The Avon takes its course from a moss in the
parish of New Monkland, and is augmented by a small tributary from
Tannyside Loch, and another stream from Moss Cannel. At the outset it is
dull and sluggish, but after cutting the flank of the Bathgate hills,
between Carrubber castle and Muiravonside house, its now wooded banks
rise nearly 200 feet. Running towards the flood mark of the Forth,
scenes still more precipitous and inaccessible are to be found on the
river as it bursts through the high-ground of Kinneil into the alluvial
carse. Good trout were common in its waters before poisonous pollution
came from lint-pools. It forms the south-eastern limit of the county,
and was anciently noted for its nunnery of Manuel.
The Blane – Beulabhuin,
pronounced Beul-uin, and signifying "river issuing from the
ravine" – rises from the earl’s seat in the Lennox hills. The
nobles of the old race of Levenax had a castle near, and in sight of,
this romantic spot. Speeding onwards, the stream proceeds in a
south-westerly direction for three miles, when, thereafter, it is
precipitated over several lofty falls. The lowest, but the most
remarkable of these is the Spout of Ballagan, a cascade 70 feet in
height. Here a very singular section of the hill is presented. The side
of it is cut perpendicularly by the water, and shows no fewer than 192
alternate strata of earth and limestone. Near the bottom of the section
are found several thin strata of alabaster of the purest white.
Fragments of antimony have also been got, and, when tried by a chemical
process, proved to be exceedingly rich specimens. After an additional
course of 8 miles, the Blane loses itself in the Endrick, which, in its
turn, flows westward to Loch Lomond.
The burn of Boquhan forms the boundary
between the parishes of Kippen and Gargunnock. Descending from the rock
of Ballochleam, it meets with the red sandstone through which it has
opened a passage, and wrought its soft materials into a number of
curious forms, resembling the wells and cauldrons of the Devon. After
running through a beautiful and well-wooded glen, along which the
proprietor of Boquhan has made extensive and agreeable walks, it
discharges itself into the Forth at the Bridge of Frew.
The Carron, famed in ancient Celtic song,
and of importance in modern trade and manufactures, issues from the
Campsie hills near the middle of the isthmus between the firths of Clyde
and Forth. Both the source and the place where it discharges itself into
the sea, are within the shire of Stirling, which it divides into about
two equal parts. The whole length of its course, from west to east, is
some 14 miles, the first half of which is spent among bleak hills and
rocks, but, when it has reached the low grounds, its banks are fertile
and wooded, and, as it advances, the neighbouring soil increases in
richness and value till, after passing through the carse of Falkirk, it
falls into the Firth of Forth. The stream is small comparatively, yet
there is no river in Scotland whose surroundings have been the scene of
so many memorable events. Etymological researches are for the most part
void of instruction, as they seldom result in certainty. Names of
rivers, mountains, and towns have perhaps more frequently had their
origin from casual circumstances than from important transactions, or
natural peculiarities. Nennius, an author of the ninth century, derives
the name of this river from Carausius, who is commonly called the
Usurper. The translator of Ossian’s poems informs us, that it is of
Gaelic origin, and that Caraon signifies "Winding
River." This fully expresses one characteristic of the stream,
which, in former times, before it had forced a new channel for itself in
some places, and been straightened by human industry in others, fetched
many serpentine sweeps in its passage through the carses. Nevertheless,
if we say that the original name was Caeravon, that is, river on
the Caers, or castles, alluding to the Roman fortifications upon
its banks, we probably give an etymology just as plausible, though
equally uncertain. A short distance from its source, the river enters
the Carron Bog. This vast plain and meadow lies partly in the parishes
of St. Ninians and Kilsyth, but chiefly in Fintry. Its length is about 4
miles, and its medium breadth 1 mile. Considerably elevated above the
ocean, it occupies part of the table-land between the eastern and
western coasts. It has, probably, been a lake at no very distant period,
and gradually filled by the hill brooks washing down debris. Part,
indeed, is a swamp scarcely passable at any time, but nearly inundated
by every heavy rain. Two miles below Graham’s castle, in the division
called Temple Denny, the Carron, having worn a hollow channel in the
rock, forms a beautiful cascade, by pouring its contracted stream over a
precipice above 20 feet in height. This cataract is little known, being
situated in a very remote and unfrequented valley, and, were we writing
in verse, we would say of it what Horace says of the little town, in
which he lodged a night, on his journey from Rome to Brundusium, "Versu
dicere non est." It goes by the name of Auchinlilly-lin-spout
– "Field of the overflowing torrent and pool." Spout is an
absurd tautology of what has been expressed with emphasis by the
reduplication of ly in the middle of the compound Celtic name.
