Speculations in the Old Red Sandstone, and their Character.--George,
first Earl of Cromarty.--His Sagacity as a Naturalist at fault in
one Instance.--Sets himself to dig for Coal in the Lower Old lied
Sandstone.--Discovers a fine Artesian Well.--Value of Geological
Knowledge in an economic View.--Scarce a Secondary Formation in the
Kingdom in which Coal has not been sought for.--Mineral Springs
of the Lower Old Red Sandstone.--Strathpeffer.--Its Peculiarities
whence derived.--Chalybeate Springs of Easter Ross and the Black
Isle.--Petrifying Springs.--Building-Stone and Lime of the Old Red
Sandstone.--Its various Soils.
There has been much money lost, and a good deal won, in speculations
connected with the Old Red Sandstone. The speculations in which money
has been won have consorted, if I may so speak, with the character
of the system, and those in which money has been lost have not.
Instead, however, of producing a formal chapter on the economic uses
to which its various deposits have been applied, or the unfortunate
undertakings which an acquaintance with its geology would have
prevented, I shall throw together, as they occur to me, a few simple
facts illustrative of both.
George, first Earl of Cromarty, seems, like his namesake and
contemporary, the too celebrated Sir George M'Kenzie, of Roseavoch,
to have been a man of an eminently active and inquiring mind. He
found leisure, in the course of a very busy life, to write several
historical dissertations of great research, and a very elaborate
_Synopsis Apocalyptica_. He is the author, too, of an exceedingly
curious letter on the "Second Sight," addressed to the philosophic
Boyle, which contains a large amount of amusing and extraordinary
fact; and his description of the formation of a peat-moss in the
central Highlands of Ross-shire has been quoted by almost every
naturalist who, since the days of the sagacious, nobleman, has
written on the formation of peat. His life was extended to extreme
old age; and as his literary ardor remained undiminished till the
last, some of his writings were produced at a period when most other
men are sunk in the incurious indifferency and languor of old age.
And among these later productions are his remarks on peat. He relates
that, when a very young man, he had marked, in passing on a journey
through the central Highlands of Ross-shire, a wood of very ancient
trees, doddered and moss-grown, and evidently passing into a state of
death through the last stages of decay. He had been led by business
into the same district many years after, when in middle life, and
found that the wood had entirely disappeared, and that the heathy
hollow which it had covered was now occupied by a green, stagnant
morass, unvaried in its tame and level extent by either bush or tree.
In his old age he again visited the locality, and saw the green
surface roughened with dingy-colored hollows, and several Highlanders
engaged in it in cutting peat in a stratum several feet in depth.
What he had once seen an aged forest had now become an extensive
peat-moss.
Some time towards the close of the seventeenth century he purchased
the lands of Cromarty, where his turn for minute observation seems
to have anticipated--little, however, to his own profit--some of
the later geological discoveries. There is a deep, wooded ravine in
the neighborhood of the town, traversed by a small stream, which
has laid bare, for the space of about forty yards in the opening
of the hollow, the gray sandstone and stratified clays of the
inferior fish bed. The locality is rather poor in ichthyolites,
though I have found in it, after minute search, a few scales of the
_Osteolepis_, and on one occasion one of the better marked plates of
the _Coccosteus_; but in the vegetable impressions peculiar to the
formation it is very abundant. These are invariably carbonaceous,
and are not unfrequently associated with minute patches of bitumen,
which, in the harder specimens, present a coal-like appearance; and
the vegetable impressions and the bitumen seem to have misled the
sagacious nobleman into the belief that coal might be found on his
new property. He accordingly brought miners from the south, and set
them to bore for coal in the gorge of the ravine. Though there was
probably a register kept of the various strata through which they
passed, it must have long since been lost; but from my acquaintance
with this portion of the formation, as shown in the neighboring
sections, where it lies uplifted against the granitic gneiss of the
Sutors, I think I could pretty nearly restore it. They would first
have had to pass for about thirty feet through the stratified clays
and shales of the ichthyolite bed, with here and there a thin band
of gray sandstone, and here and there a stratum of lime; they would
next have had to penetrate through from eighty to a hundred feet of
coarse red and yellow sandstone, the red greatly predominating. They
would then have entered the great conglomerate, the lowest member of
the formation; and in time, if they continued to urge their fruitless
labors, they would arrive at the primary rock, with its belts of
granite, and its veins and huge masses of hornblende. In short, there
might be some possibility of their penetrating to the central fire,
but none whatever of their ever reaching a vein of coal. From a
curious circumstance, however, they were prevented from ascertaining,
by actual experience, the utter barrenness of the formation.
