Chapter VII: A Great Storm in Utah9 (2)

But notwithstanding the many porous fields thus fertilized, considerable portions of the waters of all these rivers continue to reach their old deathbeds in the desert, indicating that in these salt valleys there still is room for coming farmers. In middle and eastern Nevada, however, every rill that I have seen in a ride of three thousand miles, at all available for irrigation, has been claimed and put to use.

It appears, therefore, that under present conditions the limit of agricultural development in the dry basin between the Sierra and the Wahsatch has been already approached, a result caused not alone by natural restrictions as to the area capable of development, but by the extraordinary stimulus furnished by the mines to agricultural effort. The gathering of gold and silver, hay and barley, have gone on together. Most of the mid-valley bogs and meadows, and foothill rills capable of irrigating from ten to fifty acres, were claimed more than twenty years ago.

A majority of these pioneer settlers are plodding Dutchmen, living content in the back lanes and valleys of Nature; but the high price of all kinds of farm products tempted many of even the keen Yankee prospectors, made wise in California, to bind themselves down to this sure kind of mining. The wildest of wild hay, made chiefly of carices and rushes, was sold at from two to three hundred dollars per ton on ranches. The same kind of hay is still worth from fifteen to forty dollars per ton, according to the distance from mines and comparative security from competition. Barley and oats are from forty to one hundred dollars a ton, while all sorts of garden products find ready sale at high prices.

With rich mine markets and salubrious climate, the Nevada farmer can make more money by loose, ragged methods than the same class of farmers in any other State I have yet seen, while the almost savage isolation in which they live seems grateful to them. Even in those cases where the advent of neighbors brings no disputes concerning water rights and ranges, they seem to prefer solitude, most of them having been elected from adventurers from California—the pioneers of pioneers. The passing stranger, however, is always welcomed and supplied with the best the home affords, and around the fireside, while he smokes his pipe, very little encouragement is required to bring forth the story of the farmer’s life—hunting, mining, fighting, in the early Indian times, etc. Only the few who are married hope to return to California to educate their children, and the ease with which money is made renders the fulfillment of these hopes comparatively sure.

After dwelling thus long on the farms of this dry wonderland, my readers may be led to fancy them of more importance as compared with the unbroken fields of Nature than they really are. Making your way along any of the wide gray valleys that stretch from north to south, seldom will your eye be interrupted by a single mark of cultivation. The smooth lake-like ground sweeps on indefinitely, growing more and more dim in the glowing sunshine, while a mountain range from eight to ten thousand feet high bounds the view on either hand. No singing water, no green sod, no moist nook to rest in—mountain and valley alike naked and shadowless in the sun-glare; and though, perhaps, traveling a well-worn road to a gold or silver mine, and supplied with repeated instructions, you can scarce hope to find any human habitation from day to day, so vast and impressive is the hot, dusty, alkaline wildness.

But after riding some thirty or forty miles, and while the sun may be sinking behind the mountains, you come suddenly upon signs of cultivation. Clumps of willows indicate water, and water indicates a farm. Approaching more nearly, you discover what may be a patch of barley spread out unevenly along the bottom of a flood bed, broken perhaps, and rendered less distinct by boulder piles and the fringing willows of a stream. Speedily you can confidently say that the grain patch is surely such; its ragged bounds become clear; a sand-roofed cabin comes to view littered with sun-cracked implements and with an outer girdle of potato, cabbage, and alfalfa patches.

The immense expanse of mountain-girt valleys, on the edges of which these hidden ranches lie, make even the largest fields seem comic in size. The smallest, however, are by no means insignificant in a pecuniary view. On the east side of the Toyabe Range I discovered a jolly Irishman who informed me that his income from fifty acres, reinforced by a sheep range on the adjacent hills, was from seven to nine thousand dollars per annum. His irrigating brook is about four feet wide and eight inches deep, flowing about two miles per hour.