When the river is in flood, and a triumphant torrent sweeps down the
glen, this cascade is unsurpassed among Scottish streams for the
grandeur of its storm of spray. The ruins of the Hermitage, too, are to
be seen here on the very margin of a deep fissure of rock. The rustic
cottage of whin-stone, now utterly desolate – roof fallen, windows
gone, and crumbling gables ivy and lichen draped – was built in 1801
by Mr. Robert Hill, W.S., Edinburgh, who had purchased the lands of
Forest Hill. It was a thoroughly romantic building, most suitable, in
its wild situation and surroundings, for habits inclined to the delights
of shrieking solitude. In 1840, a reservoir, near the Carron Bog, broke
through its embankments, when the heavy down-rush of water carried away
much of the masonry of the deserted house. Strange stories are told of
the reasons why men have been influenced to seek seclusion from the
world in an eremitical life, and we can readily imagine a powerful
combination of circumstances leading thitherward. Sad experiences may
have given them a distaste for society, or, possibly, noble aspirations
and generous feelings have been cruelly chilled and disappointed. But,
in early times, the recluse’s cave had often in or near it a rudely
carved chapel in the rock for piety and prayer, while the foliage of the
trees that surrounded the arched cavern gave a deeper shade of sanctity
to the lonely cell. Such, for example, as Bridgenorth Hermitage, in
Shropshire, wherein dwelt that royal anchorite, Athelward, the Saxon
prince, brother of King Athelstan, or the cave presently occupied by a
Welsh hermit, on the estate of the Earl of Powis in Montgomeryshire.
Leaving the hermitage ruins, the waters of the Carron rumble and foam
through a deep ravine for a spray-wreathed cauldron, from which, with
deafening din, they speed on buoyantly in their sea-ward course; where,
at many points,
"Grey rock is brown
beneath the flow of limpid water."
Over the serpentine road down-hill to
Denny the spirit of beauty everywhere prevails. The intervening
district, indeed, is famous for its pastoral undulations; and from
almost every breezy brae-top a charming view is got of the wooded banks
of the river – foliage which, even in the present green-tide, displays
all the variety of autumnal richness. The "Lady’s Loup,"
with the romance that hangs over the linn, merits more in passing than a
prosaic paragraph. But, here, we must simply refer the reader ignorant
of the tragic tradition to the well-known "Douglas" play, in
which the heroic incidents of the leap are fully and vigorously told.
"She ran, she flew
like lightning up the hill,
Nor halted till the precipice she gained,
Beneath whose low’ring top the river falls
Engulf’d in rifted rocks.
Oh, had you seen her last despairing look!
Upon the brink she stood, and cast her eyes
Down on the deep; then lifting up her head
And her white hands to heaven, seeming to say,
Why am I forced to this? she plunged herself
Into the empty air."
Now we tread ground filled with classic
memories. What a thrilling and matchless story we should have could the
river, as it rolls along, only tell of all it has seen and known! Here
Ossian, the ancient Gaelic bard, tuned his lyre; and here also young
Oscar won his brightest laurels in war. In a poem entitled "The War
of Caros," and dedicated to Malvina, the daughter of Toscar, the
son of Fingal, sang –
"He (Oscar) came not
over the streamy Carum
The bard returned with his song.
