SANQUHAR is situated on the left bank of the Nith,
twenty-six miles north-west of Dumfries. The Parish is eighteen
miles in length, by five miles in breadth, and embraces an area of
above sixty-one square miles. The Nith, which takes its rise in
Ayrshire, a few miles above New Cumnock, passes into Dumfriesshire
at a point eight miles north-west of Sanquhar, by an opening in the
chain of hills which skirts the northern boundary of the county, and
terminates in Corsancone, the hills on the west side of the valley
being linked with the great Galloway range. Having traversed the
parish of Kirkconnel for a distance of seven miles, the river enters
the parish of Sanquhar at the point where it is joined by Crawick.
This stream forms the boundary between the two parishes on the east
side of the valley, while on the west they are divided by Kello,
which flows into Nith two miles higher. On the right bank the ground
rises gradually to a range of hills which runs parallel to the
course of the river. These hills are very uniform in height, and are
smooth and green to their summits. They contain two principal
eminences, the Black Lorg, 2890, and Cairnkinnow, 1813 feet in
height. At the back of the range, and overlooking Scaur, is the
tremendous precipice of Glenwhargen, rising almost perpendicularly
to the height of about 1000 feet. The Black Lorg stands at the
north-west corner of the county. Forming, as it does, the water-shed
of this region, the sources of several streams are to be found here,
giving rise to the rhyme—
“Euehan, Scaur, Kello, and Ken
A’ rise oot o’ ae wee hill-en’.”
Kello, as has been said, forms the boundary between
Sanquhar and Kirkconnel, while Euehan, taking a more southerly
course, drains the west side of Sanquhar parish, and falls into Nith
just opposite the town. Near the head of Euehan there is on the
summit of the hill above Glenglass, Polvaird Loch, a sheet of water
a little over three acres in extent, and unique both in its
situation and appearance. It is situated on the top of a hill 1800
feet above sea-level. It is in shape a parallelogram, not quite
rectangular, two of the opposite corners being drawn out on the line
of the diagonal. Its sides are so regular as to give the impression
of its having been the work of man, but it is one of the
mountain-tarns, which are so common a feature of Scottish scenery.
This loch has no surface feeder except the rainfall which may find
its way into the little basin in which it lies. It is, however,
undoubtedly fed by springs, as is evidenced by the fact that,
notwithstanding its great elevation, it is never quite frozen over
even in the severest winter. Nor had it any natural overflow except
what trickled through some marshy ground on the north-west side into
the head of Polvaird Burn, which flows down to Euehan, till some
years ago a ditch was dug connecting it with the burn, whereby its
depth was reduced and its area somewhat restricted. This was done by
the then tenant of the farm of Barr, on which the loch lies, on
account of his having suffered the loss of a sheep by drowning in
its waters. Polvaird contains very few fish. Efforts have been made
from time to time to stock it with trout, a number having been
transferred from the neighbouring Euchan, but they do not appear to
thrive ; at all events, the angler’s art is plied with scant
success. There are several rude curling-stones, with primitive
handles, lying on its banks; and to prevent the credulous antiquary
of a future time from constructing some wonderful theory on the
existence of these stones, it may be explained that they were
carried up by the family of one of the shepherds on Euchan water, in
order that they might have the opportunity of enjoying Scotland’s
“roaring game” in the only possible place in this region.
Towards the end of last century, this country-side
was robbed of much of its natural beauty by the despicable policy of
the last Duke of Queensberry. He had no issue, and, it is supposed,
to spite the collateral branch of the family who were to succeed
him, doomed to destruction the woods on the estate. It does seem
that the Duke had been animated by some such malicious, spiteful
motive, for had the raising of money merely been his object, he
would have confined the fell work of destruction to the enclosed
woods and plantations, which were of some commercial value, whereas
we find that not even the bonnie glens were spared, but that they
were robbed of their adornment of natural wood. It was at this time
that one of the sides of the Euchan was cleared, but, fortunately,
the other had not been overtaken when the old Duke’s death occurred,
and then the work was promptly put an end to. The following verses
were found written on a window-shutter of a small inn on the banks
of the Nith soon after this district, one of the finest in the south
of Scotland, had been thus disfigured to gratify an unworthy
passion. It is not unlikely that they were written, as has been
supposed, by Burns, as he was given to scribbling down his effusions
in such places :—
“As on the banks of wandering Nith
Ae smiling morn I strayed,
And traced its bonnie howes and haughs,
Where linties sang and lambkins played,
I sat me down upon a craig,
And drank my fill o’ fancy’s dream,
When, from the eddying pool below,
Up rose the genius of the stream.
Dark, like the frowning rock, his brow,
'And troubled, like his wintry wave,
And deep, as sighs the boding wind
Among his caves, the sighs he gave:
‘And cam’ ye here, my son,’ he cried,
‘To wander in my birken shade?
To muse some favourite Scottish theme,
Or sing some favourite Scottish maid?
There was a time, it’s nae lang syue,
Ye might hae seen me in my pride;
When a’ my weel-clad banks could see
Their woody pictures in my tide;
When hanging beech and spreading elms
Shaded my streams sae clear and cool,
And stately oaks their twisted arms
Threw broad and dark across the pool.
When, glittering through the trees, appeared
The wee white cot aboon the mill,
And peaceful rose its ingle reek
That slowly curling clamb the hill.
But now the cot is bare and cauld,
It’s branchy shelter’s lost and gane,
And scarce a stinted birch is left
To shiver in the blast its lane. ’
‘Alas,’ said I, ‘what wofu’ chance
Has tyned ye o’ your stately trees?
Has laid your rocky bosom bare?
Has stripped the cleading aff your braes?
Was it the bitter eastern blast
That scatters blight in early spring?
Or was’t the wil’ fire scorched their boughs,
Or canker-worm wi’ secret sting?’
‘Nae eastern blast,’ the sprite replied;
It blaws nae here sae fierce and fell;
And on my dry and halesome banks
Nae canker-worms get leave to dwell.
