The Cruise of the Betsey Part 3

A deep indentation of the coast, which forms the bay of Broadford, corresponds with the hollow of the valley. It is simply a portion of the valley itself occupied by the sea; and we find the Lias, from its lower to its upper beds, exposed in unbroken series along the beach. In the middle of the opening lies the green level island of Pabba, altogether composed of this formation, and which, differing, in consequence, both in outline and color, from every neighboring island and hill, seems a little bit of flat fertile England, laid down, as if for contrast's sake, amid the wild rough Hebrides. Of Pabba and its wonders, however, more anon. I explored a considerable range of sh.o.r.e along the bay; but as I made it the subject of two after explorations ere I mastered its deposits, I shall defer my description till a subsequent chapter. It was late this evening ere the post-gig arrived from the south, and the night and several hours of the following morning were spent in travelling to Portree. I know not, however, that I could have seen some of the wildest and most desolate tracts in Skye to greater advantage. There was light enough to show the bold outlines of the hills,--lofty, abrupt, pyramidal,--just such hills, both in form and grouping, as a profile in black showed best; a low blue vapor slept in the calm over the marshes at their feet; the sea, smooth as gla.s.s, reflected the dusk twilight gleam in the north, revealing the narrow sounds and deep mountain-girdled lochs along which we pa.s.sed; gray crags gleamed dimly on the sight; birch-feathered acclivities presented against sea and sky their rough bristly edges; all was vast, dreamy, obscure, like one of Martin's darker pictures: the land of the seer and the spectre could not have been better seen. Morning broke dim and gray, while we were yet several miles from Portree; and I reached the inn in time to see from my bed-room windows the first rays of the rising sun gleaming on the hill-tops.

CHAPTER VII.

Exploration resumed--Geology of Rasay--An Ill.u.s.tration--Storr of Skye--From Portree to Holm--Discovery of Fossils--An Island Rain--Sir R. Murchison--Labor of drawing a Geological Line--Three Edinburgh Gentlemen--_Prosopolepsia_--Wrong surmises corrected--The Mail Gig--The Portree Postmaster--Isle Ornsay--An Old Acquaintance--Reminiscences--A Run for Rum--"Semi-fossil Madeira"--Idling on Deck--Prognostics of a Storm--Description of the Gale--Loch Scresort--The Minister's lost _Sou-wester_--The Free Church Gathering--The weary Minister.

I breakfasted in the travellers' room with three gentlemen from Edinburgh; and then, accompanied by a boy, whom I had engaged to carry my bag, set out to explore. The morning was ominously hot and breathless; and while the sea lay moveless in the calm, as a floor of polished marble, mountain and rock, and distant island, seemed tremulous all over, through a wavy medium of thick rising vapor. I judged from the first that my course of exploration for the day was destined to terminate abruptly; and as my arrangements with Mr. Swanson left me, for this part of the country, no second day to calculate upon, I hurried over deposits which in other circ.u.mstances I would have examined more carefully,--content with a glance. Accustomed in most instances to take long aims, as Cuddy Headrig did, when he steadied his musket on a rest behind the hedge, and sent his ball through Laird Oliphant's forehead, I had on this occasion to shoot flying; and so, selecting a large object for a mark, that I might run the less risk of missing, I strove to acquaint myself rather with the general structure of the district than with the organisms of its various fossiliferous beds.

The long narrow island of Rasay lies parallel to the coast of Skye, like a vessel laid along a wharf, but drawn out from it as if to suffer another vessel of the same size to take her berth between; and on the eastern sh.o.r.es of both Skye and Rasay we find the same Oolitic deposits tilted up at nearly the same angle. The section presented on the eastern coast of the one is nearly a duplicate of the section presented on the eastern coast of the other. During one of the severer frosts of last winter I pa.s.sed along a shallow pond, studded along the sides with boulder stones. It had been frozen over; and then, from the evaporation so common in protracted frosts, the water had shrunk, and the sheet of ice which had sunk down over the central portion of the pond exhibited what a geologist would term very considerable marks of disturbance among the boulders at the edges. Over one sharp-backed boulder there lay a sheet tilted up like the lid of a chest half-raised; and over another boulder immediately behind it there lay another uptilted sheet, like the lid of a second half-open chest; and in both sheets, the edges, lying in nearly parallel lines, presented a range of miniature cliffs to the sh.o.r.e. Now, in the two uptilted ice-sheets of this pond I recognized a model of the fundamental Oolitic deposits Rasay and Skye. The mainland of Scotland had its representative in the crisp snow-covered sh.o.r.e of the pond, with its belt of faded sedges; the place of Rasay was indicated by the inner, that of Skye by the outer boulder; while the ice-sheets, with their sh.o.r.eward-turned line of cliffs, represented the Oolitic beds, that turn to the mainland their dizzy range of precipices, varying from six to eight hundred feet in height, and then, sloping outwards and downwards, disappear under mountain wildernesses of overlying trap. And it was along a portion of the range of cliff that forms the outermost of the two uptilted lines, and which presents in this district of Skye a frontage of nearly twenty continuous miles to the long Sound of Rasay, that my to-day's course of exploration lay.

From the top of the cliff the surface slopes downwards for about two miles into the interior, like the half-raised chest-lid of my ill.u.s.tration sloping towards the hinges, or the uptilted ice-table of the boulder sloping towards the centre of the pond; and the depression behind forms a flat moory valley, full fifteen miles in length, occupied by a chain of dark bogs and treeless lochans. A long line of trap-hills rises over it, in one of which, considerably in advance of the others, I recognized the Storr of Skye, famous among lovers of the picturesque for its strange group of mingled pinnacles and towers; while directly crossing into the valley from the Sound, and then running southwards for about two miles along its bottom, is the n.o.ble sea-arm, Loch Portree, in which, as indicated by the name (the King's Port) a Scottish king of the olden time, in his voyage round his dominions, cast anchor. The opening of the loch is singularly majestic;--the cliffs tower high on either side in graceful magnificence: but from the peculiar inward slope of the land, all within, as the loch reaches the line of the valley, becomes tame and low, and a black dreary moor stretches from the flat terminal basin into the interior. The opening of Loch Portree is a palace gateway, erected in front of some homely suburb, that occupies the place which the palace itself should have occupied.