Grey night grows dim on Crona."
Historians also mention a bloody battle
fought upon the banks here between the Romans and the confederate armies
of the Scots and Picts, commanded by Fergus II., in the beginning of the
fifth century. Probably the two armies disputed the passage of the river
at Dunipace. The Romans remained masters of the field; but not without
such dreadful slaughter on both sides, that authors, in their
description of the combat, have used the extravagant, though trite,
hyperbole of the waters running red for miles with blood. From this
point to Dorrator and West Carron, the stream runs sinuously in a
flattish haugh, which varies in breadth at different places; and is, for
the most part, bounded by sloping banks of sand. For lovers of the
piscatorial sport merely, the Carron offers little attraction. It was at
one time, however, famed alike for the quantity, quality, and size of
its trout. The endless variety of alternate pool and stream, and the
openness of its banks, rendered it the favourite resort of the angler.
But its waters have been polluted; and it is, in fact, nothing now as a
fishing river, although a few of the common trout may occasionally be
hooked. Many rills, of course, find their way to the Carron. The Bonny,
supposed to be the Crona, celebrated by Ossian, falls into it about a
mile below the village of Bonnybridge. Near Camelon, it also receives
the Light-water-burn, which flows in the center of what, to all
appearance, must at some remote period have formed the bed of a
considerable river. The Grange Burn, too, from the upper part of the
parish of Polmont, unites with it in the vicinity of Grangemouth.
The Devon is a mere rivulet, which washes
a detachment of Stirlingshire, and divides it from Clackmannan. It has
its source among the hills in the parish of Blackford, Perthshire; and
was written Dovan in a charter granted by Robert III. to the burgh of
Inverkeithing. Dhu-avon, "black river," seems a not
improbable etymon, it being a deep and sable stream, as it lazily creeps
along the plain from near the Cauldron Linn, till it falls into the
Forth at Cambus, a course, including curves, of a dozen miles. Although
the run of the romantic and beautiful little river is peculiarly
circuitous and winding in its round of the Ochils, it flows at first
almost due east towards Glendevon; but, near the church of Fossaway, it
makes a sudden turn westward, and passing through the parishes of
Muckhart, Dollar, and Tillicoultry, gently glides along the southern
boundary of Alva district. It is somewhat odd, that the stream, after
having performed a circular route of about 30 miles, should end its
career nearly opposite the point at which it started on the other side
of the hills, reaching the Forth exactly where the latter assumes the
character of a firth, two miles above Alloa. The first of its principal
waterfalls is the Rumbling Bridge, so-called from the hoarse music made
by the river in its wonderful passage through arching rocks; but a
little further on, amid a series of cascades, we find the water
producing the curious excavation of that never empty boiler, the
Cauldron Linn.
The number of the lesser streams in the
county is legion. The Dualt, which flows through mossy ground in the
parish of Killearn, would not be thus particularized, but for a fine
cataract it presents in the glen of Dualt, near Killearn house. In a
deep, wooded ravine, with many smaller falls, the rivulet rushes over a
precipice of 60 feet. In the same neighbourhood, the Carnock has worn a
channel 70 feet deep, through red sandstone. The chasm is called Ashdow,
a corruption of Uisk-dhu, "black water."
The Duchray, which is the southern and
most considerable branch of the Forth, rises near the summit of
Benlomond, and forms the northern boundary, for some miles, of the
parish of Drymen. Leaving it on the south, it joins a tributary from
Loch Ard; and now acquiring the name of Forth, it again approaches and
skirts the same parish as far as its eastern extremity.