Man! cruel Man!’ the genius sighed,
As through the cliffs he sank him down,
The worm that gnawed my bonnie trees—
That reptile wears a Ducal Crown.’”
In spite, however, of the extent to which Euchan was
thus disrobed of much of its beauty, it is a bonnie glen. A good
road runs along almost its entire length, and no pleasanter walk on
a summer day could be desired. It is necessary to offer a word of
caution to visitors by informing them that this glen is infested
with adders. These snakes are frequently to be seen basking
themselves on the sunny brae which forms the left bank of the
stream. They measure about 18 inches and even more in length. The
careless walker might readily step on one of them, for in parts the
ground is covered with deep heather, but this would be a case of
“caught napping,” for the adder at the sound of human footstep
glides rapidly out of sight. He will not stand his ground, far less
offer attack, unless he be come upon unexpectedly and find his
retreat cut off. But the danger is more imaginary than real, for
there is no record of any accident through adder-bite there. There
is excellent trout fishing in the tributaries of the Nith, and
particularly in Euchan. During last year, up to the month of June,
one angler alone caught over one hundred dozen of fair size, all the
smaller being returned to the water. There is nothing particularly
noteworthy about the hills in the upper part of Euchan glen, unless
it be what is known as the Banyan Crag, a little above the Bank
dyke. This Crag presents a bold, precipitous front several hundred
feet in height. While the water of Crawick and Mennock is remarkably
clear and limpid, Euchan, particularly when it is in flood, pours
down a volume of water embrowned with peat, which forms dark,
mysterious pools, and shews a fine rich colour where it tosses
impetuously over its rocky bed. For two miles above its outlet the
course of this stream is most picturesque. Ceasing at the farm-house
of Old Barr to flow, as it has done from its source, in the open, it
enters between walls of rock, through which it has, in the course of
ages, worn a deep channel, washing the whinstone perfectly smooth,
and into the most fantastic shapes. One cascade after another, with
dark, deep narrow pools between, forms a most striking and charming
picture. When in flood the Euchan here roars and thunders like a
miniature Niagara, and a peep of the “Deil’s Dungeon”—for so this
part is named—can only be obtained from one point or another of the
overhanging crag ; but on a summer day, when the volume of water is
small in comparison, a splendid view of the “ Dungeon ” can be
obtained by descending to the bed of the stream by a steep narrow
path at the point where that dark gruesome gullet ceases. Here the
stream parts into two, leaving a spacious level rock in the centre
quite dry. This rock can be easily enough reached from either side
by-creeping along the bank till where the parted stream is at the
narrowest, and a short step lands one safely. It is well worth the
trouble of the descent. The rocks rise up in huge masses on either
side, and are crowned with trees, which swing their arms over the
overhanging ledge. Looking up, one sees the water sweep round a
bend, which forms the limit of the view, turning the whole into a
sort of chamber. It tumbles over a large rock, which still obstructs
its progress, and then sweeps down as if it would carry one away,
but presently, being no longer fretted by any barrier, it finds
ample room for itself in a dark pool, and then parting, it glides
swiftly and silently past in two black narrow channels. But for the
difficulty of access this would form an admirable place for a
pic-nic.
A little distance below the “Deil’s Dungeon” the
stream again passes through a long channel of rock not more than
three or four feet wide, which bears the name of “The Lover’s Loup.”
The name is probably associated with a long-forgotten tradition; as
it is, the leap across, though not a great one, tries the nerve of
him who performs it, for the water, dark as Erebus and of profound
depth, fascinates the eye, and is apt to render the head giddy.
Immediately under “The Lover’s Loup ” we come to what are known as
the “Drappin’ Linns,” where the freestone first makes its
appearance. These Linns are on the east side of the stream, where
the soft rock towers up to a height of forty feet or so, and
overhangs the river bed in a picturesque manner; the name which it
has received being derived from the water which continually drips
from the roof of this cave-like recess. The footpath up the bank of
the stream runs over the top of the linns on a narrow ledge, and the
trepidation, caused as one passes along this dangerous path at the
sight of the overhanging precipice, would be increased were it
known, as it is not to every one, that the whole mass has such an
apparently slender hold. The course of the water now reveals the
change that has taken place in the rock strata. It runs over beds of
freestone, and traces of the coal measures become discernible. The
rock on the edge of the field is very soft in texture, yielding
readily to the influence of the waters, by which it is worked into
the most curious forms, as, for example, at the “Drappin’ Linns”
above mentioned, and the “Pamphy Linns,” a short distance across the
moor. The Falls of Euchan, a little farther down, present a face of
freestone, fifteen or twenty feet thick; while a short distance down
stream, the rock is found very hard and compact. The colour being a
very light grey, it has been quarried on an extensive scale for
building purposes. From it the material for the new bridge over the
Nith, built in 1855, was obtained. Just opposite Euchan Falls, on
the west side, tradition says there was once a waulk-mill. There are
certainly traces of what appears to have been a mill-race, whereby
the water had been diverted for some industrial purpose. Near the
same place, and on the same bank, are the remains of a cottage or
cottages, probably in connection with the mill. In the glen of
Euehan there are the ruins of quite a number of houses, but this is
an example only of what is to be seen in all directions, and affords
proof of the extent to which depopulation has been carried on in our
country districts. Between the Falls and the quarry stands an object
of antiquarian interest. In the angle formed by the junction of the
Barr Burn with Euchan is a ridge, pretty steep on the Barr Burn
side, and perfectly inaccessible from the Euchan, the rocks rising
there like a wall. A position like this, with exceptional means of
defence of a natural kind, could not escape the eye of the dwellers
of that early time, and so we find that it was once a stronghold
bearing the name of Kemp’s Castle. A more detailed description of
this spot will be found in the chapter on the antiquities of the
district.
