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The day passed pleasantly in the work of exploration and discovery; the sun had already declined far in the west; and, bearing with us our better fossils, we set out, on our return, by the opposite route to that along the Bay of Laig, which we had now thrice walked over. The grassy talus so often mentioned continues to run on the eastern side of the island for about six miles, between the sea and the inaccessible rampart of precipice behind. It varies in breadth from about two to four hundred yards; the rampart rises over it from three to five hundred feet; and a noble expanse of sea, closed in the distance by a still nobler curtain of blue hills, spreads away from its base: and it was along this grassy talus that our homeward road lay. Let the Edinburgh reader imagine the fine walk under Salisbury Crags lengthened some twenty times,—the line of precipices above heightened some five or six times,—the gravelly slope at the base not much increased in altitude, but developed transversely into a green undulating belt of hilly pasture, with here and there a sunny slope level enough for the plough, and here and there a rough wilderness of detached crags and broken banks; let him further imagine the sea sweeping around the base of this talus, with the nearest opposite land—bold, bare and undulating atop—some six or eight miles distant; and he will have no very inadequate idea of the peculiar and striking scenery through which, this evening, our homeward route lay. I have scarce ever walked over a more solitary tract. The sea shuts it in on the one hand, and the rampart of rocks on the other; there occurs along its entire length no other human dwelling than a lonely summer shieling; for full one-half the way we saw no trace of man; and the wildness of the few cattle which we occasionally startled in the hollows showed us that man was no very frequent visitor among them. About half an hour before sunset we reached the midway shieling.
Rarely have I seen a more interesting spot, or one that, from its utter loneliness, so impressed the imagination. The shieling, a rude low-roofed erection of turf and stone, with a door in the centre some five feet in height or so, but with no window, rose on the grassy slope immediately in front of the vast continuous rampart. A slim pillar of smoke ascends from the roof, in the calm, faint and blue within the shadow of the precipice, but it caught the sunlight in its ascent, and blushed, ere it melted into the ether, a ruddy brown. A streamlet came pouring from above in a long white thread, that maintained its continuity unbroken for at least two-thirds of the way; and then, untwisting into a shower of detached drops, that pattered loud and vehemently in a rocky recess, it again gathered itself up into a lively little stream, and, sweeping past the shieling, expanded in front into a circular pond, at which a few milch cows were leisurely slaking their thirst. The whole grassy talus, with a strip mayhap a hundred yards wide, of deep green sea, lay within the shadow of the tall rampart; but the red light fell, for many a mile beyond, on the glassy surface; and the distant Cuchullin Hills, so dark at other times, had all their prominent slopes and jutting precipices tipped with bronze; while here and there a mist streak, converted into bright flame, stretched along their peaks or rested on their sides. Save the lonely shieling, not a human dwelling was in sight. An island girl of eighteen, more than merely good-looking, though much embrowned by the sun, had come to the door to see who the unwonted visitors might be, and recognized in John Stewart an old acquaintance. John informed her in her own language that I was Mr. Swanson's sworn friend, and not a Moderate, but one of their own people, and that I had fasted all day, and had come for a drink of milk. The name of her minister proved a strongly recommendatory one: I have not yet seen the true Celtic interjection of welcome,—the kindly "O o o,"—attempted on paper; but I had a very agreeable specimen of it on this occasion, viva voce. And as she set herself to prepare for us a rich bowl of mingled milk and cream, John and I entered the shieling. There was a turf fire at the one end, at which there sat two little girls, engaged in keeping up the blaze under a large pot, but sadly diverted from their work by our entrance; while the other end was occupied by a bed of dry straw, spread on the floor from wall to wall, and fenced off at the foot by a line of stones. The middle space was occupied by the utensils and produce of the dairy,—flat wooden vessels of milk, a butter-churn, and a tub half-filled with curd; while a few cheeses, soft from the press, lay on a shelf above. The little girls were but occasional visitors, who had come, out of a juvenile frolic, to pass the night in the place; but I was informed by John that the shieling had two other inmates, young women, like the one so hospitably engaged in our behalf, who were out at the milking, and that they lived here all alone for several months every year, when the pasturage was at its best, employed in making butter and cheese for their master, worthy Mr. M'Donald of Keill. They must often feel lonely when night has closed darkly over mountain and sea, or in those dreary days of mist and rain so common in the Hebrides, when nought may be seen save the few shapeless crags that stud the nearer hillocks around them, and nought heard save the moaning of the wind in the precipices above, or the measured dash of the wave on the wild beach below. And yet they would do ill to exchange their solitary life and rude shieling for the village dwellings and gregarious habits of the females who ply their rural labors in bands among the rich fields of the Lowlands, or for the unwholesome backroom and weary task-work of the city seamstress. The sunlight was fading from the higher hill-tops of Skye and Glenelg as we bade farewell to the lonely shieling and the hospitable island girl.
