"It results from a combination of these observations, that the greatest chains of mountains on our globe, are ranged in an arc of a circle around the great ocean, and the sea of India; that they seem to present rapid descents towards the immense basin they surround, and gentle slopes on their opposite sides; in fine, from the Cape of Good Hope to Behring's straits, and thence to Cape Horn, the eye of the most timid observer cannot fail to see some trace of an arrangement, as surprising from its uniformity, as from the vast extent of ground which it embraces.
"Let us pause for an instant to consider this great fact of physical geography. If we conceive ourselves placed in New South Wales, with our face turned towards the north, we have America on our right hand, Africa and Asia on our left. These continents, which we hardly before ventured to approach in our imagination, considered in this point of view, form a consistent system, whose structure, as far as we are acquainted with it, presents in its great features an astonishing symmetry. A chain of enormous mountains surrounds an enormous basin; this basin, divided into two by a vast collection of islands, often bathes with its waves the feet of this great primary chain of the earth."
In this chain lie the greatest mountains of the globe. One peak of the Himmalayah rises nearly five miles above the level of the sea; another has a height of 25,500 feet; and a third of 22,217 feet. In South America are Soratu, in height 25,250 feet.
| Illimani, | 24,000 |
| Chimborazo, | 21,400 |
not to mention Antisana, Mauflos, Chillau, Cotopaxi, all of which exceed in height any mountains that do not lie in this great system. Nay, did not the great Volcano of Owyhee enter into the order with a height of 18,000 feet, the list of those surpassing the other mountains of the globe, might be very much extended.
We shall have occasion hereafter to speak of the volcanic energies still exerted in this vast stony girdle, and shall therefore confine ourselves strictly to mere external form.
The arms and branches of mountain chains enclose as has been seen, basins marked by rivers which convey their surface waters to the ocean. The rains which fall on the sides of mountains and hills, unite in torrents and streams, which follow the lines of most rapid slope in their course to the sea.
The greater rivers mark the lowest part of a principal basin, on each side of which, at a greater or less distance, are to be found rising grounds, themselves hollowed out into lateral secondary basins, containing courses of water less considerable than the first, into which they cast themselves, and whose branches they are. The borders of these secondary basins are again hollowed out into basins of a third order, whose slopes also contain water courses less considerable than the preceding, into which they in turn discharge themselves. This ramification continues until we reach the smallest ravines of the boundary mountains, and the map appears, as it were, covered with a net work of rivers and lesser streams. The great valley of the Mississippi and Missouri, forms perhaps the most striking instance of this sort, upon the surface of our globe.
Rivers and streams are constantly exerting a mechanical action on the surfaces over which they run; abrading and tearing off fragments even of the hardest rocks, they roll them in their course until the velocity becomes insufficient to transport them farther. At diminished velocities they move fragments of less size, down to the smallest pebbles; at still less velocities, they transport sand, and finally earthy matter, in the most minute division. These are deposited in succession in positions corresponding to the rapidity of the stream, and hence the beds of rivers present at each of their different sections, materials of magnitude and quality corresponding to the rate at which the stream usually flows. The increase in the magnitude of streams, due to violent rains and the melting of the snows, changes the position of the substances that compose their bed, and the more easily suspended materials are often held until the stream actually meets the ocean. In such sudden increases, the streams often overflow their usual banks, and make their deposits laterally, until the constant succession of such deposits raises the adjacent ground high enough to set bounds to the further spreading of the stream. This deposit is remarkable for its taking place in greatest quantity close to the usual bed of the stream; and thus it speedily opposes natural dykes to its own redundant waters. This action is most conspicuous at points where marked changes take place either permanently or periodically in the rapidity of running water: when streams descend from mountains into lines of less descent, a deposit uniformly takes place, forming flats or intervals, as they are styled in the United States, of which we have such beautiful instances in the valleys of the Connecticut and Mohawk, and that part of the Hudson near Albany; again, where rivers meet the sea, they are interrupted in their course by the rise of the tides of the ocean, and here again deposits take place, sometimes forming shoals and banks in the ocean itself; at other times, bars and obstructions at their own mouths; and again, deltas of solid land, constantly encroaching upon the sea. This action, which is continually going forward, is called alluvial. The delta of greatest fame, and from which the others have derived their generic name, is that of the Nile; this we have evidence, almost historic, to prove to be wholly the gift of the river. And if it no longer increase as rapidly as in former ages, the cause is obvious, for the alluvion has been pushed so far forward as to meet a strong current that sweeps along the African coast, and must carry off much of the earth the Nile discharges into the Mediterranean. The great rivers of Asia and of America carry still greater quantities of solid matter, but we have not the same distant traditions to refer to for the amount of the increase they have caused; still, however, we know that the mouth of the Mississippi has been advanced into the Gulf of Mexico several leagues since the settlement of Louisiana; and that islands of great extent are frequently formed, in the course of a single year, by the deposits of the Ganges.
We however find traces of aqueous action far more extensive and powerful than those which are now taking place under our eyes by fluviatile action. There is no part of the globe that has been examined, which does not show that it has been subjected to the action of water, in floods far more powerful than any we now are in the habit of seeing. Every where, except in the case of rocky cliffs, and steep mountains, or where we see obvious evidence of a recent elevation, we find the surface strewn with the deposits of water: boulders of greater or less size, beds of gravel, sand, and clay, form the present outer coating of the greatest part of the land. These deposits were long confounded with the alluvial, but have at length been proved, by incontrovertible evidence, to be the results of an action, which if not contemporaneous, must have been universal. We have seen an able attempt to show that this species of deposit did not take place at one and the same period, but was merely the general consequence of similar causes acting at different epochs. Our impression, we must however confess to be, that the action was not only co-extensive with the globe, but contemporaneous. It at any rate exhibits proofs the most satisfactory, that the last great and extensive change which our earth has undergone, was effected by the agency of water, in a state of rapid and violent motion. Ascribing this deposit to a single flood, it has been styled diluvial.