Around the traveler, as he rides, are beautiful wood-land landscapes. A river, dammed with brown boulders, flows by the roadside. Where its channel narrows, it runs deep and smooth under the birches, oaks and pines; then at the shallows, among the rocks, it becomes a foaming torrent. The road is on a stone causeway, high above the crooked stream. Between the over-arching trees, glimpses of level road, yellow and dusty, can be seen at times. In the center of the valley, that widens out from the foot of the stone-fronted mountains, is a comfortable farm-house, enlarged for summer boarders, and kept by General G. W. Logan. It is the central point to view this scenic region of the mountains. It is reached by good roads from Rutherfordton, seventeen miles; Hendersonville, nineteen miles; Asheville, twenty-three miles; and Shelby, the terminus of the Carolina Central railroad, forty miles distant.
One mile from the hotel are the Pools. The stream is known as Pool creek. It seeks its level down a steep ravine, clothed principally with pines and oaks. Over three ledges of brown rock, whose edges still remain abrupt, the crystal waters of the stream plunge in quick succession, in as many thundering cascades. Where the cascades fall are basins, or pot-holes, formed perfectly round by the whirling of the waters. They are from ten to fifteen feet in diameter and of fabulous depth. The lower one is the largest, and has been sounded (as any one in the neighborhood, with straight face, will tell you) to the depth of 200 feet without striking bottom. Fifteen feet of the stock end of a giant pine projects out of it. The beauty and wildness of the spot could not be enhanced by a knowledge, even if true, that a depth of more than 200 feet of water lay in the lower pool.
On the edge of the ford of the river, our party halted to witness a sunset. It was an admirable point for observation. Before us spread a level, yellow field, forming the bottom of a beautiful, little valley. High mountains bound this vale on north and south, while directly in front of us, like companion sentinels, guarding the western gateway down which the sun was to march, stand Round Top and Chimney Rock mountains. Behind Chimney Rock, trending toward the west, arise in close succession, a number of mountains with distinct, broken summits,—a long palisade, fencing the gap in whose depths rushes the Broad river. In the center of the west, stands Bear Wallow mountain, the last visible knob of Hickory Nut gap. The sun was sinking behind the white cumuli that capped this mountain. Streamers of golden light, like the spokes of a celestial chariot, whose hub was the hidden sun, barred the western sky. The clouds shone with edges of beaten gold. Their centers, with every minute, changed to all hues imaginable. The fronts of the sentinel mountains were somber in the shadows, while the gap was radiant with the light pouring through it, and every pine on the top of the palisade stood black against the glowing sky.
It was dusk a few minutes after, but the roar of the river continued; the scents of summer filled the air; the trees bowed in luxuriant greenness over the road; the chirping of insects made musical the valley; the mountains rose gloomy and magnificent in the twilight.
The famous Bald mountain forms the north wall of the valley. Its sterile face is distinctly visible from the hotel porch. Caves similar to Bat cave are high on its front. In 1874, Bald mountain pushed itself into prominence by shaking its eastern end with an earthquake-like rumble, that rattled plates on pantry-shelves in the cabins of the valleys, shook windows to pieces in their sashes, and even startled the quiet inhabitants of Rutherfordton, 17 miles away. Since then rumblings have occasionally been heard, and some people say they have seen smoke rising in the atmosphere. There is an idea, wide-spread, that the mountain is an extinct volcano. As evidence of a crater, they point to a fissure about half a mile long, six feet wide in some places, and of unmeasured depth. This fissure, bordered with trees, extends across the eastern end of the peak. But the crater idea is effectually choked up by the fact that the crack is of recent appearance. The crack widens every year, and, as it widens, stones are dislodged from the mountain steeps. Their thundering falls from the heights may explain the rumbling, and their clouds of dust account for what appears to be smoke. The widening of the crack is possibly due to the gradual upheaval of the mountain.