There was, however, no such mixture of the homely and the magnificent in the route I had selected to explore. It lay under the escarpment of the cliff; and I purposed pursuing it from Portree to Holm, a distance of about six miles, and then returning by the flat interior valley. On the one hand rose a sloping rampart, full seven hundred feet in height, striped longitudinally with alternating bands of white sandstone and dark shale, and capped atop by a continuous coping of trap, that lacked not ma.s.sy tower, and overhanging turret, and projecting sentry-box; while, on the other hand, spreading outwards in the calm from the line of dark trap-rocks below, like a mirror from its carved frame of black oak, lay the Sound of Rasay, with its n.o.ble background of island and main rising bold on the east, and its long mountain vista opening to the south. The first fossiliferous deposit which gave me occasion this morning to use my hammer occurs near the opening of the loch, beside an old Celtic burying-ground, in the form of a thick bed of hard sandstone, charged with Belemnites,--a bed that must at one time have existed as a widely-spread acc.u.mulation of sand,--the bottom, mayhap, of some extensive bay of the Oolite, resembling the Loch Portree of the present day, in which eddy tides deposited the sand swept along by the tidal currents of some neighboring sound, and which swarmed as thickly with Cephalopoda as the loch swarmed this day with minute purple-tinged Medusae. I found detached on the sh.o.r.e, immediately below this bed, a piece of calcareous fissile sandstone, abounding in small sulcated Terebratulae, identical, apparently, with the Terebratula of a specimen in my collection from the inferior Oolite of Yorkshire. A colony of this delicate Brachiopod must have once lain moored near this spot, like a fleet of long-prowed galleys at anchor, each one with its cable of many strands extended earthwards from the single _dead-eye_ in its umbone.

For a full mile after rounding the northern boundary of the loch, we find the immense escarpment composed from top to bottom exclusively of trap; but then the Oolite again begins to appear, and about two miles further on the section becomes truly magnificent,--one of the finest sections of this formation exhibited anywhere in Britain, perhaps in the world. In a ravine furrowed in the face of the declivity by the headlong descent of a small stream, we may trace all the beds of the system in succession, from the Cornbrash, an upper deposit of the Lower Oolite, down to the Lias, the formation on which the Oolite rests. The only modifying circ.u.mstance to the geologist is, that though the sandstone beds run continuously along the cliff for miles together, distinct as the white bands in a piece of onyx, the intervening beds of shale are swarded over, save where we here and there see them laid bare in some abrupter acclivity or deeper water-course. In the shale we find numerous minute Ammonites, sorely weathered; in the sandstone, Belemnites, some of them of great size; and dark carbonaceous markings, pa.s.sing not unfrequently into a glossy cubical coal. At the foot of the cliff I picked up an ammonite of considerable size and well-marked character,--the _Ammonites Murchisonae_, first discovered on this coast by Sir R. Murchison about fifteen years ago. It measures, when full grown, from six to seven inches in diameter; the inner whorls, which are broadly visible, are ribbed; whereas the two, and sometimes the three outer ones, are smooth,--a marked characteristic of the species. My specimen merely enabled me to examine the peculiarities of the sh.e.l.l just a little more minutely than I could have done in the pages of Sowerby; for such was its state of decay, that it fell to pieces in my hands. I had now come full in view of the rocky island of Holm, when the altered appearance of the heavens led me to deliberate, just as I was warming in the work of exploration, whether, after all, it might not be well to scale the cliffs, and strike directly on the inn. It was nearly three o'clock; the sky had been gradually darkening since noon, as if one thin covering of gauze after another had been drawn over it; hill and island had first dimmed and then disappeared in the landscape; and now the sun stood up right over the fast-contracting vista of the Sound, round and lightless as the moon in a haze; and the downward cataract-like streaming of the gray vapor on the horizon showed that there the rain had already broken, and was descending in torrents. We had been thirsty in the hot sun, and had found the springs few and scanty; but the boy now a.s.sured me, in very broken English, that we were to get a great deal more water than would be good for us, and that it might be advisable to get out of its way. And so, climbing to the top of the cliffs, along a water-course, we reached the ridge, just as the fog came rolling downwards from the peaked brow of the Storr into the flat moory valley, and the melancholy lochans roughened and darkened in the rain. We were both particularly wet ere we reached Portree.

In exploring our Scotch formations, I have had frequent occasion, in Ross, Sutherland, Caithness, and now once more in Skye, to pa.s.s over ground described by Sir R. Murchison; and in every instance have I found myself immensely his debtor. His descriptions possess the merit of being true: they are simple outlines often, that leave much to be filled up by after discovery; but, like those outlines of the skilful geographer that fix the place of some island or strait, though they may not entirely define it, they always indicate the exact position in the scale of the formations to which they refer. They leave a good deal to be done in the way of mapping out the interior of a deposit, if I may so speak; but they leave nothing to be done in the way of ascertaining its place. The work accomplished is _bona fide_ work,--actual, solid, not to be done over again,--work such as could be achieved in only the school of Dr.

William Smith, the father of English Geology. I have found much to admire, too, in the sections of Sir R. Murchison. His section of this part of the coast, for example, strikes from the extreme northern part of Skye to the island of Holm, thence to Sc.r.a.pidale in Rasay, thence along part of the coast of Scalpa, thence direct through the middle of Pabba, and thence to the sh.o.r.e of the Bay of Laig. The line thus taken includes, in regular sequence in the descending order, the whole Oolitic deposits of the Hebrides, from the Cornbrash, with its overlying fresh-water outliers of mayhap the Weald, down to where the Lower Lias rests on the primary red sandstones of Sleat. It would have cost M'Culloch less exploration to have written a volume than it must have cost Sir R. Murchison to draw this single line; but the line once drawn, is work done to the hands of all after explorers. I have followed repeatedly in the track of another geologist, of, however, a very different school, who explored, at a comparatively recent period, the deposits of not a few of our Scotch counties. But his labors, in at least the fossiliferous formations, seem to have accomplished nothing for Geology,--I am afraid, even less than nothing. So far as they had influence at all, it must have been to throw back the science. A geologist who could have a.s.serted only three years ago ("Geognostical Account of Banffshire," 1842), that the Old Red Sandstone of Scotland forms merely "a part of the great coal deposit," could have known marvellously little of the fossils of the one system, and nothing whatever of those of the other. Had he examined ere he decided, instead of deciding without any intention of examining, he would have found that, while both systems abound in organic remains, they do not possess, in Scotland at least, a single species in common, and that even their types of being, viewed in the group, are essentially distinct.

The three Edinburgh gentlemen whom I had met at breakfast were still in the inn. One of them I had seen before, as one of the guests at a Wesleyan soiree, though I saw he failed to remember that I had been there as a guest too. The two other gentlemen were altogether strangers to me. One of them,--a man on the right side of forty, and a superb specimen of the powerful, six-feet two-inch Norman Celt,--I set down as a scion of some old Highland family, who, as the broadsword had gone out, carried on the internal wars of the country with the formidable artillery of Statute and Decision. The other, a gentleman more advanced in life, I predicated to be a Highland proprietor, the uncle of the younger of the two,--a man whose name, as he had an air of business about him, occurred, in all probability, in the Almanac, in the list of Scotch advocates. Both were of course high Tories,--I was quite sure of that,--zealous in behalf of the Establishment, though previous to the Disruption they had not cared for it a pin's point,--and prepared to justify the virtual suppression of the toleration laws in the case of the Free Church. I was thus decidedly guilty of what old Dr. More calls a _prosopolepsia_,--_i.e._ of the crime of judging men by their looks.