Directly in the gorge of the ravine, where we may see the partially
wooded banks receding as they ascend from the base to the centre,
and then bellying over from the centre to the summit, there is a
fine chalybeate spring, surmounted by a dome of hewn stone. It was
discovered by the miners when in quest of the mineral which they did
not and could not discover, and forms one of the finest specimens of
a true Artesian well which I have any where seen. They had bored to
a considerable depth, when, on withdrawing the kind of auger used
for the purpose, a bolt of water, which occupied the whole diameter
of the bore, came rushing after, like the jet of a fountain, and
the work was prosecuted no further; for, as steam-engines were not
yet invented, no pit could have been wrought with so large a stream
issuing into it; and as the volume was evidently restricted by the
size of the bore, it was impossible to say how much greater a stream
the source might have supplied. The spring still continues to flow
towards the sea, between its double row of cresses, at the rate of
about a hogshead per minute--a rate considerably diminished, it is
said, from its earlier volume, by some obstruction in the bore.
The waters are not strongly tinctured--a consequence, perhaps, of
their great abundance; but we may see every pebble and stock in
their course enveloped by a ferruginous coagulum, resembling burnt
sienna, that has probably been disengaged from the dark red sandstone
below, which is known to owe its color to the oxide of iron. A Greek
poet would probably have described the incident as the birth of the
Naiad; in the north, however, which, in an earlier age, had also
its Naiads, though, like the fish of the Old Red Sandstone, they
have long since become extinct, the recollection of it is merely
preserved by tradition, as a curious, though by no means poetical
fact, and by the name of the well, which is still known as the well
of the _coal-heugh_--the old Scotch name for a coal-pit. Calderwood
tells us, in his description of a violent tempest which burst out
immediately as his persecutor, James VI., breathed his last, that in
Scotland the sea rose high upon the land, and that many "coal-heughs
were drowned."
There is no science whose value can be adequately estimated by
economists and utilitarians of the lower order. Its true quantities
cannot be represented by arithmetical figures or monetary tables;
for its effects on mind must be as surely taken into account as its
operations on matter, and what it has accomplished for the human
intellect as certainly as what it has done for the comforts of
society or the interests of commerce. Who can attach a marketable
value to the discoveries of Newton? I need hardly refer to the
often-quoted remark of Johnson; the beauty of the language in
which it is couched has rendered patent to all the truth which it
conveys. "Whatever withdraws us from the power of the senses,"
says the moralist--"whatever makes the past, the distant, or the
future, predominate over the present, advances us in the dignity
of thinking beings." And Geology, in a peculiar manner, supplies
to the intellect an exercise of this ennobling character. But
it has, also, its cash value. The time and money squandered in
Great Britain alone in searching for coal in districts where the
well-informed geologist could have at once pronounced the search
hopeless, would much more than cover the expense at which geological
research has been prosecuted throughout the world. There are few
districts in Britain occupied by the secondary deposits, in which,
at one time or another, the attempt has not been made. It has been
the occasion of enormous expenditure in the south of England among
the newer formations, where the coal, if it at all occurs, (for
we occasionally meet with wide gaps in the scale,) must be buried
at an unapproachable depth. It led in Scotland--in the northern
county of Sutherland--to an unprofitable working for many years of
a sulphureous lignite of the inferior Oolite, far above the true
Coal Measures. The attempt I have just been describing was made in
a locality as far beneath them. There is the scene of another and
more modern attempt in the same district, on the shores of the Moray
Frith, in a detached patch of Lias, where a fossilized wood would
no doubt be found in considerable abundance, but no continuous vein
even of lignite. And it is related by Dr. Anderson, of Newburgh,
that a fruitless and expensive search after coal has lately been
instituted in the Old Red Sandstone beds which traverse Strathearn
and the Carse of Gowrie, in the belief that they belong not to
the Old, but to the New Red Sandstone--a formation which has been
successfully perforated in prosecuting a similar search in various
parts of England. All these instances--and there are hundreds
such--show the economic importance of the study of fossils. The
Oolite has its veins of apparent coal on the coast of Yorkshire,
and its still more amply developed veins--one of them nearly four
feet in thickness--on the eastern coast of Sutherlandshire; the
Lias has its coniferous fossils in great abundance, some of them
converted into a lignite which can scarce be distinguished from a
true coal; and the bituminous masses of the Lower Old Red, and its
carbonaceous markings, appear identical, to an unpractised eye, with