On the Barr Burn are the “Pamphy Linns”—curious and
interesting, but not so imposing as the name by which they have been
dignified would lead one to expect. They are, however, well worth a
visit. There being no road up the burn, the visitor must proceed by
the Barr and Barr Moor house. Passing round behind the latter one
must strike straight across the field towards the wood in front,
where a gate in the dyke gives him entrance to the wood, through
which the burn here pursues its course. The Linns are formed by the
action, on the soft freestone, of the two small burns, which at the
foot join to form the Barr Burn, by which it has been carved into
the most grotesque forms. The rock lies near the surface, and the
burn having washed away its slight covering of soil has worn a
channel narrow and ever deepening. Curiously enough, the lower
stratum of rock is much softer than the portion overlying it. Thus
it is, that so soon as the water had worn its way through the upper
stratum, the lower was scooped out on all sides when the burn was in
flood, leaving the harder upper rock overhanging these subterranean
chambers in the most wonderful manner. The rock had originally
stretched across the course of both burns, and each had cut its way
through, leaving the centre part towering up intact between them.
When the wood was enclosed about forty years ago, there was
perpetrated what some will regard as a piece of vandalism, for, with
no regard to the romantic beauty of this secluded spot, the rocks
were torn down and carted away for the construction of the dyke. It
was a wanton act, too, for the same rock lies all round in the
fields quite near to the surface, and it stripped the “Pamphy Linns”
of much of their former glory. We have been thus particular in
giving the approach to these linns because, like many of the natural
beauties to be met with in moorland districts, they might, being all
under the level of the ground, be passed unobserved by any one not
acquainted with their locality. The same natural operation is to be
seen on a larger scale at Crichope Linns, near Thornhill, where the
rock, being of the same description, like results have been produced
by the water’s influence.
Not a hundred yards from the foot of the road which
leads to Euchan quarry, and which thereafter continues up the side
of the stream as a footpath, there issues from the face of the rocky
bank a spring known as Euchan Well, or Baird’s Well—Baird, who
resided in the little cottage at the opening of the road, being a
“character” in his way. That the spring has a deep source is evident
from the fact that the quantity of water issuing from it is not
affected by the rainfall, nor is its temperature by the season, the
latter quality giving rise to the popular notion, which applies to
many deep springs, that it is coldest in summer and wannest in
winter—that being so only in imagination, and caused by the contrast
which its equable temperature presents to the prevailing temperature
of other objects. Some years ago attention was drawn to the
character of this well, which is of the chalybeate class. The
analysis will be found at the end of this chapter. Numbers of people
professed to having found its water to be valuable in its tonic and
other properties. It was opened out, a pipe inserted, by which the
water is now discharged, a drinking cup attached to the rock, and a
gravelled footpath constructed alongside the road leading past it.
Dreams were cherished of the possible revival of the prosperity of
Sanquhar, which was in a sadly reduced state, owing, first, to the
closing of the carpet works at Crawick Mill, and next, to the decay
of the handloom weaving, which was driven to the wall by the
introduction of machinery. It was hoped that, with this medicinal
spring and all the attractions of pure air and charming scenery,
Sanquhar might become a popular health resort, but that hope has not
been realised as yet to any great extent.
There are few districts in Scotland which can be
compared with that of Upper Nithsdale, of which Sanquhar is the
centre, for all that goes to make a desirable summer resort. The
description which is here given of its topographical features will
give the reader an idea, however imperfect, of its wealth of natural
beauty—a beauty which embraces every element of mountain and plain,
hill and dale, forest glade and dark ravine, lonely moor and
cultivated holm-lands, roaring cataract and placid pool, breezy
upland and bosky glen—the whole invested with an historical interest
of no common order. What besides increases the attractions of the
district to the visitor is the almost absolute and unrestrained
freedom to be enjoyed. Notices of “Trespassers will be prosecuted,”
“Keep to the road,” and others of a like nature, by which a selfish
and exclusive landlordism would seek to deprive the general public
of enjoyments which are the heritage of humanity, are nowhere to be
seen. In this respect the Duke of Buccleuch, and, following his
example, the other landed proprietors of the district, have allowed
to all the liberty to roam wheresoever they list. In this and other
respects the family of Buccleuch have, constantly in their-relations
with the public, set an example of unselfishness and kindly feeling,
which were it more widely imitated would go far to soften the
antagonism that has oftentimes been created between class and class
by those petty and irritating restrictions upon the exercise of
privileges which are the source of the purest delight to the people,
and which neither invade the natural rights nor injure the interests
of the possessors of the soil in any conceivable way.
It is evident that considerable changes have occurred
in the course of the River Nith and some of its tributary streams.
Gradual changes are common enough in most river courses, and are
usually caused by the detrition of the banks from the action of the
waters. Within recent times Nith has made serious inroads, for
example, on its right bank just below the Bridge, and opposite the
Washing Green, the river now running much farther south, and in a
deeper channel, than it did within the memory of the present
generation ; but we refer to what must have been a sudden and
complete change of course, the result, probably, of a more than
ordinarily heavy flood. Judging from the configuration and the
constitution of the soil, which is very gravelly, Crawick, when it
had reached the open valley, instead of pursuing a straight westerly
course till it was received into the bosom of the larger stream,
must at one time have swept round in a more southerly direction,
skirting the base of the plateau which is here formed, and on which
the Manse stands, and have joined Nith about the farmhouse of
Blackaddie, if not farther down. Then, with regard to Nith itself,
we conclude on similar grounds that its course opposite Sanquhar has
undergone a material alteration. On the left bank, from where the
Old Bridge crossed the river at the foot of the Washing Green to the
King’s Scaur, a distance of a mile, the ground rises quite
precipitously to a height of 100 feet. This line of cliffs is known
as the Brae-heads, and there can be little doubt that at one time
Nith flowed close to their base all the way. The line takes a
somewhat sharp bend at a certain point, and here it is that the
river, swollen to an unusual height, had burst its southern bank,
and pursued its headlong career through the alluvial plain. It was
speedily checked, however, in its wayward course, for the cliff at
the Mains Pool stood in its way. There it was compelled to turn
again towards the east, and after a graceful curve and sweep round
the Mains Holm, it regained its ancient course at the Kings Scaur.