At dinner, however, we gradually ate ourselves into conversation: we differed, and disputed, and agreed, and then differed, disputed and agreed again. I found first, that my chance companions were really not very high Tories; and then, that they were not Tories at all; and then, that the younger of the two was very much a Whig, and the more advanced in life,--strange as the fact might seem,--very considerably a _Presbyterian_ Whig; and finally, that this latter gentleman, whom I had set down as an intolerant Highland proprietor, was a respected writer to the signet, a Free Church elder in Edinburgh; and that the other, his equally intolerant nephew, was an Edinburgh advocate, of vigorous talent, much an enemy of all oppression, and a brother contributor of my own to one of the Quarterlies. Of all my surmisings regarding the stranger gentlemen, only two points held true,--they were both gentlemen of the law, and both had Celtic blood in their veins. The evening pa.s.sed pleasantly; and I can now recommend from experience, to the hapless traveller who gets thoroughly wet thirty miles from a change of dress, that some of the best things he can resort to in the circ.u.mstances are, a warm room, a warm gla.s.s, and agreeable companions.

On the morrow I behooved to return to Isle Ornsay, to set out on the following day, with my friend the minister, for Rum, where he purposed preaching on the Sabbath. To have lost a day would have been to lose the opportunity of exploring the island, perhaps forever; and, to make all sure, I had taken a seat in the mail gig, from the postman who drives it, ere going to bed, on the morning of my arrival; and now, when it drove up, I went to take my place in it. The postmaster of the village, a lean, hungry-looking man, interfered to prevent me. I had secured my seat, I said, two days previous. Ah, but I had not secured it from him.

"I know nothing of you," I replied; "but I secured it from one who deemed himself authorized to receive the fare; was he so?" "Yes." "Could you have received it?" "No." "Show me a copy of your regulations." "I have no copy of regulations; but I have given the place in the gig to another." "Just so; and what say you, postman?" "That you took the place from me, and that _he_ has no right to give a place to any one: I carry the Portree letters to him, but he has nothing to do with the pa.s.sengers." A person present, the proprietor or stabler of the horse, I believe, also interfered on the same side; but what Carlyle terms the "gigmanity" of the postmaster was all at stake,--his whole influence in the mail-gig of Portree; and so he argued, and threatened withal, and, what was the more serious part of the business, the person he had given the seat to had taken possession of the gig; and so we had to compound the matter by carrying a pa.s.senger additional. The incident is scarce worth relating; but the postmaster was so vehement and terrible, so defiant of us all,--post, stabler, and simple pa.s.senger,--and so justly impressed with the importance of being postmaster of Portree, that, as I am in the way of describing rare specimens at any rate, I must refer to him among the rest, as if he had been one of the minor carnivorae of a Skye deposit,--a cuttlefish, that preyed on the weaker molluscs, or a hungry polypus, terrible among the animalculae.

We drove heavily, and had to dismount and walk afoot over every steeper acclivity; but I carried my hammer, and only grieved that in some one or two localities the road should have been so level. I regretted it in especial on the southern and eastern side of Loch Sligachan, where I could see from my seat, as we drove past, the dark blue rocks in the water-courses on each side the road, studded over with that characteristic sh.e.l.l of the Lias, the _Gryphaea incurva_, and that the dry-stone fences in the moor above exhibit fossils that might figure in a museum. But we rattled by. At Broadford, twenty-five miles from Portree, and nine miles from Isle Ornsay, I partook of a hospitable meal in the house of an acquaintance; and in little more than two hours after was with my friend the minister at Isle Ornsay. The night wore pleasantly by. Mrs. Swanson, a niece of the late Dr. Smith of Campbelton, so well known for his Celtic researches and his exquisite translations of ancient Celtic poetry, I found deeply versed in the legendary lore of the Highlands. The minister showed me a fine specimen of Pterichthys which I had disinterred for him, out of my first discovered fossiliferous deposit of the Old Red Sandstone, exactly thirteen years before, and full seven years ere I had introduced the creature to the notice of Aga.s.siz. And the minister's daughter, a little chubby girl of three summers, taking part in the general entertainment, strove to make her Gaelic sound as like English as she could, in my especial behalf. I remembered, as I listened to the unintelligible prattle of the little thing, unprovided with a word of English, that just eighteen years before, her father had had no Gaelic; and wondered what he would have thought, could he have been told, when he first sat down to study it, the story of his island charge in Eigg, and his Free Church yacht the Betsey. Nineteen years before, we had been engaged in beating over the Eathie Lias together, collecting Belemnites, Ammonites, and fossil wood, and striving in friendly emulation the one to surpa.s.s the other in the variety and excellence of our specimens. Our leisure hours were s.n.a.t.c.hed, at the time, from college studies by the one, from the mallet by the other: there were few of them that we did not spend together, and that we were not mutually the better for so spending. I at least, owe much to these hours,--among other things, views of theologic truth, that determined the side I have taken in our ecclesiastical controversy. Our courses at an after period lay diverse; the young minister had greatly more important business to pursue than any which the geologic field furnishes; and so our amicable rivalry ceased early. In the words in which an English poet addresses his brother,--the clergyman who sat for the picture in the "Deserted Village,"--my friend "entered on a sacred office, where the harvest is great and the laborers are few, and left to me a field in which the laborers are many, and the harvest scarce worth carrying away."

Next day at noon we weighed anchor, and stood out for Rum, a run of about twenty-five miles. A kind friend had, we found, sent aboard in our behalf two pieces of rare antiquity,--rare anywhere, but especially rare in the lockers of the Betsey,--in the agreeable form of two bottles of semi-fossil Madeira,--Madeira that had actually existed in the grape exactly half a century before, at the time when Robespierre was startling Paris from its propriety, by mutilating at the neck the busts of other people, and multiplying casts and medals of his own; and we found it, explored in moderation, no bad study for geologists, especially in coa.r.s.e weather, when they had got wet and somewhat fatigued. It was like Landlord Boniface's ale, mild as milk, had exchanged its distinctive flavor as Madeira for a better one, and filled the cabin with fragrance every time the cork was drawn. Old observant Homer must have smelt some such liquor somewhere, or he could never have described so well the still more ancient and venerable wine with which wily Ulysses beguiled one-eyed Polypheme:--

"Unmingled wine, Mellifluous, undecaying, and divine, Which now, some ages from his race concealed, The h.o.a.ry sire in grat.i.tude revealed....