the impressions on the carboniferous sandstones, and the bituminous
masses which they, too, are occasionally found to enclose. Nor does
the mineralogical character of its middle beds differ in many cases
from that of the lower members of the New Red Sandstone. I have seen
the older rock in the north of Scotland as strongly saliferous as
any of the newer sandstones, of well nigh as bright a brick-red
tint, of as friable and mouldering a texture, and variegated as
thickly with its specks and streaks of green and buff-color. But
in all these instances there are strongly characterized groups of
fossils, which, like the landmarks of the navigator, or the findings
of his quadrant, establish the true place of the formations to
which they belong. Like the patches of leather, of scarlet, and of
blue, which mark the line attached to the deep-sea lead, they show
the various depths at which we arrive. The Earls of Sutherland set
themselves to establish a coal-work among the chambered univalves
of the Oolite, and a vast abundance of its peculiar bivalves. The
coal-borers who perforated the Lias near Cromarty passed every day
to and from their work over one of the richest deposits of animal
remains in the kingdom--a deposit full of the most characteristic
fossils; and drove their auger through a thousand belemnites and
ammonites of the upper and inferior Lias, and through gryphites and
ichthyodorulites innumerable. The sandstones of Strathearn and the
Carse of Gowrie yield their plates and scales of the _Holoptychius_,
the most abundant fossil of the Upper Old Red; and the shale of the
little dell in which the first Earl of Cromarty set his miners to
work, contains, as I have said, plates of the Coccosteus and scales
of the _Osteolepis_--fossils found only in the Lower Old Red. Nature,
in all these localities, furnished the index, but men lacked the
skill necessary to decipher it.[AU] I may mention that, independently
of their well-marked organisms, there is a simple test through which
the lignites of the newer formations may be distinguished from the
true coal of the carboniferous system. Coal, though ground into an
impalpable powder, retains its deep black color, and may be used as
a black pigment; lignite, on the contrary, when fully levigated,
assumes a reddish, or, rather, umbry hue.
[Footnote AU: There occurs in Mr. Murchison's _Silurian System_ a
singularly amusing account of one of the most unfortunate of all
coal-boring enterprises; the unlucky projector, a Welsh farmer,
having set himself to dig for coal in the lowest member of the
system, at least six formations beneath the only one at which the
object of his search could have been found. Mr. Murchison thus
relates the story:--
"At Tin-y-coed I found a credulous farmer ruining himself in
excavating a horizontal gallery in search of coal, an ignorant miner
being his engineer. The case may serve as a striking example of the
_coal-boring_ mania in districts which cannot by possibility contain
that mineral; and a few words concerning it may, therefore, prove
a salutary warning to those who speculate for coal in the Silurian
Rocks. The farmhouse of Tin-y-coed is situated on the sloping sides
of a hill of trap, which throw off, upon its north-western flank,
thin beds of black grauwacke shale, dipping to the west-north-west at
a high angle. The color of the shale, and of the water that flowed
down its sides, the pyritous veins, and other vulgar symptoms of
coal-bearing strata, had long convinced the farmer that he possessed
a large hidden mass of coal, and, unfortunately, a small fragment
of real anthracite was discovered, which burnt like the best coal.
Miners were sent for, and operations commenced. To sink a shaft was
impracticable, both from the want of means, and the large volume
of water. A slightly inclined gallery was therefore commenced, the
mouth of which was opened at the bottom of the hill, on the side of
the little brook which waters the dell. I have already stated that,
in many cases, where the intrusive trap throws off the shale, the
latter preserves its natural and unaltered condition to within a
certain distance of the trap; and so it was at Tin-y-coed, for the
level proceeded for 155 feet with little or no obstacle. Mounds of
soft black shale attested the rapid progress of the adventurers, when
suddenly they came to a 'change of metal.' They were now approaching
the nucleus of the little ridge; and the rock they encountered was,
as the men informed me, '_as hard as iron_,' viz., of lydianized
schist, precisely analogous to that which is exposed naturally in
ravines where all the phenomena are laid bare. The deluded people,
however, endeavored to penetrate the hardened mass, but the vast
expense of blasting it put a stop to the undertaking, not, however,
without a thorough conviction on the part of the farmer, that, could
he but have got through that hard stuff, he would most surely have
been well recompensed, for it was just thereabouts that they began
to find '_small veins of coal_.' It has been before shown, that
portions of anthracite are not unfrequent in the altered shale,
where it is in contact with the intrusive rock. And the occurrence
of the smallest portion of anthracite is always sufficient to lead
the Radnorshire farmer to suppose that he is very near 'El Dorado.'