The evening deepened as we hurried southwards along the scarce visible pathway, or paused for a few seconds to examine some shattered block, bulky as a Highland cottage, that had fallen from the precipice above. Now that the whole landscape lay equally in shadow, one of the more picturesque peculiarities of the continuous rampart came out more strongly as a feature of the scene than when a strip of shade rested along the face of the rock, imparting to it a retiring character, and all was sunshine beyond. A thick bed of white sandstone, as continuous as the rampart itself, runs nearly horizontally about midway in the precipice for mile after mile, and, standing out in strong contrast with the dark-colored trap above and below, reminds one of a belt of white hewn work in a basalt house front, or rather,—for there occurs above a second continuous strip, of an olive hue, the color assumed, on weathering by a bed of amygdaloid,—of a piece of dingy old-fashioned furniture, inlaid with one stringed belt of bleached holly, and another of faded green-wood. At some of the more accessible points I climbed to the line of white belting, and found it to consist of the same soft quartzy sandstone that in the Bay of Laig furnishes the musical sand. Lower down there occur, alternating with the trap, beds of shale and of blue clay, but they are lost mostly in the talus. Ill adapted to resist the frosts and rains of winter, their exposed edges have mouldered into a loose soil, now thickly covered over with herbage; and, but for the circumstance that we occasionally find them laid bare by a water-course, we would scarce be aware of their existence at all. The shale exhibits everywhere, as on the opposite side of the Ru-Stoir, faint impressions of a minute shell resembling a Cyclas, and ill-preserved fragments of fish-scales. The blue clay I found at one spot where the pathway had cut deep into the hill-side, richly charged with bivalves of the species I had seen so abundant in the resembling clay of the Bay of Laig; but the closing twilight prevented me from ascertaining whether it also contained the characteristic univalves of the deposit, and whether its shells,—for they seem identical with those of the altered shales of the Ru-Stoir,—might not be associated, like these, with reptilian remains. Night fell fast, and the streaks of mist that had mottled the hills at sunset began to spread gray over the heavens in a continuous curtain; but there was light enough left to show me that the trap became more columnar as we neared our journey's end. One especial jutting in the rock presented in the gloom the appearance of an ancient portico, with pediment and cornice, such as the traveller sees on the hill-sides of Petraea in front of some old tomb; but it may possibly appear less architectural by day. At length, passing from under the long line of rampart, just as the stars that had begun to twinkle over it were disappearing, one after one, in the thickening vapor, we reached the little bay of Kildonan, and found the boat waiting us on the beach. My friend the minister, as I entered the cabin, gathered up his notes from the table, and gave orders for the tea-kettle; and I spread out before him—a happy man—an array of fossils new to Scotch Geology. No one not an enthusiastic geologist or a zealous Roman Catholic can really know how vast an amount of interest may attach to a few old bones. Has the reader ever heard how fossil relics once saved the dwelling of a monk, in a time of great general calamity, when all his other relics proved of no avail whatever?
Thomas Campbell, when asked for a toast in a society of authors, gave the memory of Napoleon Bonaparte; significantly adding, "he once hung a bookseller." On a nearly similar principle I would be disposed to propose among geologists a grateful bumper in honor of the revolutionary army that besieged Maestricht. That city, some seventy-five or eighty years ago, had its zealous naturalist in the person of M. Hoffmann, a diligent excavator in the quarries of St. Peter's mountain, long celebrated for its extraordinary fossils. Geology, as a science, had no existence at the time; but Hoffmann was doing, in a quiet way, all he could to give it a beginning;—he was transferring from the rock to his cabinet, shells, and corals, and crustacea, and the teeth and scales of fishes, with now and then the vertebrae, and now and then the limb-bone, of a reptile. And as he honestly remunerated all the workmen he employed, and did no manner of harm to any one, no one heeded him. On one eventful morning, however, his friends the quarriers laid bare a most extraordinary fossil,—the occipital plates of an enormous saurian, with jaws four and a half feet long, bristling over with teeth, like chevaux de frise; and after Hoffmann, who got the block in which it lay embedded, cut out entire, and transferred to his house, had spent week after week in painfully relieving it from the mass, all Maestricht began to speak of it as something really wonderful. There is a cathedral on St. Peter's mountain,—the mountain itself is church-land; and the lazy canon, awakened by the general talk, laid claim to poor Hoffmann's wonderful fossil as his property. He was lord of the manor, he said, and the mountain and all that it contained belonged to him. Hoffmann defended his fossil as he best could in an expensive lawsuit; but the judges found the law clean against him; the huge reptile head was declared to be "treasure trove" escheat to the lord of the manor; and Hoffmann, half broken-hearted, with but his labor and the lawyer's bills for his pains, saw it transferred by rude hands from its place in his museum, to the residence of the grasping churchman. The huge fossil head experienced the fate of Dr. Chalmer's two hundred churches. Hoffmann was a philosopher, however, and he continued to observe and collect as before; but he never found such another fossil; and at length, in the midst of his ingenious labors, the vital energies failed within him, and he broke down and died. The useless canon lived on. The French Revolution broke out; the republican army invested Maestricht; the batteries were opened; and shot and shell fell thick on the devoted city. But in one especial quarter there alighted neither shot nor shell. All was safe around the canon's house. Ordinary relics would have availed him nothing in the circumstances,—no, not "the three kings of Cologne," had he possessed the three kings entire, or the jaw-bones of the "eleven thousand virgins;" but there was virtue in the jaw-bones of the Mosasaurus, and safety in their neighborhood. The French savans, like all the other savans of Europe, had heard of Hoffmann's fossil, and the French artillery had been directed to play wide of the place where it lay. Maestricht surrendered; the fossil was found secreted in a vault, and sent away to the Jardin des Plantes at Paris, maugre the canon, to delight there the heart of Cuvier; and the French, generously addressing themselves to the heirs of Hoffmann as its legitimate owners, made over to them a considerable sum of money as its price. They reversed the finding of the Maestricht judges; and all save the monks of St. Peter's have acquiesced in the justice of the decision.