It is on the edge of the cliffs above mentioned that the Castle of
Sanquhar stands. The ancient strongholds which are scattered all
over the country are generally found built on positions of natural
.strength, presenting as great difficulty of attack as possible. The
position of Sanquhar Castle on this, the south-west side was thus
well protected, and with the river running at the base of the cliff
it would be practically unassailable. Proceeding southwards, the
valley contracts, the hills rising abruptly on both sides from the
river, which now loses its general character of a broad,
smooth-flowing stream, and is confined within a narrow rocky
channel, its course for several miles being marked by a succession
of rushing rapids and long, deep, dark pools. Its banks are here in
many parts densely wooded, and without doubt this is the most
picturesque part of the whole of Nithsdale. Indeed, the road from
Sanquhar to Thornhill, which runs close to the river the greater
part of the way, is one of the most charming walks or drives in the
whole South of Scotland. A grand and most commanding view of this
part of the valley can be obtained from the railway, which is cut
out of the hill-side high above the bed of the river, and travellers
whose attention may be drawn to it at the proper moment are
enthusiastic in their praise of the charming combination of woodland
and stream. In leafy June the trees overhanging its banks—oak,
birch, and hazel, with many a bush and shrub between—spread a mantle
of green so thick as almost to entirely screen the river from view,
as it tosses and foams down its rocky channel or glides slowly along
smooth deep reaches; but in October the scene has a fresh charm, for
the trees put on their autumn tints, and the eye is delighted with
the glory of the woods with all their endless variety of brown and
red. Nowhere is this aspect of nature to be witnessed in greater
perfection than on the finely-wooded estate of Eliock, which, in
addition to its plantations of larch and spruce, possesses a fair
stock of natural woods. The first notable specimens are a pair of
Scotch firs growing at the road-side close to the Lodge, which
measure nine feet round the base. These are typical specimens of the
Scotch fir, being straight and clean for fifty feet from the ground,
and surmounted by a shaggy head of dark green branches. Close to
them stands a fine example of spruce, of the same girth, and 100
feet in height. A still better grown specimen, of the same height,
but measuring twelve feet, stands majestically in front of Eliock
House, while another, even more stoutly built, tapes 172 inches
round the butt. A splendid ash adorns the avenue, whose
wide-spreading branches cover a circle seventy feet in diameter,
while a beech is not far distant under whose umbrageous shade a very
large party might find shelter from a noon-day sun, the area
embraced being 240 feet in circumference. The outlook from the
house, of noble trees of this description, has a singular grace lent
to it by the magnificent specimens of weeping birch which are
scattered over the policies. Individual trees of this variety are to
be seen nine feet in girth and 80 feet in height. They are built in
elegant and symmetrical fashion, and form a beautiful feature of the
landscape. These birches with their spreading branches, from which
hang pendant long lacelike tendrils, are an engaging sight at any
season, but when covered with hoar-frost glistening in the sunlight
of a winter morning like a thousand diamond points they form a
brilliant spectacle. Perhaps the most notable of all in the whole
woods, however, is a magnificent row of silver firs, seventeen in
number, which stand in line on the top of a slightly raised bank not
far from the house, and flanking the main park. They are, without
exception, grand examples of their kind, averaging 100 feet in
height, and, standing shoulder to shoulder, show an unbroken mass of
foliage from one end to the other. The one which stands at the
eastern flank of the line slightly over-tops its neighbours, and
measures eighteen feet at the ground. What a pity, one feels, that
they had not been planted along the avenue, where a double row would
have given to the approach to the house a dignity and character
which it lacks. Standing where they .do, however, they look stately
and imposing when viewed from a little distance. A little way up the
hill brings us into a part of the wood where oaks grow unusually
straight and clean. One shoots up like an arrow for twenty feet from
the ground, and is fourteen feet in girth. Strange to say, a large
proportion of the finer trees on this estate are planted in
out-of-the-way situations, but a lover of forestry will find himself
delighted with a ramble through the woods.
On the left bank of the river farther down lies dark
Auchensell, the terror of all travellers by road in the olden time,
with which is associated many a story of highway robbery and of
uncanny sights to be there seen in the dark winter nights. These
traditions and superstitions (for the most part they were nothing
more) have given way before the advance of education and
enlightenment ; still his is a stout heart which does not beat
faster as he finds himself plunged in its gloomy depths. On the
slope of the hill near Auchensell stands the ancient Church of
Kirkbride, belonging to the pre-Reformation period. Kirkbride was
long a separate parish. It lay mainly on the east side of the Nith,
between the parishes of Sanquhar and Durisdeer, but there were also
included within its bounds the lands of Craigdar-roch,
Twenty-shilling, Hawcleughside, Rowantreefiat, and Little Mark, all
on the estate of Elioek, on the opposite side of the water. The old
Church is beautifully situated on the western side of the glen of
Enterkin, opposite the farmhouse of Cosh ogle. From the shoulder of
the ridge immediately below the Church, just where the Nith takes a
sharp bend in its course, the most extensive view possible of the
valley is to be obtained. This is the only point, unless one climbs
to a great height, whence Corsancone, at the head of the valley, on
the borders of Ayrshire, and Criffel overlooking the Solway at the
mouth of the river, a stretch of fort}’ miles can be taken in by the
eye. Crossing to the opposite side of the Nith, and looking to the
north-east from the crest of Drumlanrig Ridge, another grand and
most striking view of the ..district is to be had. So abruptly does
the Ridge rise from the water’s edge, and so narrow is the valley,
that one feels as if he might toss a stone across to the other side
of the glen. The lower reaches of the ground are spread out beneath
the feet ; the comfortable farm-houses and cottages with which the
country-side is dotted can be easily picked out, and every little
ravine and bosky dell lies plainly revealed to the eye. Immediately
opposite, the old Kirkbride Kirk stands, as has been said,
pleasantly situated on the green hill-side, its hoary ruins carrying
us back in memory to the Reformation period and the times of the
Covenant. The yawning mouth of Enterkin Pass is dark and gloomy, and
draws the eye upwards to where the mighty Lowthers lift their broad
shoulders to the sky. Eastward, the Durisdeer hills—on the one side
of the Carron soft and green, and on the other black and
frowning—show us in the back-ground the opening of the famous
Dalveen Pass and the Wall path, while to the south the valley of the
Nith is spread out in panoramic beauty, forming a picture that the
eye delights to rest upon. Nowhere in the southern highlands can a
scene be viewed of such an extensive range, and embracing such
contrasts of rugged mountain and gloomy pass, rolling upland and
fruitful field, trickling rivulet and burn, fringed with birch and
hazel, moss and fern, and broad-bosomed river sweeping through rich
woodland and meadow.