On Duckwater Creek, Nye County, Mr. Irwin has reclaimed a tule swamp several hundred acres in extent, which is now chiefly devoted to alfalfa. On twenty-five acres he claims to have raised this year thirty-seven tons of barley. Indeed, I have not yet noticed a meager crop of any kind in the State. Fruit alone is conspicuously absent.

On the California side of the Sierra grain will not ripen at much greater elevation than four thousand feet above sea level. The valleys of Nevada lie at a height of from four to six thousand feet, and both wheat and barley ripen, wherever water may be had, up to seven thousand feet. The harvest, of course, is later as the elevation increases. In the valleys of the Carson and Walker Rivers, four thousand feet above the sea, the grain harvest is about a month later than in California. In Reese River Valley, six thousand feet, it begins near the end of August. Winter grain ripens somewhat earlier, while occasionally one meets a patch of barley in some cool, high-lying cañon that will not mature before the middle of September.

Unlike California, Nevada will probably be always richer in gold and silver than in grain. Utah farmers hope to change the climate of the east side of the basin by prayer, and point to the recent rise in the waters of the Great Salt Lake as a beginning of moister times. But Nevada’s only hope, in the way of any considerable increase in agriculture, is from artesian wells. The experiment has been tried on a small scale with encouraging success. But what is now wanted seems to be the boring of a few specimen wells of a large size out in the main valleys. The encouragement that successful experiments of this kind would give to emigration seeking farms forms an object well worthy the attention of the Government. But all that California farmers in the grand central valley require is the preservation of the forests and the wise distribution of the glorious abundance of water from the snow stored on the west flank of the Sierra.

Whether any considerable area of these sage plains will ever thus be made to blossom in grass and wheat, experience will show. But in the mean time Nevada is beautiful in her wildness, and if tillers of the soil can thus be brought to see that possibly Nature may have other uses even for _rich_ soils besides the feeding of human beings, then will these foodless “deserts” have taught a fine lesson.

XIII. Nevada Forests[17]

When the traveler from California has crossed the Sierra and gone a little way down the eastern flank, the woods come to an end about as suddenly and completely as if, going westward, he had reached the ocean. From the very noblest forests in the world he emerges into free sunshine and dead alkaline lake-levels. Mountains are seen beyond, rising in bewildering abundance, range beyond range. But however closely we have been accustomed to associate forests and mountains, these always present a singularly barren aspect, appearing gray and forbidding and shadeless, like heaps of ashes dumped from the blazing sky.

But wheresoever we may venture to go in all this good world, nature is ever found richer and more beautiful than she seems, and nowhere may you meet with more varied and delightful surprises than in the byways and recesses of this sublime wilderness—lovely asters and abronias on the dusty plains, rose-gardens around the mountain wells, and resiny woods, where all seemed so desolate, adorning the hot foothills as well as the cool summits, fed by cordial and benevolent storms of rain and hail and snow; all of these scant and rare as compared with the immeasurable exuberance of California, but still amply sufficient throughout the barest deserts for a clear manifestation of God’s love.

Though Nevada is situated in what is called the “Great Basin,” no less than sixty-five groups and chains of mountains rise within the bounds of the State to a height of about from eight thousand to thirteen thousand feet above the level of the sea, and as far as I have observed, every one of these is planted, to some extent, with coniferous trees, though it is only upon the highest that we find anything that may fairly be called a forest. The lower ranges and the foothills and slopes of the higher are roughened with small scrubby junipers and nut pines, while the dominating peaks, together with the ridges that swing in grand curves between them, are covered with a closer and more erect growth of pine, spruce, and fir, resembling the forests of the Eastern States both as to size and general botanical characteristics. Here is found what is called the heavy timber, but the tallest and most fully developed sections of the forests, growing down in sheltered hollows on moist moraines, would be regarded in California only as groves of saplings, and so, relatively, they are, for by careful calculation we find that more than a thousand of these trees would be required to furnish as much timber as may be obtained from a single specimen of our Sierra giants.

