appear close to the river, and as you ascend, these become more frequent and extensive; the rising grounds change to a brown or red clay, and you lose sight of the sand, which, however, still continue to run parallel to the river, at some distance back, and thus to accompany it almost to its source; on the left bank, ascending the river behind the alluvial flats, is a border of rising ground, generally composed of a brown or red sandy loam, upon which rests a plain or high table land of stiff clay, stretching back to a considerable distance.
In many places, however, the high land rises boldly up from the river, so as to alternate with the flat on the opposite side. The alluvial flats are covered with a luxuriant crop of grasses. But on the table lands the grass is not abundant. There has now been a year's experience of the capability of the soil, and there is no doubt that it can abundantly produce any grain, fruit, vegetable, tree, or shrub, which belongs to its parallel of latitude. The sandy loam is considered the best for present purposes, the stiff clay lands being difficult to break up, and requiring more time and labour than many are willing to bestow. I have seen within two miles of this, a fine crop of wheat grown without any manure, and with much less preparatory culture than would be required in England. This was produced on an alluvial flat, the grain being ploughed in, just before the