On the translation in 1727 of Peter Rae, its last
minister, and a famous man of his time, to Kirkcounel, Kirkbride was
merged by the Lords Commissioners of Teinds in the neighbouring
parishes of Sanquhar and Durisdeer. The Water of Mennock having been
the boundary between Kirkbride and Sanquhar, it was at this time
that Dalpeddar, Glenim, and a small portion of Cosh ogle were added
to the latter parish. The Auld Kirk of St. Bride had long been
regarded by the country folks as a particularly holy spot : the
disjunction of the parish, therefore, caused a considerable feeling
of resentment, and burials were continued in the Kirkyard long after
religious service in the Church had ceased—indeed, burials still
occur, at rare intervals, of people who have long- been connected
with the district, and whose ancestors lie in this “bonnie Kirkyard.”
The ruins of the Kirk continued to be held in great veneration, and
according to the superstitious notions of the age no good could come
to anyone who interfered with the sacred fabric. As an example of
this, it was firmly believed that the untimely death of the
redoubtable Abraham Crichton, Provost of Sanquhar, who fell from his
horse at Dalpeddar and broke his neck, was to be attributed to the
fact that he had impiously threatened to destroy the ancient
edifice, declaring “I’ll sutie ding doon the Whigs’ sanctuary.” For
some time after his burial in Sanquhar Churchyard his troubled
spirit moved abroad, and was a terror to the young girls, at whom it
grinned over the Kirkyard dyke as they passed to the milking of
their cows. At last these cantrips could be no longer endured, and,
after a chain had been fixed over his grave to keep him down, but
without effect, more spiritual means were adopted, and the services
of an eminently godly man, the Rev. Mr Hunter of Penpont, were
invoked. This worthy minister had “personal dealings” with the
ghost. Whether the restless spirit found peace by a full confession
of sins committed while in the body, or whether it was rebuked with
authority and power by this man of God, and commanded to forsake for
ever the realms of the living, and confine itself to its own native
shades, can never be known. No mortal ear listened to the solemn
interview, but the palpitating hearts of the maidens were composed,
and Abraham’s ghost ceased from troubling. For the last twenty years
or so, from time to time, an open-air sermon has been preached at
Kirkbride on the first Sabbath of July, in commemoration of the
Covenanters’ struggle, and with the object of raising funds for the
repair of the Churchyard wall, which was fast becoming dilapidated.
An occasional sermon was preached prior to that period, for Dr (then
Mr) Simpson, of Sanquhar, the historian of the Covenanters, did
preach at the Auld Kirk about sixty years ago. The choice of a
suitable text caused the preacher much concern, and during a walk
with Dr Purdie, with whom, being still unmarried, he then lodged, he
said that he had searched diligently, but could not fix upon one
that satisfied him. "Aye, man, Robert,’' answered the Doctor,
“there’s surely no mickle in yer heid. What do you think of this for
your text, “Our fathers worshipped in this mountain" “Oh, man,”
replied the minister, “that’s the very thing, Doctor;” and upon
these suggestive words he, when the day came, preached what was then
described as a grand sermon, and which was held in remembrance in
the countryside for many a day.
The Pass of Enterkin, which here runs into the Nith
valley, with its wildness and solitude, was visited by Dr John
Brown, of Edinburgh, the author of “Rab and His Friends,” who wrote
the following description of it. It will be well, however, to
explain that Dr Brown descended the glen— contrary to the usual
practice, which is to ascend—lest any visitor should, after reading
the description, experience the same perplexity that befel a
traveller, who ascended, in identifying its features as therein
given. He was about to conclude that the paper more correctly
represented the fertile imagination of the writer than the actual
facts, when the thought flashed upon him that he might be traversing
the scene in the opposite direction to that followed by the learned
doctor. Having reached the top, he retraced his steps, and then all
was plain and intelligible :—
“We are now nearing the famous Enterkin Pass; a few
steps and you are on its edge, looking down giddy and amazed into
its sudden and immense depths. We have seen many of our most
remarkable glens and mountain gorges—Gleneroe and Glencoe—Glen
Nevis, the noblest of them all—the Sma’ Glen, Wordsworth’s Glen
Almain (Glenalmond), where Ossian sleeps, the lower part of Glen
Lyon, and many others of all kinds of sublimity and beauty—but we
know nothing more noticeable, more unlike any other place, more
impressive than this short, deep, narrow, and sudden glen. There is
only room for its own stream at its bottom, and the sides rise in
one smooth and all but perpendicular ascent to the height, on the
left, of 1895, Thirstane Hill, and on the right of 1875, the
exquisitely moulded Stey Gail or Steep Gable—so steep that it is no
easy matter keeping your feet, and if you slip you might just as
well go over a bona-fide mural precipice. This sense of personal
fear has a fairly idealistic effect upon the mind, makes it
impressionable and soft, and greatly promotes the after enjoyment of
the visit. The aforesaid Stey Gail makes one dizzy to look at
it—such an expanse of sheer descent. If a sheep dies when on its
side, it never lies still, but tumbles down into the burn ; and when
we were told that Grierson of Lag once rode at full gallop along its
slope after a fox, one feels it necessary to believe that either he
or his horse were of Satanic lineage. No canny man or horse could do
this and live.