Amid all their failures, I never met with an individual who was
really disheartened; a frequent exclamation being, 'O, if our squires
were only men of _spirit_, we should have as fine coal as any in the
world!'"--(_Silurian System_, Part I., p. 328.)]
I have said that the waters of the well of the coal-heugh are
chalybeate--a probable consequence of their infiltration through
the iron oxides of the superior beds of the formation, and their
subsequent passage through the deep red strata of the inferior bed.
There could be very curious chapters written on mineral springs,
in their connection with the formations through which they pass.
Smollett's masterpiece, honest old Matthew Bramble, became thoroughly
disgusted with the Bath waters on discovering that they filtered
through an ancient burying-ground belonging to the Abbey, and that
much of their peculiar taste and odor might probably be owing to
the "rotten bones and mouldering carcasses" through which they were
strained. Some of the springs of the Old Red Sandstone have also the
churchyard taste, but the bones and carcasses through which they
strain are much older than those of the Abbey burying-ground at Bath.
The bitumen of the strongly impregnated rocks and clay-beds of this
formation, like the bitumen of the still more strongly impregnated
limestones and shales of the Lias, seems to have had rather an animal
than vegetable origin. The shales of the Eathie Lias burn like turf
soaked in oil, and yet they hardly contain one per cent, of vegetable
matter. In a single cubic inch, however, I have counted about eighty
molluscous organisms, mostly ammonites, and minute striated scallops;
and the mass, when struck with the hammer, still yields the heavy
odor of animal matter in a state of decay. The lower fish-beds of
the Old Red are, in some localities, scarcely less bituminous.
The fossil scales and plates, which they enclose, burn at the
candle; they contain small cavities filled with a strongly scented,
semi-fluid bitumen, as adhesive as tar, and as inflammable; and for
many square miles together the bed is composed almost exclusively
of a dark-colored, semi-calcareous, semi-aluminous schist, scarcely
less fetid, from the great quantity of this substance which it
contains, than the swine-stones of England. Its vegetable remains
bear but a small proportion to its animal organisms; and from huge
accumulations of these last decomposing amid the mud of a still sea,
little disturbed by tempests or currents, and then suddenly interred
by some widely spread catastrophe, to ferment and consolidate under
vast beds of sand and conglomerate, the bitumen[AV] seems to have
been elaborated. These bituminous schists, largely charged with
sulphuret of iron, run far into the interior, along the flanks
of the gigantic Ben Nevis, and through the exquisitely pastoral
valley of Strathpeffer. The higher hills which rise over the valley
are formed mostly of the great conglomerate--Knockferril, with its
vitrified fort--the wooded and precipitous ridge over Brahan--and
the middle eminences of the gigantic mountain on the north; but
the bottom and the lower slopes of the valley are occupied by the
bituminous and sulphureous schists of the fish-bed, and in these,
largely impregnated with the peculiar ingredients of the formation,
the famous medicinal springs of the Strath have their rise. They
contain, as shown by chemical analysis, the sulphates of soda, of
lime, of magnesia, common salt, and, above all, sulphuretted hydrogen
gas--elements which masses of sea-mud, charged with animal matter,
would yield as readily to the chemist as the medicinal springs of
Strathpeffer. Is it not a curious reflection, that the commercial
greatness of Britain, in the present day, should be closely connected
with the towering and thickly spread forests of arboraceous ferns and
gigantic reeds--vegetables of strange form and uncouth names--which
flourished and decayed on its surface, age after age, during the
vastly extended term of the carboniferous period, ere the mountains
were yet upheaved, and when there was as yet no man to till the
ground? Is it not a reflection equally curious, that the invalids of
the present summer should be drinking health, amid the recesses of
Strathpeffer, from the still more ancient mineral and animal debris
of the lower ocean of the Old Red Sandstone, strangely elaborated
for vast but unreckoned periods in the bowels of the earth? The fact
may remind us of one of the specifics of a now obsolete school of
medicine, which flourished in this country about two centuries ago,
and which included in its _materia medica_ portions of the human
frame. Among these was the flesh of Egyptian mummies, impregnated
with the embalming drugs--the dried muscles and sinews of human
creatures who had walked in the streets of Thebes or of Luxor three
thousand years ago.