CHAPTER VI.
Something for Non-geologists—Man Destructive—A Better and Last Creation coming—A Rainy Sabbath—The Meeting House—The Congregation—The Sermon in Gaelic—The Old Wondrous Story—The Drunken Minister of Eigg—Presbyterianism without Life—Dr. Johnson's Account of the Conversion of the People of Rum—Romanism at Eigg—The Two Boys—The Freebooter of Eigg—Voyage Resumed—The Homeless Minister—Harbor of Isle Ornsay—Interesting Gneiss Deposit—A Norwegian Keep—Gneiss at Knock—Curious Chemistry—Sea-cliffs beyond Portsea—The Goblin Luidag—Scenery of Skye.
I reckon among my readers a class of non-geologists, who think my geological chapters would be less dull if I left out the geology; and another class of semi-geologists, who say there was decidedly too much geology in my last. With the present chapter, as there threatens to be an utter lack of science in the earlier half of it, and very little, if any, in the latter half, I trust both classes may be in some degree satisfied. It will bear reference to but the existing system of things,—assuredly not the last of the consecutive creations,—and to a species of animal that, save in the celebrated Guadaloupe specimens, has not yet been found locked up in stone. There have been much of violence and suffering in the old immature stages of being,—much, from the era of the Holoptychius, with its sharp murderous teeth and strong armor of bone, down to that of the cannibal Ichthyosaurus, that bears the broken remains of its own kind in its bowels,—much, again, from the times of the crocodile of the Oolite, down to the times of the fossil hyena and gigantic shark of the Tertiary. Nor, I fear, have matters greatly improved in that latest-born creation in the series, that recognizes as its delegated lord the first tenant of earth accountable to his Maker. But there is a better and a last creation coming, in which man shall re-appear, not to oppress and devour his fellow-men, and in which there shall be no such wrongs perpetrated as it is my present purpose to record,—"new heavens and a new earth, wherein dwelleth righteousness." Well sung the Ayrshire ploughman, when musing on the great truth that the present scene of being "is surely not the last,"—a truth corroborated since his day by the analogies of a new science,—
"The poor, oppressed, honest man, Had never sure been born, Had not there been some recompense To comfort those that mourn."
It was Sabbath, but the morning rose like a hypochondriac wrapped up in his night-clothes,—gray in fog, and sad with rain. The higher grounds of the island lay hid in clouds, far below the level of the central hollow; and our whole prospect from the deck was limited to the nearer slopes, dank, brown, and uninhabited, and to the rough black crags that frown like sentinels over the beach. Now the rime thickened as the rain pattered more loudly on the deck; and even the nearer stacks and precipices showed as unsolid and spectral in the cloud as moonlight shadows thrown on a ground of vapor; anon it cleared up for a few hundred yards, as the shower lightened; and then there came in view, partially at least, two objects that spoke of man,—a deserted boat harbor, formed of loosely piled stone, at the upper extremity of a sandy bay; and a roofless dwelling beside it, with two ruinous gables rising over the broken walls. The entire scene suggested the idea of a land with which man had done for ever;—the vapor-enveloped rocks,—the waste of ebb-uncovered sand,—the deserted harbor,—the ruinous house,—the melancholy rain-fretted tides eddying along the strip of brown tangle in the foreground,—and, dim over all, the thick, slant lines of the beating shower!—I know not that of themselves they would have furnished materials enough for a finished picture in the style of Hogarth's "End of all Things;" but right sure am I that in the hands of Bewick they would have been grouped into a tasteful and poetic vignette. We set out for church a little after eleven,—the minister encased in his ample-skirted storm-jacket of oiled canvas, and protected atop by a genuine sou-wester, of which the broad posterior rim eloped half a yard down his back; and I closely wrapped up in my gray maud, which proved, however, a rather indifferent protection against the penetrating powers of a true Hebridean drizzle. The building in which the congregation meets is a low dingy cottage of turf and stone, situated nearly opposite to the manse windows. It had been built by my friend, previous to the Disruption, at his own expense, for a Gaelic school, and it now serves as a place of worship for the people.