“After our first surprise, we were greatly struck
with the likeness of the place to a picture of it by Mr Harvey,
exhibited in our Academy in 1846, and now in Mr Campbell of
Blythswood’s collection. This was one of this great painter’s first
landscapes, and gives the spirit, the idea of the place with
wonderful truth and beauty—its solemnity and loneliness, its still
power, its gentle gloom, its depth and height, its unity, its sacred
peace.
‘It is not quiet, is not ease,
But something deeper far than these;
The separation that is here
Is of the grave; and of austere
Yet happy feeling of the dead.’
We have heard that the artist, who sat alone for
hours sketching, got so eerie, so overpowered with the loneliness
and silence that he relieved himself from time to time by loud
shouts, and was glad to hear his own voice or anything. It must be a
wonderful place to be alone in on a midsummer’s midnight, or at its
not less bcwitching noon.
‘In such a glen as this, on such a day,
A poet might in solitude recline;
And, while the hours unheeded stole away,
Gather rich fancies in the art divine :
Great thoughts that float through Nature’s silent air,
And fill the soul with hope, and love, and prayer.’ ”
This Enterkin Pass is cut deep into the great range
of mountains which, encircling the northern border of the County of
Dumfries, culminate overhead in the Lowthers, a great and imposing
mass. From the summit of the Lowthers, at a height of 2400 feet, a
view is to be obtained unsurpassed in its range and its diversity of
feature. It comprehends the greater part of the southern counties of
Scotland. The valleys of the Nith and the Annan lie under the fe£t,
spread out in all their expanse of cultivated beauty ; the head
waters of the Tweed and Clyde are seen starting as little trickling
rills on their journey to the sea ; the dark brow of Skiddaw is
visible as he stands head and shoulders above the mighty group by
which he is surrounded, and which do him reverence ; while to the
west the hills of Galloway stretch away like a billowy sea as far as
the eye can reach. . The extensive panorama also includes the Firth
of Clyde and Goatfell, and the mighty Ben Lomond. The view, whether
for extent or magnificence, undoubtedly rivals that to be obtained
from any of the loftiest eminences in the whole kingdom.
In the superstitious times, reaching down to a
comparatively recent period, the right of Christian burial was
denied to suicides, and the corpse was dragged with every
circumstance of ignominy and disgrace to some lonely spot, as if the
poor creature were an outcast from both heaven and earth. For this
purpose the summit of the Lowthers, which, being on the boundaries
of two counties, and also of the lands of three lairds, was regarded
as a sort of “ No man’s land,” was a place chosen for the burial of
suicides. The scene is depicted with graphic power by Dr John Brown
in his interesting paper on “Enterkin ” thus:—
“The bodies were brought from great distances all
round, and, in accordance with the dark superstitions of the time,
the unblest corpse was treated with curious indignity—no dressing
with grave-clothes, no striekhvj of the pitiful limbs—the body was
thrust with the clothes it was found in into a rude box, not even
shaped like a coffin, and hurried away on some old shattered cart or
sledge with ropes for harness. One can imagine the miserable
procession as it. slunk, often during night, through the villages,
and past the farmsteads, every one turning from it as abhorred.
Then, arrived at this high and desolate region, the horse was taken
out, and the weary burden dragged with pain up to its resting place,
carried headforemost as in despite; then a shallow hole dug, and the
long uncouth box pushed in —the cart and harness left to rot as
accursed. The white human bones may sometimes be seen among the
thick, short grass; and one that was there more than fifty years ago
remembers, with a shudder still, coming—when crossing that
hill-top—upon a small outstretched hand, as of one crying from the
ground ; this one little hand, with its thin fingers held up to
heaven, as if in agony of supplication or despair. What a sight seen
against the spotless sky, or crossing the disc of the waning moon!”
And what a commentary upon that harsh, stern time. A
very striking example of how, actuated by a supposed religious
feeling, men will be guilty of acts which we now hold to be an
outrage upon natural feeling and a denial of all Christian charity;
for there is little doubt that a false religious sentiment underlay
the harsh and contemptuous treatment to which the corpse of the poor
unfortunate who> bereft of reason, took his life into his own hands,
was subjected. Trained in a hard Calvinistic creed, the men of that
age regarded the taking of one’s own life as an interference with
God’s decree, and, therefore, as one of the most impious acts before
high heaven of which a human being could be guilty. But they must
not be judged too quickly when we consider how short is the time
since an enlightened medical science, with a better understanding of
the philosophy of the human mind, first taught us that these poor
creatures were proper objects, not of hatred and scorn, but of
loving and tender consideration, and to turn our lunatic asylums
from what they had hitherto been, penal settlements, whose miserable
inmates were subjected to cruelties of a fearful kind, into
institutions where they should be regarded with Christian pity and
sympathy, and no effort spared to irradiate their dark and
disordered intellects with light and cheerfulness.
From the summit of the Braeheads, to which reference
has been made, the ground stretches back for the distance of half a
mile, and on this plateau the town of Sanquhar stands. Immediately
behind the town, the ground takes a sudden rise till it reaches a
height of between 700 and 800 feet, .whence it stretches right away
to the base of the mountain range which runs along the northern
boundary of the county.
The tributaries of the Nith on the east side are
Crawick* and Mennock. Mr Glennie, in his “Arthuriana,” which treats
of matters connected with the half-mythical, half-real character,
King Arthur, thinks that there are traces of his presence in this
district. In the “Book of Taliessin” mention is made of Caer Rywe,
probably referring to Crawick, a name formed from Caer Rawick.