Scarce twenty measures from the living stream To cool one cup sufficed: the goblet crowned, Breathed aromatic fragrances around."

Winds were light and variable. As we reached the middle of the sound opposite Armadale, there fell a dead calm; and the Betsey, more actively idle than the ship manned by the Ancient Mariner, dropped sternwards along the tide, to the dull music of the flapping sail. The minister spent the day in the cabin, engaged with his discourse for the morrow; and I, that he might suffer as little from interruption as possible, _mis_-spent it upon the deck. I tried fishing with the yacht's set of lines, but there were no fish to bite,--got into the boat, but there were no neighboring islands to visit,--and sent half a dozen pistol-bullets after a shoal of porpoises, which, coming from the Free Church yacht, must have astonished the fat sleek fellows pretty considerably, but did them, I am afraid, no serious damage. As the evening began to close gloomy and gray, a tumbling swell came heaving in right ahead from the west; and a bank of cloud, which had been gradually rising higher and darker over the horizon in the same direction, first changed its abrupt edge atop for a diffused and broken line, and then spread itself over the central heavens. The calm was evidently not to be a calm long; and the minister issued orders that the gaff-topsail should be taken down, and the storm-jib bent; and that we should lower our topmast, and have all tight and ready for a smart gale ahead. At half past ten, however, the Betsey was still pitching to the swell, with not a breath of wind to act on the diminished canvas, and with the solitary circ.u.mstance in her favor, that the tide ran no longer against her, as before. The cabin was full of all manner of creakings; the close lamp swung to and fro over the head of my friend; and a refractory Concordance, after having twice travelled from him along the entire length of the table, flung itself pettishly upon the floor. I got into my snug bed about eleven; and at twelve, the minister, after poring sufficiently over his notes, and drawing the final score, turned into his. In a brief hour after, on came the gale, in a style worthy of its previous hours of preparation; and my friend,--his Sat.u.r.day's work in his ministerial capacity well over when he had completed his two discourses,--had to begin the Sabbath morning early as the morning itself began, by taking his stand at the helm, in his capacity of skipper of the Betsey. With the prospect of the services of the Sabbath before him, and after working all Sat.u.r.day to boot, it was rather hard to set him down to a midnight spell at the helm, but he could not be wanted at such a time, as we had no other such helmsman aboard. The gale, thickened with rain, came down, shrieking like a maniac, from off the peaked hills of Rum, striking away the tops of the long ridgy billows that had risen in the calm to indicate its approach, and then carrying them in sheets of spray aslant the furrowed surface, like snow-drift hurried across a frozen field. But the Betsey, with her storm-jib set, and her mainsail reefed to the cross, kept her weather bow bravely to the blast, and gained on it with every tack. She had been the pleasure yacht, in her day, of a man of fortune, who had used, in running south with her at times as far as Lisbon, to encounter, on not worse terms than the stateliest of her neighbors in the voyage, the swell of the Bay of Biscay; and she still kept true to her old character, with but this drawback, that she had now got somewhat crazy in her fastenings, and made rather more water in a heavy sea than her one little pump could conveniently keep under. As the fitful gust struck her headlong, as if it had been some invisible missile hurled at us from off the hill-tops, she stooped her head lower and lower, like old stately Hardyknute under the blow of the "King of Norse," till at length the lee chain-plate rustled sharp through the foam; but, like a staunch Free Churchwoman, the lowlier she bent, the more steadfastly did she hold her head to the storm. The strength of the opposition served but to speed her on all the more surely to the desired haven. At five o'clock in the morning we cast anchor in Loch Scresort,--the only harbor of Rum in which a vessel can moor,--within two hundred yards of the sh.o.r.e, having, with the exception of the minister, gained no loss in the gale.

He, luckless man, had parted from his excellent _sou-wester_; a sudden gust had seized it by the flap, and hurried it away far to the lee. He had yielded it to the winds, as he had done the temporalities, but much more unwillingly, and less as a free agent. Should any conscientious mariner pick up any where in the Atlantic a serviceable ochre-colored _sou-wester_, not at all the worse for the wear, I give him to wit that he holds Free Church property, and that he is heartily welcome to hold it, leaving it to himself to consider whether a benefaction to its full value, deducting salvage, is not owing, in honor, to the Sustenation Fund.

It was ten o'clock ere the more fatigued aboard could muster resolution enough to quit their beds a second time; and then it behooved the minister to prepare for his Sabbath labors ash.o.r.e. The gale still blew in fierce gusts from the hills, and the rain pattered like small shot on the deck. Loch Scresort, by no means one of our finer island lochs, viewed under any circ.u.mstances, looked particularly dismal this morning.

It forms the opening of a dreary moorland valley, bounded on one of its sides, to the mouth of the loch, by a homely ridge of Old Red Sandstone, and on the other by a line of dark augitic hills, that attain, at the distance of about a mile from the sea, an elevation of two thousand feet. Along the slopes of the sandstone ridge I could discern, through the haze, numerous green patches, that had once supported a dense population, long since "cleared off" to the backwoods of America, but not one inhabited dwelling; while along a black moory acclivity under the hills on the other side I could see several groups of turf cottages, with here and there a minute speck of raw-looking corn beside them, that, judging from its color, seemed to have but a slight chance of ripening. The hill-tops were lost in cloud and storm; and ever and anon, as a heavier shower came sweeping down on the wind, the intervening hollows closed up their gloomy vistas, and all was fog and rime to the water's edge. Bad as the morning was, however, we could see the people wending their way, in threes and fours, through the dark moor, to the place of worship,--a black turf hovel, like the meeting-house in Eigg.

The appearance of the Betsey in the loch had been the gathering signal; and the Free Church islanders,--three-fourths of the entire population--had all come out to meet their minister.

On going ash.o.r.e, we found the place nearly filled. My friend preached two long energetic discourses, and then returned to the yacht, "a worn and weary man." The studies of the previous day, and the fatigues of the previous night, added to his pulpit duties, had so fairly prostrated his strength, that the sternest teetotaller in the kingdom would scarce have forbidden him a gla.s.s of our fifty-year-old Madeira. But even the fifty-year-old Madeira proved no specific in the case. He was suffering under excruciating headache, and had to stretch himself in his bed, with eyes shut but sleepless, waiting till the fit should pa.s.s,--every pulse that beat in his temples a throb of pain.

CHAPTER VIII.

Geology of Rum--Its curious Character ill.u.s.trated--Rum famous for Bloodstones--Red Sandstones--"Scratchings" in the Rocks--A Geological Inscription without a Key--The Lizard--Vitality broken into two--Ill.u.s.trations--Speculation--Scuir More--Ascent of the Scuir--The Bloodstones--An Ill.u.s.trative Set of the Gem--M'Culloch's Pebble--A Chemical Problem--The solitary Shepherd's House--Sheep _versus_ Men--The Depopulation of Rum--A Haul of Trout--Rum Mode of catching Trout--At Anchor in the Bay of Glenelg.