We found the congregation already gathered, and that the very bad morning had failed to lessen their numbers. There were a few of the male parishioners keeping watch at the door, looking wistfully out through the fog and rain for their minister; and at his approach nearly twenty more came issuing from the place,—like carder bees from their nest of dried grass and moss,—to gather round him, and shake him by the hand. The islanders of Eigg are an active, middle-sized race, with well-developed heads, acute intellects, and singularly warm feelings. And on this occasion at least there could be no possibility of mistake respecting the feelings with which they regarded their minister. Rarely have I seen human countenances so eloquently vocal with veneration and love. The gospel message, which my friend had been the first effectually to bring home to their hearts,—the palpable fact of his sacrifice for the sake of the high principles which he has taught,—his own kindly disposition,—the many services which he has rendered them, for not only has he been the minister, but also the sole medical man, of the Small Isles, and the benefit of his practice they have enjoyed, in every instance, without fee or reward,—his new life of hardship and danger, maintained for their sakes amid sinking health and great privation,—their frequent fears for his safety when stormy nights close over the sea,—and they have seen his little vessel driven from her anchorage, just as the evening has fallen,—all these are circumstances that have concurred in giving him a strong hold on their affections.
The rude turf-building we found full from end to end, and all a-steam with a particularly wet congregation, some of whom, neither very robust nor young, had travelled in the soaking drizzle from the farther extremities of the island. And, judging from the serious attention with which they listened to the discourse, they must have deemed it full value for all it cost them. I have never yet seen a congregation more deeply impressed, or that seemed to follow the preacher more intelligently; and I was quite sure, though ignorant of the language in which my friend addressed them, that he preached to them neither heresy nor nonsense. There was as little of the reverence of externals in the place as can well be imagined: an uneven earthen floor,—turf-walls on every side, and a turf-roof above,—two little windows of four panes a-piece, adown which the rain-drops were coursing thick and fast,—a pulpit grotesquely rude, that had never employed the bred carpenter,—and a few ranges of seats of undressed deal, such were the mere materialisms of this lowly church of the people; and yet here, notwithstanding, was the living soul of a Christian community,—understandings convinced of the truth of the gospel, and hearts softened and impressed by its power.
My friend, at the conclusion of his discourse, gave a brief digest of its contents in English, for the benefit of his one Saxon auditor; and I found, as I had anticipated, that what had so moved the simple islanders was just the old wondrous story, which, though repeated and re-repeated times beyond number, from the days of the apostles till now, continues to be as full of novelty and interest as ever,—"God so loved the world, that he gave his only begotten Son, that whosoever believeth on Him should not perish, but have everlasting life." The great truths which had affected many of these poor people to tears, were exactly those which, during the last eighteen hundred years, have been active in effecting so many moral revolutions in the world, and which must ultimately triumph over all error and all oppression. On this occasion, as on many others, I had to regret my want of Gaelic. It was my misfortune to miss being born to this ancient language, by barely a mile of ferry. I first saw light on the southern shore of the Frith of Cromarty, where the strait is narrowest, among an old established Lowland community, marked by all the characteristics, physical and mental, of the Lowlanders of the southern districts; whereas, had I been born on the northern shore, I would have been brought up among a Celtic tribe, and Gaelic would have been my earliest language. Thus distinct was the line between the two races preserved, even after the commencement of the present century.
