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Why the Federal system is not adapted to all peoples, and how the Anglo-Americans were enabled to adopt it.. 195.

CHAPTER IX.

Why the people may strictly be said to govern in the

The Constitution of the United States

The Constitution of the State of New York..

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DEMOCRACY IN AMERICA.

CHAPTER I.

EXTERIOR FORM OF NORTH AMERICA.

North America divided into two vast regions, one inclining towards the Pole, the other towards the Equator.-Valley of the Mississippi.-Traces of the Revolutions of the Globe.-Shore of the Atlantic Ocean, where the English Colonies were founded.-Difference in the appearance of North and of South America at the time of their discovery.-Forests of North America.-Prairies.-Wandering Tribes of Natives.-Their outward appearance, manners, and language.-Traces of an unknown people.

NORTH AMERICA presents in its external form certain general features which it is easy to discriminate at the first glance.

A sort of methodical order seems to have regulated the separation of land and water, mountains and valleys. A simple but grand' arrangement is discoverable amidst the confusion of objects, and the prodigious variety of

scenes.

This continent is divided, almost equally, into two vast regions*, one of which is bounded, on the north by the Arctic Pole, and by the two great Oceans on the east and west. It stretches towards the south, forming a triangle, whose irregular sides meet at length below the great lakes of Canada.

The second region begins where the other terminates, and includes all the remainder of the continent.

VOL. I.

See the Map at the end of the Volume.

B

The one slopes gently towards the Pole, the other towards the Equator.

The territory comprehended in the first region descends towards the north with so imperceptible a slope, that it may almost be said to form a level plain. Within the bounds of this immense tract of country there are neither high mountains nor deep valleys. Streams meander through it irregularly: great rivers mix their currents, separate and meet again, disperse and form vast marshes, losing all trace of their channels in the labyrinth of waters they have themselves created; and thus at length, after innumerable windings, fall into the Polar seas. The great lakes which bound this first region are not walled in, like most of those in the Old World, between hills and rocks. Their banks are flat, and rise but a few feet above the level of their waters; each of them thus forming a vast bowl filled to the brim. The slightest change in the structure of the globe would cause their waters to rush either towards the Pole or to the Tropical Sea.

The second region is more varied on its surface and better suited for the habitation of man. Two long chains of mountains divide it from one extreme to the other; the Alleghany ridge takes the form of the shores of the Atlantic Ocean; the other is parallel with the Pacific.

The space which lies between these two chains of mountains contains 1,341,649 square miles*. Its surface is therefore about six times as great as that of France.

This vast territory, however, forms a single valley, one side of which descends gradually from the rounded summits of the Alleghanies, while the other rises in an uninterrupted course towards the tops of the Rocky Mountains.

At the bottom of the valley flows an immense river, # Darby's View of the United States.'

into which the various streams issuing from the mountains fall from all parts. In memory of their native land, the French formerly called this river the St. Louis. The Indians, in their pompous language, have named it the father of Waters, or the Mississippi.

The Mississippi takes its source above the limit of the two great regions of which I have spoken, not far from the highest point of the table-land where they unite. Near the same spot rises another river*, which empties itself into the Polar seas. The course of the Mississippi

is at first dubious: it winds several times towards the north, from whence it rose; and at length, after having been delayed in lakes and marshes, it flows slowly onwards to the south.

Sometimes quietly gliding along the argillaceous bed which nature has assigned to it; sometimes swoln by storms, the Mississippi waters 2500 miles in its course+. At the distance of 1364 miles from its mouth this river attains an average depth of fifteen feet; andit is navigated by vessels of 300 tons burden for a course of nearly 500 miles. Fifty-seven large navigable rivers contribute to swell the waters of the Mississippi; amongst others, the Missouri which traverses a space of 2500 miles, the Arkansas of 1300 miles, the Red River 1000 miles; four whose course is from 800 to 1000 miles in length, viz. the Illinois, the St. Peter's, the St. Francis, and the Moingona; besides a countless multitude of rivulets which unite from all parts their tributary streams.

The valley which is watered by the Mississippi seems formed to be the bed of this mighty river, which like a god of antiquity, dispenses both good and evil in its On the shores of the stream nature displays an inexhaustible fertility; in proportion as you recede from

course.

*The Red River.

+ Warden's 'Description of the United States.'

its banks, the powers of vegetation languish, the soil becomes poor, and the plants that survive have a sickly growth. Nowhere have the great convulsions of the globe left more evident traces than in the valley of the Mississippi: the whole aspect of the country shows the powerful effects of water, both by its fertility and by its barrenness. The waters of the primæval ocean accumulated enormous beds of vegetable mould in the valley, which they levelled as they retired. Upon the right shore of the river are seen immense plains, as smooth as if the husbandman had passed over them with his roller. As you approach the mountains, the soil becomes more and more unequal and sterile; the ground is, as it were, pierced in a thousand places by primitive rocks, which appear like the bones of a skeleton whose flesh is partly consumed. The surface of the earth is covered with a granitic sand and huge irregular masses of stone, among which a few plants force their growth, and give the appearance of a green field covered with the ruins of a vast edifice. These stones and this sand discover, on examination, a perfect analogy with those which compose the arid and broken summits of the Rocky Mountains. The flood of waters which washed the soil to the bottom of the valley afterwards carried away portions of the rocks themselves; and these, dashed and bruised against the neighbouring cliffs, were left scattered like wrecks at their feet*.

The Valley of the Mississippi is, upon the whole, the most magnificent dwelling-place prepared by God for man's abode; and yet it may be said that at present it is but a mighty desert.

On the eastern side of the Alleghanies, between the base of these mountains and the Atlantic Ocean, there lies a long ridge of rocks and sand, which the sea appears to *See Appendix A.