The geology of the island of Rum is simple, but curious. Let the reader take, if he can, from twelve to fifteen trap-hills, varying from one thousand to two thousand three hundred feet in height; let him pack them closely and squarely together, like rum-bottles in a case-basket; let him surround them with a frame of Old Red Sandstone, measuring rather more than seven miles on the side, in the way the basket surrounds the bottles; then let him set them down in the sea a dozen miles off the land,--and he shall have produced a second island of Rum, similar in structure to the existing one. In the actual island, however, there is a defect in the inclosing basket of sandstone: the basket, complete on three of its sides, wants the fourth: and the side opposite to the gap which the fourth should have occupied is thicker than the two other sides put together. Where I now write there is an old dark-colored picture on the wall before me. I take off one of the four bars of which the frame is composed,--the end-bar,--and stick it on to the end-bar opposite, and then the picture is fully framed on two of its sides, and doubly framed on a third, but the fourth side lacks framing altogether.

And such is the geology of the island of Rum. We find the one loch of the island,--that in which the Betsey lies at anchor,--and the long withdrawing valley, of which the loch is merely a prolongation, occurring in the double sandstone bar: it seems to mark--to return to my ill.u.s.tration--the line in which the superadded piece of frame has been stuck on to the frame proper. The origin of the island is ill.u.s.trated by its structure: it has left its story legibly written, and we have but to run our eye over the characters and read. An extended sea-bottom, composed of Old Red Sandstone, already tilted up by previous convulsions, so that the strata presented their edges, tier beyond tier, like roofing slate laid aslant on a floor, became a centre of Plutonic activity. The molten trap broke through at various times, and presenting various appearances, but in nearly the same centre; here existing as an augitic rock, there as a syenite, yonder as a basalt or amygdaloid. At one place it uptilted the sandstone; at another it overflowed it; the dark central ma.s.ses raised their heads above the surface, higher and higher with every earthquake throe from beneath; till at length the gigantic Ben More attained to its present alt.i.tude of two thousand three hundred feet over the sea-level, and the sandstone, borne up from beneath like floating sea-wrack on the back of a porpoise, reached in long outside bands its elevation of from six to eight hundred. And such is the piece of history, composed in silent but expressive language, and inscribed in the old geological character, on the rocks of Rum.

The wind lowered and the rain ceased during the night, and the morning of Monday was clear, bracing, and breezy. The island of Rum is chiefly famous among mineralogists for its heliotropes or bloodstones; and we proposed devoting the greater part of the day to an examination of the hill of Scuir More, in which they occur, and which lies on the opposite side of the island, about eight miles from the mooring ground of the Betsey. Ere setting out, however, I found time enough, by rising some two or three hours before breakfast, to explore the Red Sandstones on the southern side of the loch. They lie in this bar of the frame,--to return once more to my old ill.u.s.tration,--as if it had been cut out of a piece of cross-grained deal, in which the annular bands, instead of ranging lengthwise, ran diagonally from side to side; stratum leans over stratum, dipping towards the west at an angle of about thirty degrees; and as in a continuous line of more than seven miles there seem no breaks or repet.i.tions in the strata, the thickness of the deposit must be enormous,--not less, I should suppose, than from six to eight thousand feet. Like the Lower Old Red Sandstones of Cromarty and Moray, the red arenaceous strata occur in thick beds, separated from each other by bands of a grayish-colored stratified clay, on the planes of which I could trace with great distinctness ripple markings; but in vain did I explore their numerous folds for the plates, scales, and fucoid impressions which abound in the gray argillaceous beds of the sh.o.r.es of the Moray and Cromarty Friths. It would, however, be rash to p.r.o.nounce them non-fossiliferous, after the hasty search of a single morning,--unpardonably so in one who had spent very many mornings in putting to the question the gray stratified beds of Ross and Cromarty, ere he succeeded in extorting from them the secret of their organic riches.

We set out about half-past ten for Scuir More, through the Red Sandstone valley in which Loch Scresort terminates, with one of Mr. Swanson's people, a young active lad of twenty, for our guide. In pa.s.sing upwards for nearly a mile along the stream that falls into the upper part of the loch, and lays bare the strata, we saw no change in the character of the sandstone. Red arenaceous beds of great thickness alternate with grayish-colored bands, composed of a ripple-marked micaceous slate and a stratified clay. For a depth of full three thousand feet, and I know not how much more,--for I lacked time to trace it further,--the deposit presents no other variety: the thick red bed of at least a hundred yards succeeds the thin gray band of from three to six feet, and is succeeded by a similar gray band in turn. The ripple-marks I found as sharply relieved in some of the folds as if the wavy undulations to which they owed their origin had pa.s.sed over them within the hour. The comparatively small size of their alternating ridges and furrows give evidence that the waters beneath which they had formed had been of no very profound depth. In the upper part of the valley, which is bare, trackless, and solitary, with a high monotonous sandstone ridge bounding it on the one side, and a line of gloomy trap-hills rising over it on the other, the edges of the strata, where they protrude through the mingled heath and moss, exhibit the mysterious scratchings and polishings now so generally connected with the glacial theory of Aga.s.siz. The scratchings run in nearly the line of the valley, which exhibits no trace of moraines; and they seem to have been produced rather by the operation of those extensively developed causes, whatever their nature, that have at once left their mark on the sides and summits of some of our highest hills, and the rocks and boulders of some of our most extended plains, than by the agency of forces limited to the locality. They testify, Aga.s.siz would perhaps say, not regarding the existence of some local glacier that descended from the higher grounds into the valley, but respecting the existence of the great polar glacier. I felt, however, in this bleak and solitary hollow, with the grooved and polished platforms at my feet, stretching away amid the heath, like flat tombstones in a graveyard, that I had arrived at one geologic inscription to which I still wanted the key. The vesicular structure of the traps on the one hand, identical with that of so many of our modern lavas,--the ripple-markings of the arenaceous beds on the other, indistinguishable from those of the sea-banks on our coasts,--the upturned strata and the overlying trap,--told all their several stories of fire, or wave, or terrible convulsion, and told them simply and clearly; but here was a story not clearly told. It summoned up doubtful, ever-shifting visions,--now of a vast ice continent, ab.u.t.ting on this far isle of the Hebrides from the Pole, and trampling heavily over it,--now of the wild rush of a turbid, mountain-high flood breaking in from the west, and hurling athwart the torn surface, rocks, and stones, and clay,--now of a dreary ocean rising high along the hills, and bearing onward with its winds and currents, huge icebergs, that now brushed the mountain-sides, and now grated along the bottom of the submerged valleys. The inscription on the polished surfaces, with its careless mixture of groove and scratch, is an inscription of very various readings.