The height of the timberline in eastern Nevada, near the middle of the Great Basin, is about eleven thousand feet above sea level; consequently the forests, in a dwarfed, storm-beaten condition, pass over the summits of nearly every range in the State, broken here and there only by mechanical conditions of the surface rocks. Only three mountains in the State have as yet come under my observation whose summits rise distinctly above the treeline. These are Wheeler’s Peak, twelve thousand three hundred feet high, Mount Moriah, about twelve thousand feet, and Granite Mountain, about the same height, all of which are situated near the boundary line between Nevada and Utah Territory.

In a rambling mountaineering journey of eighteen hundred miles across the state, I have met nine species of coniferous trees,—four pines, two spruces, two junipers, and one fir,—about one third the number found in California. By far the most abundant and interesting of these is the _Pinus Fremontiana_,[18] or nut pine. In the number of individual trees and extent of range this curious little conifer surpasses all the others combined. Nearly every mountain in the State is planted with it from near the base to a height of from eight thousand to nine thousand feet above the sea. Some are covered from base to summit by this one species, with only a sparse growth of juniper on the lower slopes to break the continuity of these curious woods, which, though dark-looking at a little distance, are yet almost shadeless, and without any hint of the dark glens and hollows so characteristic of other pine woods. Tens of thousands of acres occur in one continuous belt. Indeed, viewed comprehensively, the entire State seems to be pretty evenly divided into mountain ranges covered with nut pines and plains covered with sage—now a swath of pines stretching from north to south, now a swath of sage; the one black, the other gray; one severely level, the other sweeping on complacently over ridge and valley and lofty crowning dome.

The real character of a forest of this sort would never be guessed by the inexperienced observer. Traveling across the sage levels in the dazzling sunlight, you gaze with shaded eyes at the mountains rising along their edges, perhaps twenty miles away, but no invitation that is at all likely to be understood is discernible. Every mountain, however high it swells into the sky, seems utterly barren. Approaching nearer, a low brushy growth is seen, strangely black in aspect, as though it had been burned. This is a nut pine forest, the bountiful orchard of the red man. When you ascend into its midst you find the ground beneath the trees, and in the openings also, nearly naked, and mostly rough on the surface—a succession of crumbling ledges of lava, limestones, slate, and quartzite, coarsely strewn with soil weathered from them. Here and there occurs a bunch of sage or linosyris, or a purple aster, or a tuft of dry bunch-grass.

The harshest mountainsides, hot and waterless, seem best adapted to the nut pine’s development. No slope is too steep, none too dry; every situation seems to be gratefully chosen, if only it be sufficiently rocky and firm to afford secure anchorage for the tough, grasping roots. It is a sturdy, thickset little tree, usually about fifteen feet high when full grown, and about as broad as high, holding its knotty branches well out in every direction in stiff zigzags, but turning them gracefully upward at the ends in rounded bosses. Though making so dark a mass in the distance, the foliage is a pale grayish green, in stiff, awl-shaped fascicles. When examined closely these round needles seem inclined to be two-leaved, but they are mostly held firmly together, as if to guard against evaporation. The bark on the older sections is nearly black, so that the boles and branches are clearly traced against the prevailing gray of the mountains on which they delight to dwell.

The value of this species to Nevada is not easily overestimated. It furnishes fuel, charcoal, and timber for the mines, and, together with the enduring juniper, so generally associated with it, supplies the ranches with abundance of firewood and rough fencing. Many a square mile has already been denuded in supplying these demands, but, so great is the area covered by it, no appreciable loss has as yet been sustained. It is pretty generally known that this tree yields edible nuts, but their importance and excellence as human food is infinitely greater than is supposed. In fruitful seasons like this one, the pine nut crop of Nevada is, perhaps, greater than the entire wheat crop of California, concerning which so much is said and felt throughout the food markets of the world.

