The Heart of the Alleghanies; or, Western North Carolina — Reading Notes

ps and mentioned in text books as the highest point of rock in the eastern United States. It now holds its true position below several summits of the Black, Smoky, and Balsam ranges. From the barometrical measurements of trustworthy explorers, no less than 57 peaks in Western North Carolina are found to be over 6,000 feet in altitude. The more accurate observations being taken by means of levels, by the coast survey, may slightly reduce this number.

It was John C. Calhoun who, in 1825, first called particular attention to the southern section of the system. His attention had been turned to it by observing the numerous wide rivers, and tributaries of noble streams, which, like throbbing arteries, came forth from all sides of the North Carolina mountains, as from the chambers of a mighty heart. He saw the New river flowing towards the Ohio; the Watauga, the Nolechucky, the French Broad, the Big Pigeon, the Little Tennessee, the Hiawassee, and their thousand tributaries, pouring from the central valleys through the deep gaps of the Smokies into the western plains, and uniting with the branches from the Cumberland mountains to form the stately Tennessee; the Yadkin, the Catawba, the Broad, the Chatooga, and the headwaters of the greatest streams south of Virginia that empty into the Atlantic. From these observations he reasoned rightly that between the parallels of 35 degrees and 36 degrees and 30 minutes, north latitude, lay the highest plateau and mountains of the Atlantic coast.

The region, as measured in a bee line through the center of the plateau from Virginia to Georgia, is 200 miles in length. Its breadth, from the summits of the parallel rampart ranges of the Blue Ridge and Smokies, varies from 15 to 65 miles, and includes within this measurement a plateau expanse of 6,000 square miles, with an altitude of from 2,000 to 4,000 feet. Inclusive of the eastern slope, the off-shooting spurs of the Blue Ridge and the South mountains, the average breadth is 70 miles. A portion of the piedmont section, properly a part of the mountain district, would be taken in the latter measurement. The counties are 25 in number, reaching from Ashe, Alleghany, and Surrey in the north to Macon, Clay, and Cherokee in the south.

After the bifurcation of the Blue Ridge and Smoky mountains in Virginia, embracing with a wide sweep several counties of that state and Ashe, Alleghany, and Watauga of North Carolina, they almost meet again in the northeastern limit of Mitchell county. Here, in collosal conjunction, through their central sentinel heads, the two ranges seem holding conference before making their final separation. The Grandfather, the highest peak of the Blue Ridge and the oldest mountain of the world, stands on one side; the majestic Roan of the Smokies, on the other, connected by the short transverse upheaval known as Yellow mountain. This spot is poetically spoken of as the grand portal to the inner temple of the Alleghanies; the Grandfather and the Roan being the two pillars between which hangs, forever locked, the massive gate of Yellow mountain. The high table-land of Watauga forms the green-carpeted step to it. Trending southwest, between the two separating ranges,--the Blue Ridge bending like a bow, and the Smokies resembling the bow-string,--lies wrapped in its robe of misty purple, the central valley, comprising 13 counties.

The western rampart range, bearing the boundary line between North Carolina and Tennessee, lifts its crest much higher than the Blue Ridge; is more massive in its proportions; less straggling in its contour; but with lower gaps or gorges, narrow and rugged, through which flow all the rivers of the plateau. Generically known as the Smoky mountains, it is by the river gorges divided into separate sections, each of which has its peculiar name. The most northerly of these sections is termed the Stone mountains; then follow the Iron, Bald, Great Smoky, Unaka, and the Frog mountains of Georgia. Twenty-three peaks of the Smoky mountains are over 6,000 feet in altitude, the loftiest being Clingman’s Dome, 6,660 feet. The deepest gap is that of the Little Tennessee, 1,114 feet.

The eastern rampart range--the Blue Ridge--trends southward with the convolutions of a snake; its undulations rising seldom above a mile in altitude and sinking sometimes so low that, in passing through its wide gaps, one is not aware that he is crossing a mountain range, the fact being concealed by the parallel spurs rising, in many instances, to a higher altitude than their parent chain. In spite of its depressions, and, when compared with the Smoky mountains, the low average elevation of its crest, it is the water-shed of the system. Not a stream severs it. On the east every stream sweeps toward the Atlantic. On the west the waters of its slopes are joined at its base line by those flowing down the east or south side of the Smoky mountains; and, mingling with the latter, pour through the deep passes of the loftier range into the valley of the western confluent of the Tennessee.