The Endrick – derived from Auon,
"river," and eirich, "to rise" – springs
from the Gargunnock hills, north-east of Fintry. It is a bold and rapid
stream, subject to sudden "spates," which frequently do
serious damage. In September, 1836, twenty score of lambs were swept, by
one of its floods, from the lawn of Buchanan into Loch Lomond. After
running a short distance east at the start, it takes a southerly course;
and, gaining strength by the accession of tributary waters, it separates
the parishes of Gargunnock and St. Ninians from that of Fintry, till it
reaches the high road leading from the latter village to Denny. It then
flows for about 4 miles due west through the northern valley of Fintry,
when it becomes the boundary betwixt the parishes of Killearn and
Balfron. The Endrick comes down with a deafening noise over its rocky
channel; and in the "Loup of Fintry," pours its waters over a
rock, nearly perpendicular, of about 60 feet. When the river is much
swollen, nothing can exceed the grandeur of this scene. In its usual
state there are three breaks in the fall; but, in a flood, the waters
dash over the precipitous rock, which is upwards of 90 feet wide, in one
unbroken cataract. The stream cannot be supposed to contain a great
quantity of water. Yet it is the sole moving power of a considerable
weight of machinery in Fintry parish. A reservoir of good depth,
covering about 30 acres of land, was constructed on the high ground, and
supplied wholly by the Endrick, for driving the Culcreuch cotton
factory. At Gartness, there are also cascades of some character. For a
quarter of a mile, the channel of the stream is here scooped out of the
solid rock, and the vexed waters have to force their way over a series
of precipices. In greater part, at least, the Endrick is a clear-running
and beautifully-wooded stream, by which anglers can sport, and get
rewarded with full baskets of deliciously flavoured trout. After a
course of 18 miles, it discharges itself into Loch Lomond, being the
largest river which that lake receives.
The Forth, as we have already said,
traverses Stirlingshire for 10 miles from its source, under the name of
Duchray, or Glenguoi. Augmented as it proceeds, by numberless mountain
streams, it then enters Perthshire, where it receives an accession equal
to the volume of its own waters, in the river which issues from Loch Ard
in Aberfoyle. It is now called Avondow, or "black river,"
being generally dark and muddy here from the quantity of moss that is
floated in it. After a course of about 5 miles, it again joins
Stirlingshire below Gartmore house, where it gets the name of Forth,
which it retains. By several of the earlier writers, it has been
confounded with a much nobler river, the Teath, that flows from the
Callander district as a tributary stream, and which is nominally merged
about 2 miles above Stirling. Even Mr. Nimmo, living near the eastern
extremity of the county he described, fell into this error. Sir William
Alexander, first Earl of Stirling, was correct, however, when in his Paraenesis,
or Exhortation to Government, addressed to Prince Henry, he says: -
"Forth, when she
first doth from Benlowmond rinne,
Is poore of waters, naked of renowne;
But Carron, Allan, Teath, and Devon in,
Doth grow the greater still the further downe;
Till that abounding both in power and fame,
She long doth strive to give the sea her name."
The Romans, adopting the words of the
natives, and fitting them to their own pronunciation, called this river
"Bodotria." But what was Bodotria? Probably the Celts, in
comparing the much finer stream, the Teath, with the sluggish,
moss-banked river which the Forth exhibits from Gartmore to Frew, called
the latter Boa-shruth, "insignificant stream," or Bath-shruth,
"smooth slow stream." Still, how it came to be named Forth? Phorth,
pronounced with the aspirates quiescent, becomes Port; and changing the
Ph into F, we have Forth – a name applicable to a river affording the
means of navigation. In point of magnitude, the Forth, as a Scottish
river, is only surpassed by the Spey and Tay. The surface which it
drains is estimated at 541 square miles. Steamers ply regularly between
Granton and the port of Stirling. At neap tides the flow is about 5 1/2
feet in the harbour, at stream tides it rises to 11 feet. At one time,
the navigation between this and Alloa – a distance of 10 1/2 miles,
though the direct line is only 5 – was greatly impeded by seven fords,
or shallows, composed of boulders. But is was determined to have two of
these at least removed – the town and abbey fords, which were found
the greatest obstructions to the free passage of vessels. The works were
commenced at the lower end of the abbey ford, where the channel
excavated was about 500 yards in length and 75 in breadth; while it was
also deepened in some places 3 1/2 feet. Here is a specimen of the
wisdom of our ancestors under similar circumstances: - During the reign
of Charles II. of Spain, a company of Dutch contractors offered to
render the Mancanares navigable from Madrid to where it falls into the
Tagus, and the latter from that point to Lisbon, provided they were
allowed to levy a duty for a certain number of years on the goods
conveyed by this channel. The Council of Castile took the proposal into
their serious consideration, and after maturely weighing it, pronounced
the following singular decision: - "That if it had pleased God that
these two rivers should have been navigable, He would not have wanted
human assistance to have made them such; but, as He had not done it, it
was plain He did not think it proper that it should be done. To attempt
it, therefore, would be to violate the decree of His providence, and to
mend the imperfections which He designedly left in His works."