Crawick, as has already been said, forms the boundary between the
parishes of Sanquhar and Kirkconnel. It rises among the hills, eight
miles or thereby to the north-east. At first a tiny rivulet, it runs
only a short distance till it assumes the dimensions of /a
considerable stream, by the accession at the same point of two
tributaries—Spango, from the west, and Wanlock from the east. The
rocks in the district watered by Crawick and Mennock are blue
whinstone, and as scarcely any of the surrounding lands are
cultivated, but are chiefly pastoral hills, the water of both is
particularly clear, and where broken and fretted by obstructing rock
is lashed into foam of snowy whiteness. While Crawick itself, in its
upper part, presents no features of any particular interest, the
fall in its course being very gentle and gradual, the glen deserves
more than a passing notice, both for its physical features and on
historical grounds. In descending the glen, the eye is first
arrested by the bold face of Craignorth, a precipitous hill rising
from the bed of the stream to a great height. There is a story
connected with this hill, which, like many another from that period,
makes considerable demands upon one’s credulity. It is alleged that,
on one occasion, when a Covenanter was being hotly pursued by
Olaverhouse, “the bloody Clavers,” as he was accustomed to be called
by the “persecuted flock,” and could find no place of retreat where
he could secrete himself, turned his footsteps towards Craignorth,
and sought to put a stop to the pursuit by picking his way around
the hill face. Claverhouse, who was pressing him hard, never
hesitated for a moment, so the story goes, but rode his horse round
the perilous slope. A dare-devil ride certainly, and requiring more
than human courage, but it is incredible ; only it is just the sort
of performance which is likely to be attributed by the Covenanting
party to one whom they regarded as in league with the Evil One.
The Crawick glen is deep and narrow, as are all the
glens of this district, there being space at the bottom for nothing
but the road and the stream. The hills on either side are of
considerable height, and at various points present to the eye
combinations at once striking and picturesque. A comprehensive view
of the beauties of the glen is to be obtained from the eastern side
of Knockenhair, which is itself one of the most remarkable features
of the locality. It is a conicalshaped hill, the sloping edge of
both sides being of great regularity and terminating in a sharp
peak; which is surmounted by a cairn. It stands alone, too, being
quite detached from any of the hills by which it is surrounded, its
appearance giving the suggestion of volcanic origin. The top of
Knockenhair has always been a favourite site for a bonfire on the
occasion of public rejoicings. The last instance of the kind was on
the coming of age of Lord Eskdaill, son and heir of the then Earl of
Dalkeith and present Duke of Buccleuch, who lost his life not long
after by the accidental discharge of his gun while out deer-stalking
in the Lochiel country. This hill is so situated in the valley that
from its summit a view can be obtained of the entire course of the
Nith through Dumfriesshire, and also, on a favourable day, of the
Cumberland hills on the far side of the Solway, with the waters of
the Firth gleaming in the sunshine between.
On the opposite side of the glen from Knockenhair
stands Carco Hill, one of the loftiest eminences, and of almost
equal height with the Bale Hill, a little farther west. Along the
base of Carco Hill runs the Orchard Burn, where is to be seen an
unique specimen of boulder. It is of enormous size, many tons in
weight, and is a rare specimen of the boulders or rolling-stones,
which are supposed by geologists to have been transported on the ice
during the glacial period, and deposited in out-of-the-way places.
To use a popular Sanquhar phrase, this is an “ in-comer,” not
belonging originally to the locality, but, if its size and situation
be taken into account, it is likely to remain where it is,
undisturbed. From the foot of the Orchard Burn the interest and
beauty of the glen increase, as the stream flows onward and enters
Nithsdale proper. It falls more rapidly as it nears the termination
of its course, the channel becomes exceedingly strait and rocky, and
the banks are adorned with a profusion of natural wood. The natural
beauties of this section have been enhanced, too, by the hand of
man. Here the Duke of Buccleuch has rendered a valuable service to
the public by filling up with plantations the portions which were
bare, thus giving a completeness to the picture. Further, he has
constructed footpaths along both banks of the stream; and bridges at
the top and bottom give the freest access to visitors to view a
scene, romantic and beautiful. For there ‘is no restriction to these
charming walks, known as the "Holm walks,” so called from being in
proximity to the Holm house, which, with its grounds, was originally
a separate estate from the surrounding lands of His Grace, and was
purchased by the Duke from its owner, a Mr Macnab. The lands on the
southern bank, mentioned as having been planted, were held in lease
by Mr Macnab from the Burgh of Sanquhar, and this lease was acquired
at the same time by the Duke.
These Holm walks are justly esteemed the most
charming retreat in a district singularly well-favoured in this
respect. They wind up and down and in and out on the ledge of the
rocky channel, and advantage has been taken of crowning knoll and
shady nook to plant seats, where visitors can rest, and, sheltered
at once from the scorching sun and from every wind that blows, have
eye and ear refreshed with a display of nature’s choicest works. In
this quiet hiding place, it is said, Lord Douglas lay after his
rapid march, with the view of surprising and capturing the Castle of
Sanquhar, ehich was then in the hands of the English. Here he left
his gallant band of followers till a little reconnoitring work was
done, and a plan of attack was resolved upon. A fuller treatment of
this incident is reserved for its proper place.
Descending, the stream makes a sweep round to the
left behind the Holm house, which is pleasantly situated at the head
of a pretty little stretch of holm land, whence probably it derives
its name. The house is shut in from view on all sides by the rising
ground, except in the front, where the outlook is through a narrow
vista away to the sources of Kello and Euchan, on the other side of
the valley of the Nith. Crawick then glides smoothly past the Lawers
Braes, and passing on the left the village of Crawick, with its
woollen factory, corn-mill, and forge, for which it supplies the
motive power, it heads straight for Nith, into which it falls a
little farther down.
Mennock, the other tributary of Nith, on the left
bank, runs almost parallel with Crawick, three miles farther south.
It has a course of about six miles, rising near to Wanlockhead, a
mining village on the very borders of the parish and the county. The
narrow glen through which it finds its way to Nithsdale presents
features of a distinctly different type to those of Crawick. While
the other glens in the district are soft and pleasing to the eye,
the hills being covered with a rich verdure from base to summit, the
mountains, for so they must be called, which tower up on either side
the narrow gorge of Mennock are dark, stern, and rugged, and the
scenery is truly of an impressive grandeur.