We pa.s.sed along a transverse hollow, and then began to ascend a hill-side, from the ridge of which the water sheds to the opposite sh.o.r.e of the island, and on which we catch our first glimpse of Scuir More, standing up over the sea, like a pyramid shorn of its top. A brown lizard, nearly five inches in length, startled by our approach, ran hurriedly across the path; and our guide, possessed by the general Highland belief that the creature is poisonous, and injures cattle, struck at it with a switch, and cut it in two immediately behind the hinder legs. The upper half, containing all that anatomists regard as the vitals, heart, brain, and viscera, all the main nerves, and all the larger arteries, lay stunned by the blow, as if dead; nor did it manifest any signs of vitality so long as we remained beside it; whereas the lower half, as if the whole life of the animal had retired into _it_, continued dancing upon the moss for a full minute after, like a young eel scooped out of some stream, and thrown upon the bank; and then lay wriggling and palpitating for about half a minute more. There are few things more inexplicable in the province of the naturalist than the phenomenon of what may be termed divided life,--vitality broken into two, and yet continuing to exist as vitality in both the dissevered pieces. We see in the n.o.bler animals mere glimpses of the phenomenon,--mere indications of it, doubtfully apparent for at most a few minutes. The blood drawn from the human arm by the lancet continues to live in the cup until it has cooled and begun to coagulate; and when head and body have parted company under the guillotine, both exhibit for a brief s.p.a.ce such unequivocal signs of life, that the question arose in France during the horrors of the Revolution, whether there might not be some glimmering of consciousness attendant at the same time on the fearfully opening and shutting eyes and mouth of the one, and the beating heart and jerking neck of the other. The lower we descend in the scale of being, the more striking the instances which we receive of this divisibility of the vital principle. I have seen the two halves of the heart of a ray pulsating for a full quarter of an hour after they had been separated from the body and from each other. The blood circulates in the hind leg of a frog for many minutes after the removal of the heart, which meanwhile keeps up an independent motion of its own.

Vitality can be so divided in the earthworm, that, as demonstrated by the experiments of Spalanzani, each of the severed parts carries life enough away to set it up as an independent animal; while the polypus, a creature of still more imperfect organization, and with the vivacious principle more equally diffused over it, may be multiplied by its pieces nearly as readily as a gooseberry bush by its slips. It was sufficiently curious, however, to see, in the case of this brown lizard, the least vital half of the creature so much more vivacious, apparently, than the half which contained the heart and brain. It is not improbable, however, that the presence of these organs had only the effect of rendering the upper portion which contained them more capable of being thrown into a state of insensibility. A blow dealt one of the vertebrata on the head at once renders it insensible. It is after this mode the fisherman kills the salmon captured in his wear, and a single blow, when well directed, is always sufficient; but no single blow has the same effect on the earthworm; and here it was vitality in the inferior portion of the reptile,--the earthworm portion of it, if I may so speak,--that refused to partic.i.p.ate in the state of syncope into which the vitality of the superior portion had been thrown. The nice and delicate vitality of the brain seems to impart to the whole system in connection with it an apt.i.tude for dying suddenly,--a susceptibility of instant death, which would be wanting without it. The heart of the rabbit continues to beat regularly long after the brain has been removed by careful excision, if respiration be artificially kept up; but if, instead of amputating the head, the brain be crushed in its place by a sudden blow of a hammer, the heart ceases its motion at once. And such seemed to be the principle ill.u.s.trated here. But why the agonized dancing on the sward of the inferior part of the reptile?--why its after painful writhing and wriggling? The young eel scooped from the stream, whose motions it resembled, is impressed by terror, and can feel pain; was _it_ also impressed by terror, or susceptible of suffering? We see in the case of both exactly the same signs,--the dancing, the writhing, the wriggling; but are we to interpret them after the same manner? In the small red-headed earthworm divided by Spalanzani, that in three months got upper extremities to its lower part, and lower extremities, in as many weeks, to its upper part, the dividing blow must have dealt duplicate feelings,--pain and terror to the portion below, and pain and terror to the portion above,--so far, at least, as a creature so low in the scale was susceptible of these feelings; but are we to hold that the leaping, wriggling tail of the reptile possessed in any degree a similar susceptibility? _I_ can propound the riddle, but who shall resolve it?

It may be added, that this brown lizard was the only recent saurian I chanced to see in the Hebrides, and that, though large for its kind, its whole bulk did not nearly equal that of a single vertebral joint of the fossil saurians of Eigg. The reptile, since his deposition from the first place in the scale of creation, has sunk sadly in those parts: the ex-monarch has become a low plebeian.