[Footnote AV: "In the slaty schists of Seefeld, in the Tyrol,"
say Messrs. Sedgwick and Murchison, "there is such an abundance
of a similar bitumen, that it is largely extracted for medicinal
purposes."--(_Geol. Trans. for 1829_, p. 134.)]
The commoner mineral springs of the formation, as might be
anticipated, from the very general diffusion of the oxide to which it
owes its color, are chalybeate. There are districts in Easter-Ross
and the Black Isle in which the traveller scarcely sees a runnel by
the way-side that is not half choked up by its fox-colored coagulum
of oxide. Two of the most strongly impregnated chalybeates with which
I am acquainted gush out of a sandstone bed, a few yards apart,
among the woods of Tarbat House, on the northern shore of the Frith
of Cromarty. They splash among the pebbles with a half-gurgling,
half-tinkling sound, in a solitary but not unpleasing recess,
darkened by alders and willows; and their waters, after uniting in
the same runnel, form a little, melancholy looking _lochan_, matted
over with weeds, and edged with flags and rushes, and which swarms
in early summer with the young of the frog in its tadpole state, and
in the after months with the black water-beetle and the newt. The
circumstance is a somewhat curious one, as the presence of iron as an
oxide has been held so unfavorable to both animal and vegetable life,
that the supposed poverty of the Old Red Sandstone in fossil remains
has been attributed to its almost universal diffusion at the period
the deposition was taking place. Were the system as poor as has been
alleged, however, it might be questioned, on the strength of a fact
such as this, whether the iron militated so much against the living
existences of the formation, as against the preservation of their
remains when dead.
Some of the springs which issue from the ichthyolite beds along
the shores of the Moray Frith are largely charged, not with iron,
like the well of the coal-heugh, or the springs of Tarbat House,
nor yet with hydrogen and soda, like the spa of Strathpeffer, but
with carbonate of lime. When employed for domestic purposes, they
choke up, in a few years, with a stony deposition, the spouts of
tea-kettles. On a similar principle, they plug up their older
channels, and then burst out in new ones; nor is it uncommon
to find among the cliffs little hollow recesses, long since
divested of their waters by this process, that are still thickly
surrounded by coral-like incrustations of moss and lichens, grass
and nettle-stalks, and roofed with marble-like stalactites. I am
acquainted with at least one of these springs of very considerable
volume, and dedicated of old to an obscure Roman Catholic saint,
whose name it still bears, (St. Bennet,) which presents phenomena
not unworthy the attention of the young geologist. It comes gushing
from out the ichthyolite bed, where the latter extends, in the
neighborhood of Cromarty, along the shores of the Moray Frith;
and after depositing in a stagnant morass an accumulation of a
grayish-colored and partially consolidated travertin, escapes by
two openings to the shore, where it is absorbed among the sand and
gravel. A storm about three years ago swept the beach several feet
beneath its ordinary level, and two little moles of conglomerate
and sandstone, the work of the spring, were found to occupy the two
openings. Each had its fossils--comminuted sea-shells, and stalks
of hardened moss; and in one of the moles I found imbedded a few
of the vertebral joints of a sheep. It was a recent formation on a
small scale, bound together by a calcareous cement furnished by the
fish-beds of the inferior Old Red Sandstone, and composed of sand and
pebbles, mostly from the granitic gneiss of the neighboring hill, and
organisms, vegetable and animal, from both the land and the sea.
