The French Broad changes its character at Asheville, below which place it is a torrent, and above a placid, almost immobile stream, rising to the slightly higher altitude of the upper valley, in terraces, rather than by gradual ascent. Its shallow channel is bordered by alluvial bottoms--deposits carried from the mountain slopes--varying in width from a few rods to five miles, making, with a background of mountains rising massively in the distance, a landscape of surpassing beauty. A conservative estimate places the number of acres of first bottom land along the upper valley of the French Broad and its tributaries at 20,000, and twice that number of acres could be cultivated with sulky plows and harvested with self-binding reapers. Cane creek, followed by the Henderson and Buncombe county line, drains considerable low land--at places near its mouth almost marshy. On the opposite side of the French Broad there is a wide expanse of alluvial land, cut by Mill’s river, and extending for a distance of two miles up that stream, where the valley becomes second bottom and slope. Ochlawaha (Mud creek, locally named) emptying into the French Broad from the east, like its Florida namesake, is a lazy, sluggish stream. Its headsprings are in the crest of the Blue Ridge, all the way from the high Pinnacle and Hebron range to Sugarloaf and Bearwallow. The immediate basin of the stream from a short distance below Flat Rock, to its mouth, bears a unique character, being the only marsh in Western North Carolina. Its width varies from one fourth to two miles, and its length may be estimated at ten miles. A rank growth of vegetation is annually submerged. A soil of vegetable mold several feet in depth has been formed. Recent surveys show that the decline is sufficient to admit of perfect drainage, which would make this one of the most valuable agricultural and grazing tracts in the country. The crest of the Blue Ridge, in Henderson county, is an undulating plateau, which will not be recognized by the traveler in crossing. The Saluda mountains, beyond Green river, are the boundary line of vision on the south. The general surface features of the central part of this pearl of counties will be best seen by a glance at the pictorial view from Dun Cragin, near Hendersonville. Above the mouth of Ochlawaha the bottoms of French Broad gradually widen. The foot hills being the fartherest distance apart above the mouth of Little river, Boylston creek, Cathey’s creek, Davidson’s river, Little river and both forks of French Broad all have tempting valleys. It should be remarked that a large percentage of the land in these fair and fertile bottoms has been badly worn by much poor farming, but very little is worn out, so that there is yet not only hope but certainty of redemption by proper management. The expense of reinvigorating exhausted tracts is materially lightened by the presence of limestone outcrops.