From the Blue Ridge is thrown off many short ranges, trending east and south across the submontane plateau. In character of outline they are similar to the parent chain. This plateau, known as the Piedmont, walled on the west by the Blue Ridge, diversified by mountains and hills, and seamed by the Yadkin, Catawba, and Broad rivers and their affluents, incloses in its limits many beautiful and fertile valleys. The outer slope of the Blue Ridge, overlooking Piedmont, is abrupt in its descent and presents wild and picturesque features; cascades marking the channels of the streams. Further south, where the range bends around the South Carolina and Georgia lines, bold escarpments of rock and ragged pine-set declivities, seamed by cataracts, and beaten on by a hot and sultry sun, break sheer off into the southern plains. The inner slope of the Blue Ridge throughout its entire length from Virginia to Georgia, as contrasted with the outer slope, is more gentle in its descent; is heavily wooded and diversified with clearings. The Smoky mountains present similar characteristics--richly wooded descents toward the central valley; rocky and sterile fronts toward Tennessee.

The reader must not imagine that the central valley or plateau, of which we have been speaking, is a level or bowl-shaped expanse between the ranges described. On the contrary, its surface is so broken by transverse mountain ranges and their foot-hills that, by means of vision alone, the observer from no one point can obtain a correct idea of the structural character of the region. From the loftiest peaks, he can see the encircling ranges and the level lands beyond their outer slopes; but below him is rolled an inner sea of mountains, which, when looked upon in some directions, seems of limitless expanse. The transverse chains, comprising the Yellow mountain, the Black, Newfound, Balsam, Cowee, Nantihala, and Valley River mountains, hold a majority of the highest summits of the Alleghanies.

The Black mountain chain, the highest of these ranges, is only 20 miles long, and has 18 peaks in altitude over 6,000 feet; the highest of which, Mitchell’s Peak, 6,711 feet above sea-level, is the sovereign mountain of the Alleghanies. The Balsam range, the longest of the transverse chains, is 45 miles in length and crested by 15 wooded pinnacles over 6,000 feet high. The parallel cross-chains have, nestling between their slopes, central valleys, varying in length and width, and opening back into little vales between the foot-hills and branching spurs. Through the lowest dip of each great valley, sweeps toward the Smokies a wide, crystal river fed by its tributaries from the mountain heights.

The great valleys, or the distinct regions drained each by one of the rivers which cut asunder the Smokies, are six in number. The extreme northern part of the state is drained by the New river and the Watauga. Between the Yellow mountain and the Blacks lies that deeply embosomed valley region watered by the head-springs of the Nolechucky. Next comes the widest and longest plain of the mountain section--the valley of the French Broad. The Big Pigeon winds through the high plateau between the Newfound and Balsam mountains. The region of the Little Tennessee comprises not only the wide lands along its own banks, but those along its great forks--the Tuckasege, Nantihala, and Ocona Lufta. West of the Valley River mountains the country is drained by the Hiawassee.

Geologically speaking, the mountains of North Carolina are the oldest in the world. During the period of general upheavals and subsidences of the crust of the earth, these mountains were the only lands remaining throughout firm above the surface of the ocean. Rocks of the Archæan or earliest age are exposed, and with their edges turned at a high angle lie upon the beds of later periods of formation. North of the southern boundary of Virginia, the structural character of the mountains is different.

The entire region is mantled with forests to the summit of every peak; the valleys and many of the adjacent coves are cleared and inhabited by a happy, healthy, and hospitable people. It is rich in picturesque scenery--romantic rivers, luxuriant forests, majestic mountain heights, valleys of exquisite beauty, quaint villages, cliffs, and waterfalls. It is rich in a life-giving climate, brilliant skies, fertile lands, pastured steeps, and timber and mineral wealth.

It is of this country--the Heart of the Alleghanies--that in the following pages we have treated in as full, concise, and entertaining a manner as we could conceive and carry into execution.

THE NATIVE MOUNTAINEERS.