In returning to the Betsey during the mid-day interval in the service, we passed the ruinous two-gabled house beside the boat-harbor. During the incumbency of my friend's predecessor, it had been the public-house of the island, and the parish minister was by far its best customer. He was in the practice of sitting in one of its dingy little rooms, day after day, imbibing whisky and peat-reek; and his favorite boon companion on these occasions was a Roman Catholic tenant who lived on the opposite side of the island, and who, when drinking with the minister, used regularly to fasten his horse beside the door, till at length all the parish came to know that when the horse was standing outside the minister was drinking within. In course of time, through the natural gravitation operative in such cases, the poor incumbent became utterly scandalous, and was libelled for drunkenness before the General Assembly; but, as the island of Eigg lies remote from observation, evidence was difficult to procure; and had not the infatuated man got senselessly drunk one evening, when in Edinburgh on his trial, and staggered, of all places in the world, into the General Assembly, he would probably have died minister of Eigg. As the event happened, however, the testimony thus unwittingly furnished in the face of the Court that tried him was deemed conclusive;—he was summarily deposed from his office, and my friend succeeded him. Presbyterianism without the animating life is a poor shrunken thing: it never lies in state when it is dead; for it has no body of fine forms, or trapping of imposing ceremonies, to give it bulk or adornment: without the vitality of evangelism it is nothing; and in this low and abject state my friend found the Presbyterianism of Eigg. His predecessor had done it only mischief; nor had it been by any means vigorous before. Rum is one of the four islands of the parish; and all my readers must be familiar with Dr. Johnson's celebrated account of the conversion to Protestantism of the people of Rum. "The inhabitants," says the Doctor, in his "Journey to the Western Islands," "are fifty-eight families, who continued Papists for some time after the laird became a Protestant. Their adherence to their old religion was strengthened by the countenance of the laird's sister, a zealous Romanist; till one Sunday, as they were going to mass under the conduct of their patroness, Maclean met them on the way, gave one of them a blow on the head with a yellow stick,—I suppose a cane, for which the Erse had no name, and drove them to the kirk, from which they have never departed. Since the use of this method of conversion, the inhabitants of Eigg and Canna who continue Papists call the Protestantism of Rum the religion of the yellow stick." Now, such was the kind of Protestantism that, since the days of Dr. Johnson, had also been introduced, I know not by what means, into Eigg. It had lived on the best possible terms with the Popery of the island; the parish minister had soaked day after day in the public-house with a Roman Catholic boon companion; and when a Papist man married a Protestant woman, the woman, as a matter of course, became Papist also; whereas, when it was the man who was a Protestant, and the woman a Papist, the woman remained what she had been. Roman Catholicism was quite content with terms, actual though not implied, of a kind so decidedly advantageous; and the Roman Catholics used good-humoredly to urge on their neighbors the Protestants, that, as it was palpable they had no religion of any kind, they had better surely come over to them, and have some. In short, all was harmony between the two Churches. My friend labored hard, as a good and honest man ought, to impart to Protestantism in his parish the animating life of the Reformation; and, through the blessing of God, after years of anxious toil, he at length fully succeeded.
I had got wet, and the day continued bad; and so, instead of returning to the evening sermon, which began at six, I remained alone aboard of the vessel. The rain ceased in little more than an hour after, and in somewhat more than two hours I got up on deck to see whether the congregation was not dispersing, and if it was not yet time to hang on the kettle for our evening tea. The unexpected apparition of some one aboard the Free Church yacht startled two ragged boys who were manoeuvring a little boat a stone-cast away, under the rocky shores of Eilean Chaisteil, and who, on catching a glimpse of me, flung themselves below the thwarts for concealment. An oar dropped into the water; there was a hasty arm and half a head thrust over the gunwale to secure it; and then the urchin to whom they belonged again disappeared. Meanwhile the boat drifted slowly away: first one little head would appear for a moment over the gunwale, then another, as if reconnoitering the enemy; but I still kept my place on deck; and at length, tired out, the ragged little crew took to their oars, and rowed into a shallow bay at the lower extremity of the glebe, with a cottage, in size and appearance much resembling an ant-hill, peeping out at its inner extremity among some stunted bushes. I had marked the place before, and had been struck with the peculiarity of the choice that could have fixed on it as a site for a dwelling: it is at once the most inconvenient and picturesque on this side the island. A semi-circular line of columnar precipices, that somewhat resembles an amphitheatre turned outside in,—for the columns that overlook the area are quite as lofty as those which should form the amphitheatre's outer wall,—sweeps round a little bay, flat and sandy at half-tide, but bordered higher up by a dingy, scarce passable beach of columnar fragments that have toppled from above. Between the beach and the line of columns there is a bosky talus, more thickly covered with brushwood than is at all common in the Hebrides, and scarce more passable than the rough beach at its feet. And at the bottom of this talus, with its one gable buried in the steep ascent,—for there is scarce a foot-breadth of platform between the slope and the beach,—and with the other gable projected to the tide-line on rugged columnar masses, stands the cottage. The story of the inmate,—the father of the two ragged boys,—is such a one as Crabbe would have delighted to tell, and as he could have told better than any one else.
