Nearly at the same time as the latest disclosures in the valley of the Clyde, workmen cutting a drain on the farm of Kinaven, Aberdeenshire, discovered another ancient boat of the same form as most of those previously described, and measuring eleven feet long, by nearly four broad. It is hewn out of the solid oak, with pointed stem, and at the stern a projection formed in the piece, and pierced with an eye, as if to attach a mooring cable. Like the Glasgow canoes, it is rudely finished, and exhibits the rough marks of the instrument with which it was reduced to shape. It lay imbedded in the moss, at a depth of five feet, at the head of a small ravine; and near it were found the stumps and roots of several large oaks. The nearest stream, the Ythan, is several miles off, and the sea is distant many more. A few years previous to this discovery, a similar canoe, of still smaller dimensions, was dug up in the moss of Drumduan, in the same county. It is described as quite entire, and neatly formed out of a single block of oak; but being left exposed, it was broken by the rude handling of some idle herd-boys.[47]
Such are a few examples of the aboriginal fleets of ancient Caledonia, found at different dates, and in various localities, yet agreeing wonderfully in every essential element of comparison. With them might also be noted the frequent discovery in bogs, or in alluvial strata, of trees felled by artificial means, and accompanied with relics of the most primitive arts. In 1830, for example, workmen engaged in constructing a sewer in Church Street, Inverness, found at a depth of fourteen feet below the surface, in a stratum of stiff blue clay, numerous large trunks of fossil oak; and along with these several deer's horns, one of which, bearing unmistakable marks of artificial cutting, is now deposited in the Museum of the Society of Antiquaries of Scotland.[48] Here surely is common ground for the antiquary and the geologist. The rude harpoon left beside the bones of the stranded whale, far up in the alluvial valley of the Forth: the oaken querne, the wheel and the arrow-heads: the boats beneath the City Cross of Glasgow, the centre of a busy population for the last thousand years: the primitive ship, as we may almost term the huge canoe on the banks of the Carron: and the tiny craft just found near the waters of the Ythan—all speak, in no doubtful language, of the presence of a human population, at a period when the geographical features of the country, and the relative levels of land and sea, must have differed very remarkably from what we know of them at the earliest ascertained epoch of definite history. They point to a time within the historic era, when the ocean tides ebbed and flowed over the carse of Stirling, at a depth sufficient to admit of the gambols of the whale, where now a child might ford the brawling stream; and when the broad estuary of the Clyde flung its waves to the shore, not far from the high ground where the first cathedral of St. Mungo was founded, A.D. 560. These evidences of population, prior to the latest geological changes which have affected the surface of the country, are indeed all found on old historic ground, according to the reckonings of written chronicles. The first of them, in the south country, have been met with in localities where the traces of Roman invasion in the second century remain uneffaced. The carse of Falkirk is still indented with the vallum of the Antonine wall. Its modern church preserves the old tablet, which assigned to the ancient structure on its site a date coeval with the founding of Scottish monarchy under Malcolm Canmore; and the broad level ground, which has disclosed evidence of such remarkable changes, alike in natural features and in national arts and manners, was the battle-field of Wallace in the thirteenth century, as of Prince Charles Edward and the Highland clansmen in the eighteenth century. Trivet thus refers to the carse of Falkirk, in describing the invasion of Edward I., thereby affording curious evidence of its state at the former period,—"Causantibus majoribus loca palustria, propter brumalem intemperiem, immeabilia esse;" on which Lord Hailes remarks—"The meaning seems to be, that the English could not arrive at Stirling without passing through some of the carse grounds, and that they were impracticable for cavalry at that season of the year."[49] Nor are the historic associations of the broad carse which the Forth has intertwined with its silver links a whit behind those of the vale of Carron. There, in all probability, Agricola marshalled the Roman legions for his sixth campaign, and watched the mustering of the army of Galgacus on the heights beyond. The ever memorable field of Bannockburn adds a sacred interest to the same soil. There, too, are the scenes of James III.'s mysterious death on the field of Stirling, and of successive operations of Montrose, Cromwell, Mar, and Prince Charles. But the oldest of these events, long regarded as the beginnings of history, are modern occurrences, when placed alongside of such as we now refer to. Guiding his team across the "bloody field," as the scene of English slaughter is still termed, the ploughman turns up the craw-foot, the small Scottish horse-shoe, and the like tokens of the memorable day when Edward's chivalry was foiled by the Scottish host. Penetrating some few feet lower with his spade, he finds the evidences of former changes in the level of land and sea, but with them stumbles also on the relics of coeval population. Lower down he will reach the stratified rocks, including the carboniferous formation, stored no less abundantly with relics of former life and change, but no longer within the historic period, or pertaining to the legitimate investigations of archæological science, unless in so far as they confirm its previous inductions, and prove the slow but well defined progress of the more recent geological changes on the earth's surface. Such reflections are not suggested for the first time in our own day, nor will a shallow part satisfy those who have gone thus far. "Nature hath furnished one part of the earth, and man another. The treasures of time lie high, in urns, coins, and monuments, scarce below the roots of some vegetables. Time hath endless rarities, and shows of all varieties, which reveals old things in heaven, makes new discoveries in earth, and even earth itself a discovery. That great antiquity, America, lay buried for thousands of years, and a large part of the earth is still in the urn unto us."[50]
Some of these historic phenomena which are indicated above required only time to produce them. The beds of sand and loam at Springfield, in which the ancient fleets of the Clyde have lain entombed for ages, are such as the slow depositions of winter floods will for the most part account for, if the chronologist can only spare for them the requisite centuries. Others seem to point to geological changes within the historic era, of a more remarkable and extensive character. These it is not our province to explain. Whether the geologist find it most consistent with the established laws of his science to assume the standing of the whole ocean at higher levels within so recent a period, or adopt the more probable theory of local upheaval and denudation to account for these phenomena, this at least must be conceded, that the lapse of many ages is required for the changes which they indicate, and we can hardly err in inferring that civilisation had advanced but a little way on the plain of Nimroud, or the banks of the Nile, when the tiny fleets of the Clyde were navigating its estuary, and the hardy fishermen were following the whale in the winding creeks of the Forth.
FOOTNOTES:
[30] Pennant's Tour, vol. ii. p. 107.
[31] Sinclair's Stat. Acc. vol. i. p. 160.
[32] New Stat. Acc. vol. iv. Wigtonshire, p. 179.
[33] Sinclair's Stat. Acc. vol. viii. p. 305. New Stat. Acc. vol. iv., Kirkcudbrightshire, p. 155.
[34] Archæologia Scotica, vol. iv. p. 299.
[35] Sinclair's Stat. Acc. vol. xv. p. 68.