The Indians alone appreciate this portion of Nature’s bounty and celebrate the harvest home with dancing and feasting. The cones, which are a bright grass-green in color and about two inches long by one and a half in diameter, are beaten off with poles just before the scales open, gathered in heaps of several bushels, and lightly scorched by burning a thin covering of brushwood over them. The resin, with which the cones are bedraggled, is thus burned off, the nuts slightly roasted, and the scales made to open. Then they are allowed to dry in the sun, after which the nuts are easily thrashed out and are ready to be stored away. They are about half an inch long by a quarter of an inch in diameter, pointed at the upper end, rounded at the base, light brown in general color, and handsomely dotted with purple, like birds’ eggs. The shells are thin, and may be crushed between the thumb and finger. The kernels are white and waxy-looking, becoming brown by roasting, sweet and delicious to every palate, and are eaten by birds, squirrels, dogs, horses, and man. When the crop is abundant the Indians bring in large quantities for sale; they are eaten around every fireside in the State, and oftentimes fed to horses instead of barley.

Looking over the whole continent, none of Nature’s bounties seems to me so great as this in the way of food, none so little appreciated. Fortunately for the Indians and wild animals that gather around Nature’s board, this crop is not easily harvested in a monopolizing way. If it could be gathered like wheat the whole would be carried away and dissipated in towns, leaving the brave inhabitants of these wilds to starve.

Long before the harvest time, which is in September and October, the Indians examine the trees with keen discernment, and inasmuch as the cones require two years to mature from the first appearance of the little red rosettes of the fertile flowers, the scarcity or abundance of the crop may be predicted more than a year in advance. Squirrels, and worms, and Clarke crows, make haste to begin the harvest. When the crop is ripe the Indians make ready their long beating-poles; baskets, bags, rags, mats, are gotten together. The squaws out among the settlers at service, washing and drudging, assemble at the family huts; the men leave their ranch work; all, old and young, are mounted on ponies, and set off in great glee to the nut lands, forming cavalcades curiously picturesque. Flaming scarfs and calico skirts stream loosely over the knotty ponies, usually two squaws astride of each, with the small baby midgets bandaged in baskets slung on their backs, or balanced upon the saddle-bow, while the nut baskets and water jars project from either side, and the long beating-poles, like old-fashioned lances, angle out in every direction.

Arrived at some central point already fixed upon, where water and grass is found, the squaws with baskets, the men with poles, ascend the ridges to the laden trees, followed by the children; beating begins with loud noise and chatter; the burs fly right and left, lodging against stones and sagebrush; the squaws and children gather them with fine natural gladness; smoke columns speedily mark the joyful scene of their labors as the roasting fires are kindled; and, at night, assembled in circles, garrulous as jays, the first grand nut feast begins. Sufficient quantities are thus obtained in a few weeks to last all winter.

The Indians also gather several species of berries and dry them to vary their stores, and a few deer and grouse are killed on the mountains, besides immense numbers of rabbits and hares; but the pine-nuts are their main dependence—their staff of life, their bread.

Insects also, scarce noticed by man, come in for their share of this fine bounty. Eggs are deposited, and the baby grubs, happy fellows, find themselves in a sweet world of plenty, feeding their way through the heart of the cone from one nut chamber to another, secure from rain and wind and heat, until their wings are grown and they are ready to launch out into the free ocean of air and light.

XIV. Nevada’s Timber Belt[19]

The pine woods on the tops of the Nevada mountains are already shining and blooming in winter snow, making a most blessedly refreshing appearance to the weary traveler down on the gray plains. During the fiery days of summer the whole of this vast region seems so perfectly possessed by the sun that the very memories of pine trees and snow are in danger of being burned away, leaving one but little more than dust and metal. But since these first winter blessings have come, the wealth and beauty of the landscapes have come fairly into view, and one is rendered capable of looking and seeing.

The grand nut harvest is over, as far as the Indians are concerned, though perhaps less than one bushel in a thousand of the whole crop has been gathered. But the squirrels and birds are still busily engaged, and by the time that Nature’s ends are accomplished, every nut will doubtless have been put to use.

All of the nine Nevada conifers mentioned in my last letter are also found in California, excepting only the Rocky Mountain spruce, which I have not observed westward of the Snake Range. So greatly, however, have they been made to vary by differences of soil and climate, that most of them appear as distinct species. Without seeming in any way dwarfed or repressed in habit, they nowhere develop to anything like California dimensions. A height of fifty feet and diameter of twelve or fourteen inches would probably be found to be above the average size of those cut for lumber. On the margin of the Carson and Humboldt Sink the larger sage bushes are called “heavy timber”; and to the settlers here any tree seems large enough for saw-logs.