He had been, after a sort, a freebooter in his time, but born an age or two rather late; and the law had proved over strong for him. On at least one occasion, perhaps oftener,—for his adventures are not all known in Eigg,—he had been in prison for sheep-stealing. He had the dangerous art of subsisting without the ostensible means, and came to be feared and avoided by his neighbors as a man who lived on them without asking their leave. With neither character nor a settled way of living, his wits, I am afraid, must have been often whetted by his necessities: he stole lest he should starve. For some time he had resided in the adjacent island of Muck; but, proving a bad tenant, he had been ejected by the agent of the landlord, I believe a very worthy man, who gave him half a boll of meal to get quietly rid of him, and pulled down his house, when he had left the island, to prevent his return. Betaking himself, with his boys, to a boat, he set out in quest of some new lodgment. He made his first attempt or two on the mainland, where he strove to drive a trade in begging, but he was always recognized as the convicted sheep-stealer, and driven back to the shore. At length, after a miserable term of wandering, he landed in the winter season on Eigg, where he had a grown-up son, a miller; and, erecting a wretched shed with some spars and the old sail of a boat placed slantways against the side of a rock, he squatted on the beach, determined, whether he lived or died, to find a home on the island. The islanders were no strangers to the character of the poor forlorn creature, and kept aloof from him,—none of them, however, so much as his own son; and, for a time, my friend the minister, aware that he had been the pest of every community among which he had lived, stood aloof from him too, in the hope that at length, wearied out, he might seek for himself a lodgment elsewhere. There came on, however, a dreary night of sleet and rain, accompanied by a fierce storm from the sea; and intelligence reached the manse late in the evening, that the wretched sheep-stealer had been seized by sudden illness, and was dying on the beach. There could be no room for further hesitation in this case; and my friend the minister gave instant orders that the poor creature should be carried to the manse. The party, however, which he had sent to remove him found the task impracticable. The night was pitch dark; and the road, dangerous with precipices, and blocked up with rough masses of rock and stone, they found wholly impassable with so helpless a burden. And so, administering some cordials to the poor, hapless wretch, they had to leave him in the midst of the storm, with the old wet sail flapping about his ears, and the half-frozen rain pouring in upon him in torrents. He must have passed a miserable night, but it could not have been a whit more miserable than that passed by the minister in the manse. As the wild blast howled around his comfortable dwelling, and shook the casements as if some hand outside were assaying to open them, or as the rain pattered sharp and thick on the panes, and the measured roar of the surf rose high over every other sound, he could think of only the wretched creature exposed to the fury of a tempest so terrible, as perchance wrestling in his death agony in the darkness beside the breaking wave, or as already stiffening on the shore. He was early astir next morning, and almost the first person he met was the poor sheep-stealer, looking more like a ghost than a living man. The miserable creature had mustered strength enough to crawl up from the beach. My friend has often met better men with less pleasure. He found a shelter for the poor outcast; he tended him, prescribed for him, and, on his recovery, gave him leave to build for himself the hovel at the foot of the crags. The islanders were aware they had got but an indifferent neighbor through the transaction, though none of them, with the exception of the poor creature's son, saw what else their minister could have done in the circumstances. But the miller could sustain no apology for the arrangement that had given him his vagabond father as a neighbor; and oftener than once the site of the rising hovel became a scene of noisy contention between parent and son. Some of the islanders informed me that they had seen the son engaged in pulling down the stones of the walls as fast as the father raised them up; and, save for the interference of the minister, the hut, notwithstanding the permission he gave, would scarce have been built.
On the morning of Monday we unloosed from our moorings, and set out with a light variable breeze for Isle Ornsay, in Skye, where the wife and family of Mr. Swanson resided, and from which he had now been absent for a full month. The island diminished, and assumed its tint of diluting blue, that waxed paler and paler hour after hour, as we left it slowly behind us; and the Scuir, projected boldly from its steep hill-top, resembled a sharp hatchet-edge presented to the sky. "Nowhere," said my friend, "did I so thoroughly realize the Disruption of last year as at this spot. I had just taken my last leave of the manse; Mrs. Swanson had staid a day behind me in charge of a few remaining pieces of furniture, and I was bearing some of the rest, and my little boy Bill, scarce five years of age at the time, in the yacht with me to Skye. The little fellow had not much liked to part from his mother, and the previous unsettling of all sorts of things in the manse had bred in him thoughts he had not quite words to express. The further change to the yacht, too, he had deemed far from an agreeable one. But he had borne up, by way of being very manly; and he seemed rather amused that papa should now have to make his porridge for him, and to put him to bed, and that it was John Stewart, the sailor, who was to be the servant girl. The passage, however, was tedious and disagreeable; the wind blew a-head, and heart and spirits failing poor Bill, and somewhat sea-sick to boot, he lay down on the floor, and cried bitterly to be taken home. 'Alas, my boy!' I said, 'you have no home now: your father is like the poor sheep-stealer whom you saw on the shore of Eigg.' This view of matters proved in no way consolatory to poor Bill. He continued his sad wail, 'Home, home, home!' until at length he fairly sobbed himself asleep; and I never, on any other occasion, so felt the desolateness of my condition as when the cry of my boy,—'Home, home, home!'—was ringing in my ears."