All kinds of creatures stand and fall By strength of prowess or of wit; ’Tis God’s appointment who must sway, And who is to submit. --_Wordsworth._

e are excluded from a knowledge of ancient American history by an impenetrable veil of mystery and silence. The past has left us only relics--relics of things and relics of races--which are interpreted by an unreined imagination. Before Europeans set foot on the western shore of the Atlantic, before the Indians occupied the forest continent, there dwelt on all the sunniest plains and fertile valleys a race well advanced in mechanical and æsthetic art, skilled in war and consecrated in religion. It came and flourished and perished, leaving only monuments of its existence in the form of works of earth, and works of stone--mounds, forts, and pottery. The old mounds scattered everywhere are the sepulchres of illustrious dead, and because of their number, the race has been designated the “Mound Builders.” They inhabited, among other places, the southern Alleghanies, the largest number of mounds being found in the upper valley of the Little Tennessee. Most of the rich mica dikes bear evidence of having been worked centuries ago. The marks of stone picks may still be seen upon the soft feldspar with which the mica is associated, and tunnels and shafts show some knowledge of mining. The fact that a great many ancient mounds all over the country contain skeletons, encased in mica plates, associates these diggings with the builders of the mounds.

The earliest traditional knowledge we have of the habitation of the southern highlands has been handed down by the Cherokees. They say that before they conquered the country and settled in the valleys, the inhabitants were “moon-eyed,” that is, were unable to see during certain phases of the moon. During a period of blindness, the Creeks swept through the mountain passes, up the valleys, and annihilated the race. The Cherokees in turn conquered the Creeks, with great slaughter, which must have occurred at a very ancient date, for the country of their conquest and adoption is the seat of their religious legends and traditional romances.

No definite boundaries can be assigned to the land of any Indian tribe, much less a nation of proud and warlike mountaineers who were happy only when carrying bloodied tomahawks into an enemy’s country. The tribe was distinguished by two great geographical divisions, the Ottari, signifying “among the mountains,” and the Erati, signifying “lowland.” Provincial historians have designated them as “In the Valley” and “Overhill” towns, the great highland belt between the Blue Ridge and Smoky mountains being designated as a valley. The ancient realm of the tribe may, in a general way, be described as the headwater valleys of the Yadkin and Catawba on the east; of the Keowee, Tugaloo, Flint, Etowa and Coosa on the south, and the several tributaries of the Tennessee on the west. There were 60 towns, and 6,000 fighting men could at any time be called by the grand chief to the war path. It was the military prowess of these warriors that gave to the nation the most picturesque and most secure home of all the American tribes. A keen and delicate appreciation of the beautiful in nature, as associated with the grandeur of their surroundings, inspired them to unparalleled heroism in its defense against intrusion. They successfully withstood neighboring tribes, but their contest with the whites was a contest with destiny, in which they yielded only after a long and bloody struggle. The ancient nation of the mountains, expelled from its home, crippled and enervated, but improved in some respects, has found a home in the less picturesque and distant west; but has left a dissevered and withered limb which, like a fossil, merely reminds us of a bygone period of history.

If any one doubts that the Cherokees possessed an appreciative love of country and a genuine sympathy with nature, let him turn to his map, and pronounce those Indian names which have not been cruelly, almost criminally, displaced by English common-places. Let him remember too that there is a meaning in their euphony, and a suggestiveness in their melody. It is a grievous fault, the more grievous because it is irreparable, that so many of the bold streams which thunder down forest slopes and through echoing cañons, have lost those designations whose syllables glide from the tongue in harmony with the music of the crystal currents. Of many natural features the names are preserved, but their meanings have been lost.

East of the Blue Ridge, in North Carolina, very few geographical names of Indian origin have survived. In the valley of the French Broad there is also a barrenness of prehistoric nomenclature. From this circumstance it is argued, and the argument is well sustained, that there was no permanent habitation of Indians in these two localities. The villages were located in valley, and were known by the name of the streams. In some instances, traditions became associated with the name, and in them we have a key to an unwritten scroll. A village, furthermore, gave to a region an importance which made its name widely known, not only in the tribe but among traders and other white adventurers, and thus made it a fixture. There is the additional negative evidence of no permanent habitation, in the fact that mention is no where made, in the annals of military expeditions against the Indians, of villages east of the Balsam mountains. Hunters and warriors penetrated the forests for game, and carried the tomahawk to every frontier, frequently making the Upper Catawba and French Broad valleys their camping ground. While we know nothing about the facts, the presumption is reasonable that at least all the larger rivers and their tributaries were given names by the Indians, which perished with the change of race and ownership.