The region of the gap is famous for sensational stories. In 1811, when known as Chimney Rock pass, a superstitious tale of a spectre cavalry fight, occurring here, was widely published in the newspapers of the day. The alleged witnesses of the spectacle were an old man and his wife living in the gap before Chimney Rock fall. So much interest was created in Rutherfordton by its recital, that a public meeting was held and a delegation, headed by Generals Miller and Walton, with a magistrate and clerk, visited the old couple and took their affidavits, to this effect: For several evenings, while shadows filled the pass and sunlight still lingered on the mountain summits, they had seen, from their doorway, two bodies of cavalry advance toward each other across the sky. They heard the charge sounded, and saw them meet in conflict, with flashing swords, groans, shouts of victory, and then disappear. Three more settlers testified as witnesses of the same vision. They were all believed trustworthy, but evidently deluded by some natural phenomenon. Giving credence to the tale, explanations were advanced, but none are satisfactory.
It is a half-day’s ride of unmarked interest from the bank of Broad river across the Bald mountains to the Catawba. The road is an old mail route to Marion, McDowell county. The air was hot and sultry in the middle of the day, when, after crossing the Bald mountains, I traveled over the foot-hills through woods of scrubby oaks and pines. The road was white, dry, and dusty. The branches of the impoverished trees, hanging with a melancholy droop, seemed panting with heat, and craving the presence of a breeze. Hawks circled overhead, and on a rail fence, visible at one break in the forest, a line of crows was roosting, with their glossy black plumage reflecting the sunlight. Their cawing heightened the effect of the scene. A ride alone through such scenery, and under such influences, tells upon one’s strength and spirits. After winding through a beautiful valley, and a moment later fording the Mill fork of Catawba river, I found myself in the little village of Old Fort. Its houses line a wide street, running parallel with the Western North Carolina railroad, and range along several short cross streets. A wooded hill rises back of it. During the Revolutionary war, and after, a fort with a strong stockade, enclosing a spring, stood on the bank of the stream. There were no battles fought here, but many depredations by Cherokees occurred, in which several people were killed in the vicinity. It is from this fort that the town takes its name.
About an hour before sunset, on that August day, I left Old Fort, by way of a well-traveled road, for Pleasant Gardens. There is many a level stretch for a gallop along this road, and I improved the opportunities afforded for a rapid push on my journey. Through the country I went, with the fields on my right, and the woods of the hills on my left; past large, pleasant-looking farm houses in the midst of ancestral orchards and wide-spreading farm lands. The streams are clear, but slow and smooth-flowing. The number of persimmon trees and hollies along the roadside mark a difference between the woods of this section and those of the higher counties.
It was after one of my easy gallops, that, bursting from a twilight wood, I beheld lying before me a valley scene of striking beauty. A broad and level tract of farming land, covered with meadows, corn and pea-fields, stretched away from the forested skirts of the hill-sides. From my point of observation not a house dotting the expanse could be seen, and not even the sound of running water (a marked feature of the higher valleys) disturbed the evening stillness. A cool pleasant breeze was stirring, but it scarcely rustled the leaves overhead. The dark outlines of Mackey’s mountains filled the foreground, making a broken horizon for the blue sky. On the right lay low hills. On the left the summits of a lofty line of peaks, behind which the sun was sinking, were crowned with clouds of flame, while the scattered cat-tails held all the tints and lustre of mother of pearl. That night I stopped in Pleasant Gardens, one of the richest and most beautiful valleys to be found in any land. It is miles in extent. John S. Brown was my hospitable and entertaining host. The large, frame house and surroundings vividly reminded me of my native state. Everything showed evidence of thrift and neatness, and withal a certain ancestral air, one that only appears with age, overhung the approach to, and portals of, the mansion. It was built a century ago, but many additions and repairs have been made since the original log-raising. Osage-orange hedges line the path to it under the cluster of noble trees. On the left as you approach, only a few feet from the house’s foundations, flows Buck creek with swift, clear waters: a trout stream in a day before civilization had cleared its banks.
Under a clouded sky I mounted my horse on the third morning of my journey, and set out from Pleasant Gardens. The fording of a stream is of so frequent occurrence in a trip through the Carolina mountains, that one is apt to have a confused recollection of any one river or creek that he crosses, although few are devoid of beauty or wildness. Those of the Catawba, as it flows through McDowell county, have lost the characteristics of the mountain ford. Boulders and out-cropping ledges of rock are absent; the rush and roar of crystal waters have given place to a smooth and less transparent flow, or noiseless, dimpled surface; the banks are of crumbling soil, and, instead of rhododendrons and pines, alders and willows fringe the waters’ edges.