Though the Forth is far from being the most sediment-carrying river in
Scotland – the Tay surpassing it in this respect many times over –
it has been calculated to bring down more than 5,000,000 cubic feet of
sediment per annum; and it is probable that, at one time, when the ice
and snow fields were melting from off the country, and the glacial
debris lay more abundantly on the higher grounds, it brought down much
more. Thus was the "fine land" accumulated in the gradually-shallowing
waters of the ancient firth. Before any written human history, but not
before the human occupation of the island, the land received its most
recent elevation of from 30 to 50 feet, and the river then began its
slow and winding course over the level tract which it had itself laid
down to the now more distant sea. Such, briefly, is the history of the
"Bonnie Links o’ Forth." In this river there are, besides
the regular flows and ebbs, several irregular motions which, betwixt
Alloa and Culross, are commonly called the Leakies. When the tide
flows some time, it intermits and ebbs for a while, and then fills till
full sea; and, on the contrary, when the tide is ebbing, it intermits
and flows for a period, and, afterwards, ebbs till low water. This
extraordinary phenomenon is called the Lakies of Forth. A large
salmon fishery is still carried on at Stirling, chiefly for exportation.
The burgh revenue derived from this source, even in 1816, was 1,200
pounds sterling; but a privilege of the inhabitants to have the fish at
3d. a pound has been, for many years, abolished. Salmon seems to have
been a staple article of diet in Lent during the reign of James IV. His
Majesty used, especially during this season, to become Franciscan monk
here, where he had founded a convent in 1494. The poet Dunbar, to whom
it had been recommended, probably by high authority, to be a friar of
the king’s favourite order; but who, not relishing the proposal,
endeavours, in what he calls "Dirigie to the king, bydand our lang
in Stirling," to prevail on his Majesty to
"Cum hame and dwell
nae mair in Stirling,
Quhair fisch to sell at nane but
spirrling.
Credo gustare statim vinum
Edinburgi."
The smelt, or sparling, was wont to be
caught here in great numbers during the spring months. A specimen of the
Beluga, or White Whale, was also killed near the town in 1815.
The Garrel, as its name denotes, is a
rough, brawling stream. But why blame the poor brook for outrageous
behavior? Similarly situated – a water-child of the mountains with
strength to be wild, and a rough road to travel – no stream could
conduct itself more circumspectly. To be what it is, and to be capable
of what it is capable of becoming, is the true end of even a river’s
existence. The Garrel rises on one of the Kilsyth range of hills; and,
within a mile and a half, falls 1,000 feet, having numerous cataracts in
its course. The narrow chasms worn by its rapid and powerful current in
winter, are singularly romantic. When it reaches the Burn Green, near
the town of Kilsyth, it is joined and augmented by the little Ebroch,
which springs from the foot of the Barwood. After flowing half-a-mile
further, in the valley westward, it loses itself in the Kelvin at the
end of a course of about three miles.