Catawba is not of Cherokee origin. The river takes its name from the tribe which inhabited its valley until a recent date; South Carolina. It was a species of vandalism to substitute French Broad for Agiqua and Tocheeostee, the former being the name applied by the Erati, or “over the mountain” Cherokees, to the lower valley, and the latter by the Ottari, or “valley” towns, to the upper or North Carolina section below Asheville. “Racing river” is a literal translation of the term Tocheeostee. Above Asheville, where the stream is placid and winds snake-like through the wide alluvions, it took the name Zillicoah.

Swanannoa is one of the most resonant of Indian names, though in being accommodated to English orthography it has lost much of its music. It would be impossible to indicate the original pronunciation. I can, perhaps, tell you nearer how to utter it. Begin with a suppressed sound of the letter “s,” then with tongue and palate lowered, utter the vowel sound of “a” in swan four times in quick succession, giving to the first as much time as to the second two, and raise the voice one note on the last. The word is said to have been derived from the sound made by a raven’s wing as it sweeps through the air. Before white settlers came into the country that species of bird was very plentiful along all the streams, and at their points of confluence were its favorite roosting places, whence, aided by the scent of the water, it sallied up stream in search of food. Hundreds collected at the mouth of the Swanannoa, and the name was the oft repeated imitation, by the voice, of the music of their wings, as they whizzed past the morning camp-fire of the hunter or warrior bands, on the bank of the stream. The hungry, homely, and hated raven is indeed an humble origin for a name so beautiful, applied to an object so much applauded for its beauty.

If the upper tributaries of the French Broad ever had names worthy of their character which have been displaced by such colloquialisms as Cathey’s creek, Davidson’s river, Mills’ river, and Little river, they perished with the race more in sympathy with nature than the inhabitants of the last century. By some chance that gentle stream which snakes through the flat valley of Henderson county, has preserved an Indian designation, though it is probably a borrowed one. Ocklawaha is the name which we find in old legal documents, and its tributary, which gives the county’s capital a peninsular situation, is designated the Little Ocklawaha--a barbarous mixture of Indian and English. The word is of Seminole origin, and means “slowly moving water.” It was applied to a river in Florida by the natives, and to this Carolina stream by the “low country” people who found summer homes beyond the Blue Ridge, because of the applicability of the name and its resemblance in some other respects to the original Ochlawaha. Reverence of antiquity and the geographical genius of the red race, can not be claimed as an argument in favor of the re-substitution of the Indian designation for the present universally used colloquialism, “Mud creek,” as homely as it is false in the idea it suggests. Ochlawaha is not only more pleasing to the ear, but gives a much more faithful description of the landscape feature designated, and hence has sufficient claims to the public recognition which we take the lead in giving it.

Going southward, and crossing the Blue Ridge and Green river, which derives its name from the tint of its water, we come to the Saluda range, the fountain of a river of the same name. The word is of Catawba origin, as is also Estatoa. Toxaway, or more properly spelled Tochawha, is Cherokee, but we have no satisfactory interpretation of its meaning.

The Balsams are rich in legendary superstitions. The gloom of their dark solitudes fills even the hurried tourist with an unaccountable fear, and makes it impossible for him to suppress the recollection of tales of ghosts and goblins upon which his childish imagination was fed. The mountains assume mysterious shapes, projecting rocks seem to stand beckoning; and the echo of cascades falls upon the ear like ominous warnings. No wonder then, that it was a region peopled by pagan superstition, with other spirits than human. It is the instinct of the human mind, no matter what may be its degree of cultivation, to seek an explanation of things. When natural causes can not be discovered for the phenomena of nature, the supernatural is drawn upon. The Cherokees knew no natural reason why the tops of high mountains should be treeless, but having faith in a personal devil they jumped at the conclusion that the “bald” spots must be the prints of his horrid feet as he walked with giant strides from peak to peak.

Near the Great Divide, between the waters of Pigeon river and French Broad, is situated the Devil’s Court-house, which rises to an altitude of 6,049 feet. Near it is Court-house mountain. At both places his Satanic majesty was believed to sit in judgment, and doom to punishment all who had been wayward in courage, or had departed from a strict code of virtue, though bravery in war atoned for a multitude of sins.