We passed, on the one hand, Loch Nevis and Loch Hourn, two fine arms of the sea that run far into the mainland, and open up noble vistas among the mountains; and, on the other, the long undulating line of Sleat in Skye, with its intermingled patches of woodland and arable on the coast, and its mottled ranges of heath and rock above. Towards evening we entered the harbor of Isle Ornsay, a quiet, well-sheltered bay, with a rocky islet for a breakwater on the one side, and the rudiments of a Highland village, containing a few good houses, on the other. Half a dozen small vessels were riding at anchor, curtained round, half-mast high, with herring nets; and a fleet of herring-boats lay moored beside them a little nearer the shore. There had been tolerable takes for a few nights in the neighboring sea, but the fish had again disappeared, and the fishermen, whose worn-out tackle gave such evidence of a long-continued run of ill-luck, as I had learned to interpret on the east coast, looked gloomy and spiritless, and reported a deficient fishery. I found Mrs. Swanson and her family located in one of the two best houses in the village, with a neat enclosure in front, and a good kitchen-garden behind. The following day I spent in exploring the rocks of the district,—a primary region with regard to organic existence, "without form and void." From Isle Ornsay to the Point of Sleat, a distance of thirteen miles, gneiss is the prevailing deposit; and in no place in the district are the strata more varied and interesting than in the neighborhood of Knockhouse, the residence of Mr. Elder, which I found pleasingly situated at the bottom of a little open bay, skirted with picturesque knolls partially wooded, that present to the surf precipitous fronts of rock. One insulated eminence, a gun-shot from the dwelling-house, that presents to the sea two mural fronts of precipice, and sinks in steep grassy slopes on two sides more, bears atop a fine old ruin. There is a blind-fronted massy keep, wrapped up in a mantle of ivy, perched at the one end, where the precipice sinks steepest; while a more ruinous though much more modern pile of building, perforated by a double row of windows, occupies the rest of the area. The square keep has lost its genealogy in the mists of the past, but a vague tradition attributes its erection to the Norwegians. The more modern pile is said to have been built about three centuries ago by a younger son of M'Donald of the Isles; but it is added that, owing to the jealousy of his elder brother, he was not permitted to complete or inhabit it. I find it characteristic of most Highland traditions, that they contain speeches: they constitute true oral specimens of that earliest and rudest style of historic composition in which dialogue alternates with narrative. "My wise brother is building a fine house," is the speech preserved in this tradition as that of the elder son: "it is rather a pity for himself that he should be building it on another man's lands." The remark was repeated to the builder, says the story, and at once arrested the progress of the work. Mr. Elder's boys showed me several minute pieces of brass, somewhat resembling rust-eaten coin, that they had dug out of the walls of the old keep; but the pieces bore no impress of the dye, and seemed mere fragments of metal beaten thin by the hammer.
The gneiss at Knock is exceedingly various in its composition, and many of its strata the geologist would fail to recognize as gneiss at all. We find along the precipices its two unequivocal varieties, the schistose and the granitic, passing not unfrequently, the former into a true mica schist, the latter into a pale feldspathose rock, thickly pervaded by needle-like crystals of tremolite, that, from the style of the grouping, and the contrast existing between the dark green of the enclosed mineral, and the pale flesh-color of the ground, frequently furnishes specimens of great beauty. In some pieces the tremolite assumes the common fan-like form; in some, the crystals, lying at nearly right angles with each other, present the appearance of ancient characters inlaid in the rock; in some they resemble the footprints of birds in a thin layer of snow; and in one curious specimen picked up by Mr. Swanson, in which a dark linear strip is covered transversely by crystals that project thickly from both its sides, the appearance presented is that of a minute stigmaria of the Coal Measures, with the leaves, still bearing their original green color, bristling thick around it. Mr. Elder showed me, intercalated among the gneiss strata of a little ravine in the neighborhood of Isle Ornsay, a thin band of a bluish-colored indurated clay, scarcely distinguishable, in the hand specimen, from a weathered clay-stone, but unequivocally a stratum of the rock. I have found the same stone existing, in a decomposed state, as a very tenacious clay, among the gneiss strata of the hill of Cromarty; and oftener than once had I amused myself in fashioning it, with tolerable success, into such rude pieces of pottery as are sometimes found in old sepulchral tumuli. Such are a few of the rocks included in the general gneiss deposit of Sleat. If we are to hold, with one of the most distinguished of living geologists, that the stratified primary rocks are aqueous deposits altered by heat, to how various a chemistry must they not have been subjected in this district! In one stratum, so softened that all its particles were disengaged to enter into new combinations, and yet not so softened but that it still maintained its lines of division from the strata above and below, the green tremolite was shooting its crystals into the pale homogeneous mass; while in another stratum the quartz drew its atoms apart in masses that assumed one especial form, the feldspar drew its atoms apart into masses that assumed another and different form, and the glittering mica built up its multitudinous layers between. Here the unctuous chlorite constructed its soft felt; there the micaceous schist arranged its undulating layers; yonder the dull clay hardened amid the intense heat, but, when all else was changing, retained its structure unchanged. Surely a curious chemistry, and conducted on an enormous scale!