The Glazert, which runs through a
considerable part of the parish of Campsie, empties itself into the
Kelvin, opposite the town of Kirkintilloch. It is formed by the junction
of three burns, near the lodge at the entrance to Lennox castle – the
Pu’, a small, sleepy streamlet which skirts the base of the South
Brae; the Finglen burn, which crosses the valley at the west end of
Haughead; and the Kirkton burn, which crosses at the eastern extremity
of the same village. No less than nineteen burns are said to discharge
themselves into the humble Glazert.
The Kelvin has its source, in a sort of
marsh, on the lands of Ruchill; and descends, as a petty rill, to the
low ground on the south, where it soon receives an accession from a
portion of Shawend burn, and further west from the Garrel. It moves
slowly forward; but near Inchterff, and near Inchbelly, it becomes a
beautiful stream with banks verdant and wooded. Until the year 1792, it
was much choked up with flags, rushes, and water-lilies, and frequently
overflowed the adjacent valley. But Sir Archibald Edmonstone, Bart., of
Duntreath, who purchased the estate of Kilsyth in 1784, projected and
carried into effect a great improvement, under the inspection and
according to the plan of Mr. Robert Whitworth, engineer, by
straightening, deepening, and embanking the river. In its route to the
Clyde, the Kelvin passes many sweet bits of scenery; but having left the
wooded bend, near the old "Three-tree well," its waters, from
industrial pollution, become sickening even to look at, and detract
greatly from the healthful amenities of that attractive breathing ground
– the West-End Park, so much and so wisely appreciated by the citizens
of Glasgow.
The county is not peculiarly rich in its
lochs. Several of the islands, however, in Loch Lomond belong to the
parish of Buchanan. Inchcaileoch, "old woman’s island," once
contained a nunnery, and the parish church; but is now without either
house or inhabitant, and stands covered with copsewood. Inchfad,
"long island"; and Inchcruin, "round island," are
arable and inhabited. Inchmurrin, the island of St. Murrin, who was
tutelary saint of Paisley, is the largest of the whole, being two miles
long and one broad, and remains preserved for fallow deer. Lomond, a
corruption of the Gaelic Lomnochd, is literally "naked," a
character which cannot apply to the thickly wooded shoulder of the
kingly "Ben" on the west. Metaphorically, it signifies
"insulated." A pronunciation of the name nearly approaching
the Gaelic occurs in a notice of a charter in David II.’s time by
Donald Earl of Levenax to Maurice of Bouchcannane, of various lands,
and, amongst others, "illam terram de Sallachy per has similiter
divisas, a Sallachy usque Kelg, et sicut descendit in stagno de
Lougchlomneid." If there be any force in these remarks, they go
to show that the loch is named from its mountain. According to Richard
of Cirencester, it was anciently called Lyncalidor, and certainly
it did not receive its present appellation till the fourteenth century.
Few there must be who have not heard of its three wonders, "waves
without wind, fish without fin, and a floating island." The swell
in the widest part, more particularly after a storm, has originated the
first. Vipers are said to swim from island to island, and may account
for the second. As for a "floating island," such a phenomenon
has been heard of elsewhere. Pliny tells us that certain green lands,
covered with rushes, float up and down in the lake of Vandimon.