Mills have been built in the most accessible cañons of the higher ranges, and sufficient lumber of an inferior kind is made to supply most of the local demand. The principal lumber trees of Nevada are the white pine (_Pinus flexilis_), foxtail pine, and Douglas spruce, or “red pine,” as it is called here. Of these the first named is most generally distributed, being found on all the higher ranges throughout the State. In botanical characters it is nearly allied to the Weymouth, or white, pine of the Eastern States, and to the sugar and mountain pines of the Sierra. In open situations it branches near the ground and tosses out long down-curving limbs all around, often gaining in this way a very strikingly picturesque habit. It is seldom found lower than nine thousand feet above the level of the sea, but from this height it pushes upward over the roughest ledges to the extreme limit of tree growth—about eleven thousand feet.

On the Hot Creek, White Pine, and Golden Gate ranges we find a still hardier and more picturesque species, called the foxtail pine, from its long dense leaf-tassels. About a foot or eighteen inches of the ends of the branches are densely packed with stiff outstanding needles, which radiate all around like an electric fox- or squirrel-tail. The needles are about an inch and a half long, slightly curved, elastic, and glossily polished, so that the sunshine sifting through them makes them burn with a fine silvery luster, while their number and elastic temper tell delightfully in the singing winds.

This tree is pre-eminently picturesque, far surpassing not only its companion species of the mountains in this respect, but also the most noted of the lowland oaks and elms. Some stand firmly erect, feathered with radiant tail tassels down to the ground, forming slender, tapering towers of shining verdure; others with two or three specialized branches pushed out at right angles to the trunk and densely clad with the tasseled sprays, take the form of beautiful ornamental crosses. Again, in the same woods you find trees that are made up of several boles united near the ground, and spreading in easy curves at the sides in a plane parallel to the axis of the mountain, with the elegant tassels hung in charming order between them the whole making a perfect harp, ranged across the main wind-lines just where they may be most effective in the grand storm harmonies. And then there is an infinite variety of arching forms, standing free or in groups, leaning away from or toward each other in curious architectural structures,—innumerable tassels drooping under the arches and radiating above them, the outside glowing in the light, masses of deep shade beneath, giving rise to effects marvelously beautiful,—while on the roughest ledges of crumbling limestone are lowly old giants, five or six feet in diameter, that have braved the storms of more than a thousand years. But, whether old or young, sheltered or exposed to the wildest gales, this tree is ever found to be irrepressibly and extravagantly picturesque, offering a richer and more varied series of forms to the artist than any other species I have yet seen.

One of the most interesting mountain excursions I have made in the State was up through a thick spicy forest of these trees to the top of the highest summit of the Troy Range, about ninety miles to the south of Hamilton. The day was full of perfect Indian-summer sunshine, calm and bracing. Jays and Clarke crows made a pleasant stir in the foothill pines and junipers; grasshoppers danced in the hazy light, and rattled on the wing in pure glee, reviving suddenly from the torpor of a frosty October night to exuberant summer joy. The squirrels were working industriously among the falling nuts; ripe willows and aspens made gorgeous masses of color on the russet hillsides and along the edges of the small streams that threaded the higher ravines; and on the smooth sloping uplands, beneath the foxtail pines and firs, the ground was covered with brown grasses, enriched with sunflowers, columbines, and larkspurs and patches of linosyris, mostly frost-nipped and gone to seed, yet making fine bits of yellow and purple in the general brown.

At a height of about ninety-five hundred feet we passed through a magnificent grove of aspens, about a hundred acres in extent, through which the mellow sunshine sifted in ravishing splendor, showing every leaf to be as beautiful in color as the wing of a butterfly, and making them tell gloriously against the evergreens. These extensive groves of aspen are a marked feature of the Nevada woods. Some of the lower mountains are covered with them, giving rise to remarkably beautiful masses of pale, translucent green in spring and summer, yellow and orange in autumn, while in winter, after every leaf has fallen, the white bark of the boles and branches seen in mass seems like a cloud of mist that has settled close down on the mountain, conforming to all its hollows and ridges like a mantle, yet roughened on the surface with innumerable ascending spires.