It had been an essential part of my plan to explore the splendid section of the Lower Oolite furnished by the line of sea-cliffs that, to the north of the Portree, rise full seven hundred feet over the beach; and on the morning of Wednesday I set out with this intention from Isle Ornsay, to join the mail gig at Broadford, and pass on to Portree,—a journey of rather more than thirty miles. I soon passed over the gneiss, and entered on a wide deposit, extending from side to side of the island, of what is generally laid down in our geological maps as Old Red Sandstone, but which, in most of its beds, quite as much resembles a quartz rock, and which, unlike any Old Red proper I have ever seen, passes, by insensible gradations, into the gneiss.[2] Wherever it has been laid bare in flat tables among the heath, we find it bearing those mysterious scratches on a polished surface which we so commonly find associated on the mainland with the boulder clay; but here, as in the Hebrides generally, the boulder clay is wanting. To the tract of Red Sandstone there succeeds a tract of Lias, which, also extending across the island, forms by far the most largely-developed deposit of this formation in Scotland. It occupies a flat dingy valley, about six miles in length, and that varies from two to four miles in breadth. The dreary interior is covered with mosses, and studded with inky pools, in which the botanist finds a few rare plants, and which were dimpled, as I passed them this morning, with countless eddies, formed by myriads of small quick glancing trout, that seemed busily engaged in fly-catching. The rock appears but rarely,—all is moss, marsh, and pool; but in a few localities on the hill-sides, where some stream has cut into the slope, and disintegrated the softer shales, the shepherd finds shells of strange form strewed along the water-courses, or bleaching white among the heath. The valley,—evidently a dangerous one to the night traveller, from its bogs and its tarns,—is said to be haunted by a spirit peculiar to itself,—a mischievous, eccentric, grotesque creature, not unworthy, from the monstrosity of its form, of being associated with the old monsters of the Lias. Luidag—for so the goblin is called—has but one leg, terminating, like an ancient satyr's, in a cloven foot; but it is furnished with two arms, bearing hard fists at the end of them, with which it has been known to strike the benighted traveller in the face, or to tumble him over into some dark pool. The spectre may be seen at the close of evening hopping vigorously among the distant bogs, like a felt ball on its electric platform; and when the mist lies thick in the hollows, an occasional glimpse may be caught of it even by day. But when I passed the way there was no fog: the light, though softened by a thin film of cloud, fell equally over the heath, revealing hill and hollow; and I was unlucky enough not to see this goblin of the Liasic valley.
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 shore 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 glass, reflected the dusk twilight gleam in the north, revealing the narrow sounds and deep mountain-girdled lochs along which we passed; 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 Illustration—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 circumstances 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 shores 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 passed 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 shore. 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 shore 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 shoreward-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 illustration 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 noble 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 massy 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 noble 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 accumulation 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 shore, 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 circumstance 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, passing 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 shell 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 assured 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 pass 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 Scrapidale in Rasay, thence along part of the coast of Scalpa, thence direct through the middle of Pabba, and thence to the shore 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 asserted 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 passed 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 circumstances are, a warm room, a warm glass, 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 passengers." 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 passenger additional. The incident is scarce worth relating; but the postmaster was so vehement and terrible, so defiant of us all,—post, stabler, and simple passenger,—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 shell 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 Agassiz. 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 surpass the other in the variety and excellence of our specimens. Our leisure hours were snatched, 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 coarse 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 hoary sire in gratitude 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 circumstance 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 Saturday'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 Saturday 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 shore, 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 ashore. 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 circumstances, 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 ashore, 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 glass 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 pass,—every pulse that beat in his temples a throb of pain.
CHAPTER VIII.
Geology of Rum—Its curious Character illustrated—Rum famous for Bloodstones—Red Sandstones—"Scratchings" in the Rocks—A Geological Inscription without a Key—The Lizard—Vitality broken into two—Illustrations—Speculation—Scuir More—Ascent of the Scuir—The Bloodstones—An Illustrative 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 illustration—the line in which the superadded piece of frame has been stuck on to the frame proper. The origin of the island is illustrated 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 masses 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 altitude 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 illustration,—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 repetitions 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 shores of the Moray and Cromarty Friths. It would, however, be rash to pronounce 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 passing 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 passed 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 Agassiz. 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, Agassiz 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, abutting 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 passed along a transverse hollow, and then began to ascend a hill-side, from the ridge of which the water sheds to the opposite shore 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 nobler 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 space 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 participate 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 aptitude 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 illustrated 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 passed 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 masses; 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 glass-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 mass 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 mass, 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 illustrated 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 mass; 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 illustrative 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 circumstances, 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 glass, 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 mass, exists in thin glassy 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. |
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