About two miles south of Sanquhar, a country road,
leaving the Nithsdale main highway, ascends the Mennock, and
crossing the watershed of the two counties of Dumfries and Lanark,
proceeds by way of Leadhills, whence falling towards the upper
valley of the Clyde, it joins the great road between Carlisle and
Edinburgh and Glasgow at Abington. For some distance the road
pursues a general level, winding round the base of bill after hill,
which slope down to the very bed of the stream, and offer at many
points an apparently insuperable barrier to all further progress. At
one place the attention is arrested by a view probably unequalled in
its unique peculiarity. Four hills, two on each side of the glen,
slope down alternately one behind the other, the outlines of the
pair on each side being almost exactly parallel. When the foot of
Glenclauch Brae is reached, the toilsome ascent begins, and after
the Lang-muir-side—a long level track high above the bed of the
stream—has been traversed, the rise is rapid and continuous, and,
just before Wanlockhead is reached, the road passes through the
“Hass,” which frequently in winter is blocked up with snow. In
truth, so high and wild is this Mennock road that in winter it is no
uncommon occurrence for vehicular traffic to be entirely suspended,
leaving the telegraph as the only mode of communication with the
outer world available to the inhabitants of Wanlockhead. In the
summer season, however, its alpine scenery makes it one of the
finest drives in the district, presenting, as it does, features of
wild grandeur and peculiar configuration of hill not surpassed even
in the western highlands. Some years ago it was visited by one who
had travelled much, and his attention was arrested by the wonderful
resemblance of this road to that leading up to Jerusalem. The same
impression has been made since on the minds of others who had made
the toilsome ascent from Joppa to the Holy City. Wanlockhead comes
into sight quite suddenly and unexpectedly. For miles no human
dwelling has been visible, nor sound heard save the murmur of the
stream, the bleating of the sheep, and the whirr of the grouse or
blackcock as, on strong wing, he sweeps across the glen and drops
out of sight among the deep heather which covers the mountain sides.
The existence of a village in such an out-of-the-world region is due
entirely to the mineral wealth of the surrounding hills, which,
though black and barren on the surface, and sustaining only a few
sheep, contain within their bowels rich deposits of lead.
From behind the Black Hill, which overlooks
Wanlockhead, another glen, “Glendyne,” runs down to the upland which
lies along the north-east side of the valley of the Nith. This glen
also well deserves a visit: indeed, it has often been said that had
Dr Brown, instead of descending Enterkin, taken Glendyne, he would
have been no less impressed with the solemn grandeur of the scene.
The only road is a narrow footpath worn along the face of the hill
side. So steep is the descent that the utmost care is necessary to
prevent serious mishap. If a stone from the path be loosened by the
foot it rolls swiftly down, and then, with a succession of mighty
bounds, dashes itself into the burn which winds along the bottom
like a silver thread. As the traveller descends, the face of the
hills on the two sides continues to be quite precipitous, the wonder
being that even the sheep can maintain their foothold ; but suddenly
the opening is reached, and with a fine sweep the beautiful glen
loses itself in the broad expanse of brown moorland. This moorland
is a high table-land stretching along the north-east of the town of
Sanquhar, four miles in length and two miles in breadth, and as it
is traversed by road and path in various directions, the
invigorating breezes which play over its surface draw thither those
who are in quest of health. It is pierced by the pretty little glen
of Lochburn, a tributary of Mennock, the clear water of which,
diverted at a point three miles from the town provide, after it has
been filtered, an excellent domestic supply. The portion of the
moorland which overlooks Sanquhar is the property of the
Corporation, and is reached by a steep ascent called Matthew’s
Folly, where numerous seats have been provided for the convenience
of visitors. These seats, and others placed here and there by the
waysides, were erected out of the balance of the fund which was
raised for the celebration of the Queen’s Jubilee in 1887. From the
top of Matthew’s Folly a splendid view of the valley for a length of
over twenty miles is obtained, and being so close at hand it is much
frequented with this object. The Moor farm, belonging to the town,
is let on lease. At one time it brought a rent of £190, but like all
other land it has fallen of recent years in value, and now the rent
is only £112. That, however, forms an important—in fact, the only
important—part of the town’s revenue since the abolition of
“Customs” in 1889. Any further reference to this and other allied
topics is reserved for the chapter dealing with the municipal
history of the place.
The chief eminences in the neighbourhood are—Dalpeddar,
1291; Brownhill, 1544; Lowther, 2377; Auchenlone, 2068; Craignorth,
1386; Auchinsow, 1378; Black Lorg, 2231 feet.
EUCHAN WELL
A sample of the water of this well was sent several
years ago to Professor Penney, of the Andersonian University,
Glasgow, who reported on it as follows:—“This water is specially
characterised by the notable quantity of iron which it contains. All
the substances included in the analyses exist in the water in a
state of perfect solution; the water is clear, bright, and nearly
colourless, shewing that the ferruginous ingredient is perfectly
dissolved. It has a styptic and astringent taste, and affords
abundance of evidence of the presence of iron on the application of
appropriate tests. The iron exists in the water in the form of the
compound called the carbonate of iron, which consists of carbonic
acid in combination with the protoxide of the metal. The tonic
astringent, and other medical qualities of chalybeate waters, are
too well recognised and appreciated by medical men to require notice
in a chemical report. These waters are by no means uncommon. In
regard to therapeutic strength, or medicinal power, as estimated
from the amount of iron it contains, the Sanquhar chalybeate is
about one-half the strength of Harrogate, Tunbridge, and Hartfell
Spa waters, which, with the exception of Cheltenham water, are the
strongest of those above mentioned. This, therefore, is not a strong
chalybeate, but from the perfect solution in which the iron exists,
and from the purity of the water, it is, in my opinion, well worth
the attention of medical men.” Professor Christison thus expresses
his view :—“The water is calculated to be serviceable in all
diseases for which simple chalybeate springs are at present resorted
to with success.” The following is Professor Penney’s analysis in
detail:—
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