We now rise a bank of considerable height, which runs nearly parallel to the coast, through Carolina and Georgia; the ascent is gradual by several flights or steps for eight or ten miles, the perpendicular height whereof, above the level of the ocean, may be two or three hundred feet (and these are called the sand-hills) when we find ourselves on the entrance of a vast plain, generally level, which extends west sixty or seventy miles, rising gently as the former, but more perceptibly. This plain is mostly a forest of the great long-leaved pine (P. palustris Linn.) the earth covered with grass, interspersed with an infinite variety of herbaceous plants, and embellished with extensive savannas, always green, sparkling with ponds of water, and ornamented with clumps of evergreen, and other trees and shrubs, as Magnolia grandiflora, Magnolia glauca, Gordonia, Ilex aquifolium, Quercus, various species, Laurus Borbonia, Chionanthus, Hopea tinctoria, Cyrilla, Kalmia angustifolia, Andromeda, varieties, Viburnum, Azalea, Rhus vernix, Prinos, varieties, Fothergilla, and a new shrub of great beauty and singularity; it grows erect, seven or eight feet high; a multitude of erect stems arise from its root; these divide themselves into ascendant branches, which are garnished with abundance of narrow lanceolate obtuse pointed leaves, of a light green, smooth and shining. These branches, with their many subdivisions, terminate in simple racemes of pale incarnate flowers, which make a fine appearance among the leaves; the flowers are succeeded by desiccated triquetrous pericarpi, each containing a single kernel. The lowest sides of these savannas are generally joined by a great cane swamp, varied with coppices and hommocks of the various trees and shrubs already mentioned. In these swamps several rivulets take their rise, which drain them and the adjoining savannas, and thence meandering to the rivers through the forests, with their banks decorated with shrubs and trees. The earth under this level plain may be described after the following manner: the upper surface, or vegetative mould, is a light sandy loam, generally nine inches or a foot deep, on a stratum of cinereous coloured clay, except the sand-hills, where the loose sandy surface is much deeper upon the clay; stone of any sort, or gravel, is seldom seen.