There is in MacFarlan of MacFarlan’s
papers, now deposited in Advocate’s Library, a curious passage,
written in 1724, by Alexander Graham, Esq. of Duchray, in his account of
several parishes, and, amongst others, that of Buchanan. "On the
north side of Loch Lomond, and about three miles west from the church,
upon a point of land which runs into the loch, called Cashel, are the
ruins of an old building of a circular shape, and in circumference about
60 paces, built all of prodigious whinstone, without lime or cement. The
walls are in some places about 9 or 10 feet high, yet standing; and it
is surprising how such big stones could be reared up by the hands of
men. This is called the Giant’s castle, and the founder thereof said
to be Keith MacInDoill, or Keith the son of Doillus, who is reported to
have been contemporary with the famous Finmacoill, and consequently to
have lived in the fifth century. This Keith, notwithstanding the great
number of natural isles in the loch, was, it seems, so curious as to
form an artificial island, which is in the loch at a little distance
from the point on which the old castle stands, founded on large square
joists of oak, firmly mortised in one another; two of which, of a
prodigious size (in each of which there are three large mortices), were
disjoined from the float in 1714, and made use of by a gentleman in that
country who was then building a house." The point on which the
castle stands is called at this day Rownafean, i.e. "giant’s
point." No doubt the buoyancy of an island, in some places, may be
ascribed to an accumulated mass of decaying vegetable matter, by which
it is surrounded; but, in our opinion, the decrease of the waters of
Loch Lomond, at certain particular seasons, affords a simple solution of
the anomaly of its so-called "floating island." The length of
this queen of Scottish lakes is 24 miles; its greatest breadth which is
nearly opposite Rossdhu, about 8 miles; and its average height above the
sea level 22 feet. From lower Inveruglass up to near its northern point,
it is of considerable depth. Opposite Farkin, it is 66 fathoms; a little
farther north, 80 fathoms; a mile south of Tarbert, 86 fathoms; and
opposite Alt Gary, 100 fathoms, which probably is its greatest depth.
South from Luss it seldom reaches 20 fathoms. The chief tributary rivers
of the loch are the Endrick on the east, and the Fruin on the west. Its
outlet is the river Leven, at Balloch, which, after a course of 5 miles,
flows into the Clyde at Dumbarton. In wet seasons, the surface of the
lake sometimes rises 6 feet, when much valuable land at the mouth of the
Endrick is heavily flooded. In 1782, a late harvest being followed by an
early and severe winter, the corn, before it was ripe, was covered with
water, and afterwards enveloped in ice. The upper part of the loch, from
its great depth, never freezes; but the lower part occasionally bears
ice of sufficient strength for the enjoyment of exhilarating exercise
and art and skating. In the beginning of 1838, it was traversed to and
from Inchmurrin by horses and vehicles. Its scenery is well known, and
has frequently been described both by practical and poetic pens. We
touch it not; but leave it with silent admiration. Singularly bold and
beautiful, it is, in its aggregation of exquisite forms, unsurpassed by
any British lake.
The other lochs which have a place in
Stirlingshire need only be summarized. Contiguous to Carron iron-works,
there are two reservoirs supplied from the Carron at Larbert, by means
of a convex dyke. The wester-dam, which covers 30 acres, is somewhat
picturesque, with trees skirting its edge, and a fleet of swans sailing
with proudly-arched neck over its surface. But at times we have seen
some memorable night effects at the forge dam, into which the belching
furnace flames are brightly reflected. More vividly seen in the water
than in the air, they seem to dart downwards into a dark abyss,
illumining the whole surface of the dam and the row of outlying cottages
with all but lime-light brilliance.
At the southern part of Killearn parish,
lies an artificial lake, covering about 150 acres, which serves as a
reservoir for the supply of water during summer to the Partick mills on
the Kelvin. The sources of that river, as many are aware, were taken to
form the high summit reservoir of the Forth and Clyde Canal. The latter
was called the Townhead Loch, and is situated near Kilsyth. It is of an
oval form, full three-quarters of a mile long, and from one-quarter to
half-a-mile broad. It covers 75 imperial acres.
On the moor of Kippen, there is a small
lake of water, called Lochleggan, about a mile in circumference, and for
the most part surrounded with wood. A considerable stream issues from
it; which, increasing as it flows, forms the burn of Broich, whose
waters, after passing through a beautiful glen close by the house of
Brioch, are chiefly employed in floating moss from the plain below.
There are two lochs in Slamannan parish
– the Little and the Great Black Lochs. The latter is the principal
feeder of the reservoir constructed on the lands of Auchingray for
supplying the Monkland Canal. Another, called Ellaig Loch, is situated
to the north-east of the annexation. Perch and eel are plentiful in all
three.
