than a few years at most. Thus we may consider ourselves as standing by the dying-beds of these creatures, with the consciousness that we shall soon see them no more; that the sentence is gone forth against them; that their sands are running to the last grains, and that no effort of ours can materially prolong their existence. The facts from which these conclusions are drawn are highly curious, and I shall endeavour to lay them, with as much brevity as they will allow, before my readers.
On that prochronic hypothesis, by which alone, as I conceive, the facts revealed by geological investigation can be reconciled with the unerring statements of Scripture—every word of which is truth, the truth of a "God that cannot lie,"—we may assume the actual creation of this earth to have taken place at that period which is geologically known as the later Tertiary Era, or thereabout. When, on the third day, "the waters under the heaven were gathered together into one place, and the dry land appeared," it is not necessary to suppose that the form assumed by the emerging land was immediately that which it now has; we may, on the other hand, I think, assume as likely, that successive or continuous changes of elevation followed, which have been protracted, perhaps constantly decreasing in extent and force, to the present hour.[2]
Perhaps between the six days' work of Creation and the Noachic Flood, Europe became much altered in outline, and in elevation. It may have been, at first, a great archipelago, agreeing with the epithet by which it is designated in early Scripture, "the Isles,"[3] and by which it was subsequently known for ages. The Pyrenees, the Alps, and the Apennines, already emerged, were slowly uniting, and the Carpathians, the Balkan, the Taurus, and the Caucasus, were uprearing, while the vast regions to the north were still an expanse of open sea. England was probably united with the newly-formed European continent, and embraced Ireland in one great mass of unbroken land, which stretched far away into the Atlantic. Volcanoes were active in the north of Ireland, and in the west of Scotland, pouring forth those floods of fiery lava which have cooled into the columnar forms seen at the Giant's Causeway and the Cave of Fingal. Slowly the north of Europe emerged, and the great south-west expanse of Britain sank beneath the sea, leaving, it may be, the large island of Atlantis in mid-ocean, to be submerged by a later catastrophe.
Probably changes very similar were coevally taking place in Asia and North America, while the vast flat alluvial regions of South America were, perhaps, even still more recently formed, and a great Pacific continent was in course of subsidence, of which Australasia and Polynesia are the existing remains.
Such changes of elevation, and of the continuity of land, must effect considerable alterations of climate; and, therefore, it is not surprising to know that, in earliest ages, animals and plants flourished in regions to which they would now be altogether unfitted, and that many races existed then which have since died out; for geological and climatal modifications are among the most easily conceivable causes of the decease of species.
In the great swamps of emerging Germany, and in the, as yet, only half-drained valleys of Switzerland, lurked then the heavy Dinothere. Huger than the hugest elephant, he carried an enormous body of twenty feet in length, vast and barrel-like, which even his columnar limbs of ten feet long scarcely sufficed to raise from the ground. His uncouth head, elephantine in shape, was furnished with a short proboscis; and two tusks, short and strong, projected from the lower jaw, not curving upward, as in the elephant, but downward, as in the walrus. In the teeming marshes lurked this ungainly beast, half immersed, digging out with his mighty pickaxe-tusks the succulent roots that permeated the soft soil, which his sensitive trunk picked up, and conveyed to his mouth.
On the southern slopes of the slowly-rising Himalayas, already clothed with forests of teak, and palm, and bamboo, revelled the Sivathere, another heavy creature, of the bulk of a rhinoceros, and therefore not more than half equalling the German colossus. He too was a strange subject. With a proportionally enormous head, in form somewhat between that of the elephant and of the rhinoceros, minute sunken piggish eyes, and a short proboscis like that of the tapir, he carried two pairs of dissimilar horns. On the forehead were placed one pair, seated upon bony cores, not unlike those of our short-horn oxen. Behind these there rose another pair, large and massive, which were palmated and branching, like those of the fallow-deer, but on a gigantic scale. What sort of a body, and what kind of limbs, furnished the complement of this curiously-compound head, we do not exactly know; but surely it must have been a very remarkable form, as it browsed quietly and blamelessly, among the luxuriant shrubs of those sun-facing slopes.
In the same regions a land Tortoise of enormous bulk, far vaster than the vastest of now existing species, to which that ponderous one which will march merrily away with a ton weight on its back, is a mere pigmy, shook the earth with its waddle, and the forests with its hoarse bellowing. Broad roads, like our highways, were beaten by it through the jungle, along which it periodically travelled to the cool springs, leisurely sauntering, and tarrying to munch the fleshy gourds and cactuses that bordered its self-made track.
The plains of Siberia, stretching away towards the Arctic Ocean, sheltered countless hosts of huge pachydermatous quadrupeds. A species of Rhinoceros, not less bulky than those of the present age, roamed to the very verge of the Icy Sea; its hide, tough and leathery, was destitute of folds, but was clothed with tufts of rigid gray hair—an ornament which is denied to our existing degenerates. Two horns, the front one of unusual massiveness and length, were seated, as in several of the African kinds, one behind the other, and were wielded by a head of great strength and development.
More remarkable still was that great hairy Elephant, called the Mammoth, which appears to have swarmed in those cold plains by myriads. Of equal dimensions to the Indian species of the present age, this denizen of the north had far more enormous curving tusks, and instead of the naked hide of those we are familiar with, his body was encased in black hair, with a thick under stratum of red curled wool, and bore a long mane on the ridge of the neck.
There was, at the same time, a quadruped, nearly allied to the elephants, but differing from them in some technical characters. With a body equally bulky, but considerably longer, it had shorter limbs, a broader head, small tusks in the lower, as well as large curving ones in the upper jaw, and probably a trunk intermediate between the elephant's and the tapir's. Truly cosmopolite as this great Mastodon was, for we dig up his bones from all parts of the world, he had his head-quarters in North America, where, from his dimensions and his numbers, he must have formed a very characteristic feature of the primeval swamps and forests. There, with his tusks, he grubbed up the young trees, whose juicy roots he ground down with his great mammillary molar teeth, or chewed up to a pulp the sapwood of the recent branches and spicy twigs. And ever and anon he would resort to the broad saline marshes—the "Licks," as they are now called—to lick up the crystallised salt on their margins, so grateful to all herbivorous quadrupeds. Here, in his eagerness to gratify his palate with the pungent condiment, he would press farther and farther into the treacherous quagmire, till he began to sink, and then, in his terror, he would plunge and flounder, getting more and more deeply bemired, till at length he could struggle no more, and the bog would close over him, and he would be no more seen till some spectacled geologist of this nineteenth century, note-book in hand, would go and dig up his remains, marvelling at the freshness with which they had been preserved in the antiseptic peat.
But let us look at South America, where, as the great back-bone chain of the Andes is being elevated out of the sea, the torrents and cataracts are pouring down from its sides immense quantities of crumbled rock and pasty mud, which, deposited upon the vast tabular field, brought by the upheaving just to the level of the sea, forms that grand alluvial plain unequalled on the face of the globe for extent, which is clothed with the mighty forests of Guiana and Brazil, or with the tall grass and thistles of the Pampas. The torrents still fall; and, meandering through this glorious plain, unite and form the most majestic of rivers, ever depositing the rich alluvium, and thus sensibly augmenting, to this day, the breadth of their noble continent, and their own length.
Strange creatures riot here in these primal ages. The young land, hot and