We came down upon the coast through a swampy valley, terminating in the interior in a frowning wall of basalt, and bounded on the south, where it opens to the sea, by the Scuir More. The Scuir is a precipitous mountain, that rises from twelve to fifteen hundred feet direct over the beach. M'Culloch describes it as inaccessible, and states that it is only among the debris at its base that its heliotropes can be procured; but the distinguished mineralogist must have had considerably less skill in climbing rocks than in describing them, as, indeed, some of his descriptions, though generally very admirable, abundantly testify. I am inclined to infer from his book, after having pa.s.sed over much of the ground which he describes, that he must have been a man of the type so well hit off by Burns in his portrait of Captain Grose,--round, rosy, short-legged, quick of eye but slow of foot, quite as indifferent a climber as Bailie Nicol Jarvie, and disposed at times, like the elderly gentleman drawn by Crabbe, to prefer the view at the hill-foot to the prospect from its summit. I found little difficulty in scaling the sides of Scuir More for a thousand feet upwards,--in one part by a route rarely attempted before,--and in ensconcing myself among the bloodstones. They occur in the amygdaloidal trap of which the upper part of the hill is mainly composed, in great numbers, and occasionally in bulky ma.s.ses; but it is rare to find other than small specimens that would be recognized as of value by the lapidary. The inclosing rock must have been as thickly vesicular in its original state as the scoria of a gla.s.s-house; and all the vesicles, large and small, like the retorts and receivers of a laboratory, have been vessels in which some curious chemical process has been carried on. Many of them we find filled with a white semi-translucent or opaque chalcedony; many more with a pure green earth, which, where exposed to the bleaching influences of the weather, exhibits a fine verdigris hue, but which in the fresh fracture is generally of an olive green, or of a brownish or reddish color. I have never yet seen a rock in which this earth was so abundant as in the amygdaloid of Scuir More. For yards together in some places we see it projecting from the surface in round globules, that very much resemble green peas, and that occur as thickly in the inclosing ma.s.s as pebbles in an Old Red Sandstone conglomerate. The heliotrope has formed among it in centres, to which the chalcedony seems to have been drawn, as if by molecular attraction. We find a ma.s.s, varying from the size of a walnut to that of a man's head, occupying some larger vesicle or crevice of the amygdaloid, and all the smaller vesicles around it, for an inch or two, filled with what we may venture to term satellite heliotropes, some of them as minute as grains of wild mustard, and all of them more or less earthy, generally in proportion to their distance from the first formed heliotrope in the middle. No one can see them in their place in the rock, with the abundant green earth all around, and the chalcedony, in its uncolored state, filling up so many of the larger cavities, without acquiescing in the conclusion respecting the origin of the gem first suggested by Werner, and afterwards adopted and ill.u.s.trated by M'Culloch. The heliotrope is merely a chalcedony, stained in the forming with an infusion of green earth, as the colored waters in the apothecary's window are stained by the infusions, vegetable and mineral, from which they derive their ornamental character. The red mottlings which so heighten the beauty of the stone occur in comparatively few of the specimens of Scuir More. They are minute jasperous formations, independent of the inclosing ma.s.s; and, from their resemblance to streaks and spots of blood, suggest the name by which the heliotrope is popularly known. I succeeded in making up, among the crags, a set of specimens curiously ill.u.s.trative of the origin of the gem. One specimen consists of white, uncolored chalcedony; a second, of a rich verdigris-hued green earth; a third, of chalcedony barely tinged with green; a fourth, of chalcedony tinged just a shade more deeply; a fifth, tinged more deeply still; a sixth, of a deep green on one side, and scarce at all colored on the other; and a seventh, dark and richly toned,--a true bloodstone,--thickly streaked and mottled with red jasper. In the chemical process that rendered the Scuir More a mountain of gems there were two deteriorating circ.u.mstances, which operated to the disadvantage of its larger heliotropes: the green earth, as if insufficiently stirred in the mixing, has gathered, in many of them, into minute soft globules, like air-bubbles in gla.s.s, that render them valueless for the purposes of the lapidary, by filling them all over with little cavities; and in not a few of the others, an infiltration of lime, that refused to incorporate with the chalcedonic ma.s.s, exists in thin gla.s.sy films and veins, that, from their comparative softness, have a nearly similar effect with the impalpable green earth in roughing the surface under the burnisher.

We find figured by M'Culloch, in his "Western Islands," the internal cavity of a pebble of Scuir More, which he picked up on the beach below, and which had been formed evidently within one of the larger vesicles of the amygdaloid. He describes it as curiously ill.u.s.trative of a various chemistry; the outer crust is composed of a pale-zoned agate, inclosing a cavity, from the upper side of which there depends a group of chalcedonic stalact.i.tes, some of them, as in ancient spar caves, reaching to the floor; and bearing on its under side a large crystal of carbonate of lime, that the longer stalact.i.tes pa.s.s through. In the vesicle in which this hollow pebble was formed three consecutive processes must have gone on. First, a process of infiltration coated the interior all around with layer after layer, now of one mineral substance, now of another, as a plasterer coats over the sides and ceiling of a room with successive layers of lime, putty, and stucco; and had this process gone on, the whole cell would have been filled with a pale-zoned agate. But it ceased, and a new process began. A chalcedonic infiltration gradually entered from above; and, instead of coating over the walls, roof, and floor, it hardened into a group of spear-like stalact.i.tes, that lengthened by slow degrees, till some of them had traversed the entire cavity from top to bottom. And then this second process ceased like the first, and a third commenced. An infiltration of lime took place; and the minute calcareous molecules, under the influence of the law of crystallization, built themselves up on the floor into a large smooth-sided rhomb, resembling a closed sarcophagus resting in the middle of some Egyptian cemetery. And then, the limestone crystal completed, there ensued no after change. As shown by some other specimens, however, there was a yet farther process: a pure quartzose deposition took place, that coated not a few of the calcareous rhombs with sprigs of rock-crystal. I found in the Scuir More several cellular agates in which similar processes had gone on,--none of them quite so fine, however, as the one figured by M'Culloch; but there seemed no lack of evidence regarding the strange and multifarious chemistry that had been carried on in the vesicular cavities of this mountain, as in the retorts of some vast laboratory. Here was a vesicle filled with green earth,--there a vesicle filled with calcareous spar,--yonder a vesicle crusted round on a thin chalcedonic sh.e.l.l with rock-crystal,--in one cavity an agate had been elaborated, in another a heliotrope, in a third a milk-white chalcedony, in a fourth a jasper. On what principle, and under what direction, have results so various taken place in vesicles of the same rock, that in many instances occur scarce half an inch apart?

Why, for instance, should that vesicle have elaborated only green earth, and the vesicle separated from it by a part.i.tion barely a line in thickness, have elaborated only chalcedony? Why should this chamber contain only a quartzose compound of oxygen and silica, and that second chamber beside it contain only a calcareous compound of lime and carbonic acid? What law directed infiltrations so diverse to seek out for themselves vesicles in such close neighborhood, and to keep, in so many instances, each to his own vesicle? I can but state the problem,--not solve it. The groups of heliotropes cl.u.s.tered each around its bulky centrical ma.s.s seem to show that the principle of molecular attraction may be operative in very dense mediae,--in a hard amygdaloidal trap even; and it seems not improbable, that to this law, which draws atom to its kindred atom, as clansmen of old used to speed at the mustering signal to their gathering place, the various chemistry of the vesicles may owe its variety.

I shall attempt stating the chemical problem furnished by the vesicles here in a mechanical form. Let us suppose that every vesicle was a chamber furnished with a door, and that beside every door there watched, as in the draught doors of our coal-pits, some one to open and shut it, as circ.u.mstances might require. Let us suppose further, that for a certain time an infusion of green earth pervaded the surrounding ma.s.s, and percolated through it, and that every door was opened to receive a portion of the infusion. We find that no vesicle wants its coating of this earthy mineral. The coating received, however, one-half the doors shut, while the other half remained agap, and filled with green earth entirely. Next followed a series of alternate infusions of chalcedony, jasper, and quartz; many doors opened and received some two or three coatings, that form around the vesicles skull-like sh.e.l.ls of agate, and then shut; a few remained open, and became as entirely occupied with agate as many of the previous ones had become filled with green earth.