Loch Coulter lies in St. Ninians parish.
It is about 2 miles in circumference, shallow to the west, but very deep
to the north-east. In 1755, the great earthquake, by which Lisbon was
destroyed, greatly agitated this lakelet, and it was then, as is
supposed, that a large stone, in weight about a ton, was raised from its
bed and carried towards shore. The shock was particularly severe around
Drymen. On that day, Whitefield, the great English divine, was preaching
in the adjoining parish of Kilmaronock. The weather was fine, and a
large concourse of people assembled to hear the noted southern preacher.
The speaker and his hearers occupied the face of an eminence. Instantly
the earth heaved, and the people were bent forward as if by a wave.
Strathblane parish contains six lakes;
Loch Ardinning, of 60 imperial acres; Craigmaddie and Dunbroch, of 10
each; Carbet of 8; and Craigallion, of 40 acres. These lie in romantic
situations; and with the exception of the first mentioned, are adorned
partly with natural wood, and partly with plantations. Mugdock Loch,
containing 25 acres, is also ornamented with trees, and is further
enhanced by the ruins of the ancient castle which stand on its
south-west point.
Milngavie has an irregular and somewhat
straggling appearance. In and around the village, on the banks of the
Allander, are a number of public works, the most extensive of which are
the calico printing and cotton spinning establishments of Messrs. John
Black & Company. About a mile north from the railway station there
is also the Mugdock reservoir, which is supplied with water from Loch
Katrine for the service of the citizens of Glasgow. It is formed in a
natural valley, by an embankment on the south side 400 yards long, and
68 feet high; and by another on the east side 240 yards long, and 50
feet high; each with a puddle wall in the center, and stone pitching 2
feet thick on the front, which is formed to a slope of 3 horizontal to 1
vertical, and covered with soil on the back, which has a slope of 3
horizontal to 1 vertical. The water surface of the reservoir extends to
60 acres, and a small detached portion at the upper end to 2 acres more;
the depth is 50 feet, and it contains 548,000,000 gallons, or a supply
for the city, at the present rate of consumption, for eighteen days. The
water is drawn from the reservoir by pipes laid in a tunnel through the
rock which forms the hill-side, there being no pipes through the
embankments themselves. These pipes lead into a well, also cut out of
the solid rock, 40 feet diameter and 63 feet deep, at the bottom of
which are placed the various valves by which the flow of the water is
regulated. At the reservoir end of the tunnel, a cast-iron stand-pipe is
erected, with sluices to draw off the water; and in the well the water
is strained by passing it through copper wire-cloth, fixed in frames of
wood, so as to form an inner well of octagonal shape, 25 feet diameter;
and from this latter the water finally passes into the mains leading to
the city. This work may truly be said to surpass the greatest of the
nine famous aqueducts which fed the city of Rome. Of the 26 miles which
lie between Loch Katrine and the Mugdock reservoir, 13 miles are
tunneling, 3 3/4 miles are iron-piping, and the remainder, where the
ground has been cut open, is an arched aqueduct. There are in the whole
work, 70 distinct tunnels, upon which 44 vertical shafts were sunk for
facilitating and expediting the completing of the scheme. In addition to
the tunnel at the commencement of the aqueduct at Loch Katrine, and the
one at its termination, there are at intermediate places, others of 700,
800, 1,100, and 1,400 yards in length. Not to speak of smaller
constructions, there are 26 important iron and masonry aqueducts over
rivers and ravines, some 60 feet and 80 feet in height, with arches 30
feet, 50 feet, and 90 feet in span. The number of people employed in
constructing the works, exclusive of iron-founders and mechanics, was
generally about 3,000; and for the greater part of these, huts and
roads, and all other accommodation had to be provided; the country in
many districts being of the wildest and most inaccessible character. The
works were designed in 1853-4; completed at a total cost of 1,987,548
pounds, in 1859; and opened by Her Majesty the Queen on 14th
October of the latter year. |