The Old Red Sandstone of Scotland has been extensively employed
for the purposes of the architect, and its limestones occasionally
applied to those of the agriculturist. As might be anticipated
in reference to a deposit so widely spread, the quality of both
its sandstones and its lime is found to vary exceedingly in even
the same beds when examined in different localities. Its inferior
conglomerate, for instance, in the neighborhood of Cromarty, weathers
so rapidly, that a fence built of stones furnished by it little more
than half a century ago, has mouldered in some places into a mere
grass-covered mound. The same bed in the neighborhood of Inverness is
composed of a stone nearly as hard and quite as durable as granite,
and which has been employed in paving the streets of the place--a
purpose which it serves as well as any of the igneous or primary
rocks could have done. At Redcastle, on the northern shore of the
Frith of Beauly, the same conglomerate assumes an intermediate
character, and forms, though coarse, an excellent building stone,
which, in some of the older ruins of the district, presents the
marks of the tool as sharply indented as when under the hands of
the workman. Some of the sandstone beds of the system are strongly
saliferous; and these, however coherent they may appear, never resist
the weather until first divested of their salt. The main ichthyolite
bed on the northern shore of the Moray Frith is overlaid by a thick
deposit of a finely-tinted yellow sandstone of this character, which,
unlike most sandstones of a mouldering quality, resists the frosts
and storms of winter, and wastes only when the weather becomes warm
and dry. A few days of sunshine affect it more than whole months of
high winds and showers. The heat crystallizes at the surface the
salt which it contains; the crystals, acting as wedges, throw off
minute particles of the stone; and thus, mechanically at least,
the degrading process is the same as that to which sandstones of a
different but equally inferior quality are exposed during severe
frosts. In the course of years, however, this sandstone, when
employed in building, loses its salt; crust after crust is formed
on the surface, and either forced off by the crystals underneath,
or washed away by the rains; and then the stone ceases to waste,
and gathers on its weathered inequalities a protecting mantle of
lichens.[AW] The most valuable quarries in the Old Red System of
Scotland yet discovered, are the flagstone quarries of Caithness
and Carmylie. The former have been opened in the middle schists of
the lower, or Tilestone formation of the system; the latter, as I
have had occasion to remark oftener than once, in the Cornstone,
or middle formation. The quarries of both Carmylie and Caithness
employ hundreds of workmen, and their flagstones form an article of
commerce. The best building-stone of the north of Scotland--best both
for beauty and durability--is a pure Quartzose Sandstone furnished
by the upper beds of the system. These are extensively quarried in
Moray, near the village of Burghead, and exported to all parts of
the kingdom. The famous obelisk of Forres, so interesting to the
antiquary--which has been described by some writers as formed of a
species of stone unknown in the district, and which, according to a
popular tradition, was transported from the Continent--is evidently
composed of this Quartzose Sandstone, and must have been dug out of
one of the neighboring quarries. And so coherent is its texture, that
the storms of, perhaps, ten centuries have failed to obliterate its
rude but impressive sculptures.
[Footnote AW: When left to time the process is a tedious one, and,
ere its accomplishment, the beauty of the masonry is always in some
degree destroyed. The following passage, from a popular work, points
out a mode by which it might possibly be anticipated, and the waste
of surface prevented:--"A hall of which the walls were constantly
damp, though every means were employed to keep them dry, was about to
be pulled down, when M. Schmithall recommended, as a last resource,
that the walls should be washed with sulphuric acid, (vitriol.)
It w T as done, and the deliquescent salts being decomposed by
acid, the walls dried, and the hall was afterwards free from
dampness."--(_Recreations in Science._)]
The limestones of both the upper and lower formations of the system
have been wrought in Moray with tolerable success. In both, however,
they contain a considerable per centage of siliceous and argillaceous
earth. The system, though occupying an intermediate place between
two metalliferous deposits,--the grauwacke and the carboniferous
limestone,--has not been found to contain workable veins any where
in Britain, and in Scotland no metallic veins of any kind, with the
exception of here and there a few slender threads of ironstone,
and here and there a few detached crystals of galena. Its wealth
consists exclusively in building and paving stone, and in lime. Some
of the richest tracts of corn land in the kingdom rest on the Old
Red Sandstone--the agricultural valley of Strathmore, for instance,
and the fertile plains of Easter-Ross: Caithness has also its deep,
corn-bearing soils, and Moray has been well known for centuries as
the granary of Scotland. But in all these localities the fertility
seems derived rather from an intervening subsoil of tenacious
diluvial clay, than from the rocks of the system. Wherever the clay
is wanting, the soil is barren. In the moor of the Milbuy,--a tract
about fifty square miles in extent, and lying within an hour's walk
of the Friths of Cromarty and Beauly,--a thin covering of soil rests
on the sandstones of the lower formation. And so extreme is the
barrenness of this moor, that notwithstanding the advantages of its
semi-insular situation, it was suffered to lie as an unclaimed common
until about twenty-five years ago, when it was parcelled out among
the neighboring proprietors.