Then an ample infusion of chalcedony pervaded the ma.s.s. Numerous doors again opened; some took in a portion of the chalcedony, and then shut; some remained open, and became filled with it; and many more that had been previously filled by the green earth opened their doors again, and the chalcedony pervading the green porous ma.s.s, converted it into heliotrope. Then an infusion of lime took place. Doors opened, many of which had been hitherto shut, save for a short time, when the green earth infusion obtained, and became filled with lime; other doors opened for a brief s.p.a.ce, and received lime enough to form a few crystals. Last of all, there was a pure quartzose infusion, and doors opened, some for a longer time, some for a shorter, just as on previous occasions. Now, by mechanical means of this character,--by such an arrangement of successive infusions, and such a device of shutting and opening of doors,--the phenomena exhibited by the vesicles could be produced. There is no difficulty in working the problem mechanically, if we be allowed to a.s.sume in our data successive infusions, well-fitted doors, and watchful door-keepers; and if any one can work it chemically,--certainly without door-keepers, but with such doors and such infusions as he can show to have existed,--he shall have cleared up the mystery of the Scuir More. I have given their various cargoes to all its many vesicles by mechanical means, at no expense of ingenuity whatever. Are there any of my readers prepared to give it to them by means purely chemical?

There is a solitary house in the opening of the valley, over which the Scuir More stands sentinel,--a house so solitary, that the entire breadth of the island intervenes between it and the nearest human dwelling. It is inhabited by a shepherd and his wife,--the sole representatives in the valley of a numerous population, long since expatriated to make way for a few flocks of sheep, but whose ranges of little fields may still be seen green amid the heath on both sides, for nearly a mile upwards from the opening. After descending along the precipices of the Scuir, we struck across the valley, and, on scaling the opposite slope sat down on the summit to rest us, about a hundred yards over the house of the shepherd. He had seen us from below, when engaged among the bloodstones, and had seen, withal, that we were not coming his way; and, "on hospitable thoughts intent," he climbed to where we sat, accompanied by his wife, she bearing a vast bowl of milk, and he a basket of bread and cheese. And we found the refreshment most seasonable, after our long hours of toil, and with a rough journey still before us. It is an excellent circ.u.mstance, that hospitality grows best where it is most needed. In the thick of men it dwindles and disappears, like fruits in the thick of a wood; but where man is planted spa.r.s.ely, it blossoms and matures, like apples on a standard or espalier. It flourishes where the inn and the lodging-house cannot exist, and dies out where they thrive and multiply.

We reached the cross valley in the interior of the island about half an hour before sunset. The evening was clear, calm, golden-tinted; even wild heaths and rude rocks had a.s.sumed a flush of transient beauty; and the emerald-green patches on the hill-sides, barred by the plough lengthwise, diagonally, and transverse, had borrowed an aspect of soft and velvety richness, from the mellowed light and the broadening shadows. All was solitary. We could see among the deserted fields the gra.s.s-grown foundations of cottages razed to the ground; but the valley, more desolate than that which we had left, had not even its single inhabited dwelling: it seemed as if man had done with it forever. The island, eighteen years before, had been divested of its inhabitants, amounting at the time to rather more than four hundred souls, to make way for one sheep-farmer and eight thousand sheep. All the aborigines of Rum crossed the Atlantic; and at the close of 1828, the entire population consisted of but the sheep-farmer, and a few shepherds, his servants; the island of Rum reckoned up scarce a single family at this period for every five square miles of area which it contained. But depopulation on so extreme a scale was found inconvenient; the place had been rendered too thoroughly a desert for the comfort of the occupant; and on the occasion of a clearing which took place shortly after in Skye, he accommodated some ten or twelve of the ejected families with sites for cottages, and pasturage for a few cows, on the bit of mora.s.s beside Loch Scresort, on which I had seen their humble dwellings. But the whole of the once-peopled interior remains a wilderness, without inhabitant,--all the more lonely in its aspect from the circ.u.mstance that the solitary valleys, with their plough-furrowed patches, and their ruined heaps of stone, open upon sh.o.r.es every whit as solitary as themselves, and that the wide untrodden sea stretches drearily around.

The armies of the insect world were sporting in the light this evening by millions; a brown stream that runs through the valley yielded an incessant popling sound, from the myriads of fish that were ceaselessly leaping in the pools, beguiled by the quick glancing wings of green and gold that fluttered over them; along a distant hill-side there ran what seemed the ruins of a gray-stone fence, erected, says tradition, in a remote age, to facilitate the hunting of the deer; there were fields on which the heath and moss of the surrounding moorlands were fast encroaching, that had borne many a successive harvest; and prostrate cottages, that had been the scenes of christenings, and bridals, and blythe new-year's days;--all seemed to bespeak the place a fitting habitation for man, in which not only the necessaries, but also a few of the luxuries of life, might be procured; but in the entire prospect not a man nor a man's dwelling could the eye command. The landscape was one without figures. I do not much like extermination carried out so thoroughly and on system;--it seems bad policy; and I have not succeeded in thinking any the better of it though a.s.sured by economists that there are more than people enough in Scotland still. There are, I believe, more than enough in our workhouses,--more than enough on our pauper-rolls,--more than enough huddled up, disreputable, useless, and unhappy, in the miasmatic alleys and typhoid courts of our large towns; but I have yet to learn how arguments for local depopulation are to be drawn from facts such as these. A brave and hardy people, favorably placed for the development of all that is excellent in human nature, form the glory and strength of a country;--a people sunk into an abyss of degradation and misery, and in which it is the whole tendency of external circ.u.mstances to sink them yet deeper, const.i.tute its weakness and its shame; and I cannot quite see on what principle the ominous increase which is taking place among us in the worse cla.s.s, is to form our solace or apology for the wholesale expatriation of the better. It did not seem as if the depopulation of Rum had tended much to any one's advantage. The single sheep-farmer who had occupied the holdings of so many had been unfortunate in his speculations, and had left the island: the proprietor, his landlord, seemed to have been as little fortunate as the tenant, for the island itself was in the market; and a report went current at the time, that it was on the eve of being purchased by some wealthy Englishman, who purposed converting it into a deer-forest. How strange a cycle! Uninhabited originally save by wild animals, it became at an early period a home of men, who, as the gray wall on the hill-side testified, derived, in part at least, their sustenance from the chase.

They broke in from the waste the furrowed patches on the slopes of the valleys,--they reared herds of cattle and flocks of sheep,--their number increased to nearly five hundred souls,--they enjoyed the average happiness of human creatures in the present imperfect state of being,--they contributed their portion of hardy and vigorous manhood to the armies of the country,--and a few of their more adventurous spirits, impatient of the narrow bounds which confined them, and a course of life little varied by incident, emigrated to America. Then came the change of system so general in the Highlands; and the island lost all its original inhabitants, on a wool and mutton speculation,--inhabitants, the descendants of men who had chased the deer on its hills five hundred years before, and who, though they recognized some wild island lord as their superior, and did him service, had regarded the place as indisputably their own. And now yet another change was on the eve of ensuing, and the island was to return to its original state, as a home of wild animals, where a few hunters from the mainland might enjoy the chase for a month or two every twelvemonth, but which could form no permanent place of human abode. Once more, a strange and surely most melancholy cycle!

There was light enough left, as we reached