharged.

I don’t know whether the matter ever again came before a judge.