Page:Notes on the State of Virginia (1853).djvu/22

6 its banks early in August. The inundation extends further on the Western than Eastern side, covering the lands in some places for 50 miles from its banks. Above the mouth of the Missouri, it becomes much such a river as the Ohio, like it clear, and gentle in its current, not quite so wide, the period of its floods nearly the same, but not rising to so great a height. The streets of the village at Cohoes are not more than 10 feet above the ordinary level of the water, and yet were never overflowed. Its bed deepens every year. Cohoes, in the memory of many people now living, was insulated by every flood of the river. What was the Eastern channel has now become a lake, 9 miles in length, and 1 in width, into which the river at this day never flows. This river yields turtle of a peculiar kind, perch, trout, gar, pike, mullets, herrings, carp, spatula fish of 50 ℔ weight, cat fish of 100 ℔ weight, buffalo fish and sturgeon. Alligators or crocodiles have been seen as high up as the Acansas. It also abounds in herons, cranes, ducks, brant, geese and swans. Its passage is commanded by a fort established by this State, 5 miles below the mouth of Ohio, and 10 miles above the Carolina boundary.

The Missouri, since the treaty of Paris, the Illinois and Northern branches of the Ohio since the cession to Congress, are no longer within our limits. Yet having been so heretofore, and still opening to us channels of extensive communication with the Western and Northwestern country, they shall be noted in their order.

The Missouri is, in fact, the principal river, contributing more to the common stream than does the Missisipi, even after its junction with the Illinois. It is remarkably cold, muddy and rapid. Its overflowings are considerable. They happen during the months of June and July. Their commencement being so much later than those of the Missisipi, would induce a belief that the sources of the Missouri are northward of those of the Missisipi, unless we suppose that the cold increases again with the ascent of the land from the Missisipi westwardly. That this ascent is great, is proved by the rapidity of the river. Six miles above the mouth it is brought within the compass of