Just above the aspens we entered a fine, close growth of foxtail pine, the tallest and most evenly planted I had yet seen. It extended along a waving ridge tending north and south and down both sides with but little interruption for a distance of about five miles. The trees were mostly straight in the bole, and their shade covered the ground in the densest places, leaving only small openings to the sun. A few of the tallest specimens measured over eighty feet, with a diameter of eighteen inches; but many of the younger trees, growing in tufts, were nearly fifty feet high, with a diameter of only five or six inches, while their slender shafts were hidden from top to bottom by a close, fringy growth of tasseled branchlets. A few white pines and balsam firs occur here and there, mostly around the edges of sunny openings, where they enrich the air with their rosiny fragrance, and bring out the peculiar beauties of the predominating foxtails by contrast.

Birds find grateful homes here—grouse, chickadees, and linnets, of which we saw large flocks that had a delightfully enlivening effect. But the woodpeckers are remarkably rare. Thus far I have noticed only one species, the golden-winged; and but few of the streams are large enough or long enough to attract the blessed ousel, so common in the Sierra.

On Wheeler’s Peak, the dominating summit of the Snake Mountains, I found all the conifers I had seen on the other ranges of the State, excepting the foxtail pine, which I have not observed further east than the White Pine range, but in its stead the beautiful Rocky Mountain spruce. First, as in the other ranges, we find the juniper and nut pine; then, higher, the white pine and balsam fir; then the Douglas spruce and this new Rocky Mountain spruce, which is common eastward from here, though this range is, as far as I have observed, its western limit. It is one of the largest and most important of Nevada conifers, attaining a height of from sixty to eighty feet and a diameter of nearly two feet, while now and then an exceptional specimen may be found in shady dells a hundred feet high or more.

The foliage is bright yellowish and bluish green, according to exposure and age, growing all around the branchlets, though inclined to turn upward from the undersides, like that of the plushy firs of California, making remarkably handsome fernlike plumes. While yet only mere saplings five or six inches thick at the ground, they measure fifty or sixty feet in height and are beautifully clothed with broad, level, fronded plumes down to the base, preserving a strict arrowy outline, though a few of the larger branches shoot out in free exuberance, relieving the spire from any unpicturesque stiffness of aspect, while the conical summit is crowded with thousands of rich brown cones to complete its beauty.

We made the ascent of the peak just after the first storm had whitened its summit and brightened the atmosphere. The foot-slopes are like those of the Troy range, only more evenly clad with grasses. After tracing a long, rugged ridge of exceedingly hard quartzite, said to be veined here and there with gold, we came to the North Dome, a noble summit rising about a thousand feet above the timberline, its slopes heavily tree-clad all around, but most perfectly on the north. Here the Rocky Mountain spruce forms the bulk of the forest. The cones were ripe; most of them had shed their winged seeds, and the shell-like scales were conspicuously spread, making rich masses of brown from the tops of the fertile trees down halfway to the ground, cone touching cone in lavish clusters. A single branch that might be carried in the hand would be found to bear a hundred or more.

Some portions of the wood were almost impenetrable, but in general we found no difficulty in mazing comfortably on over fallen logs and under the spreading boughs, while here and there we came to an opening sufficiently spacious for standpoints, where the trees around their margins might be seen from top to bottom. The winter sunshine streamed through the clustered spires, glinting and breaking into a fine dust of spangles on the spiky leaves and beads of amber gum, and bringing out the reds and grays and yellows of the lichened boles which had been freshened by the late storm; while the tip of every spire looking up through the shadows was dipped in deepest blue.

The ground was strewn with burs and needles and fallen trees; and, down in the dells, on the north side of the dome, where strips of aspen are imbedded in the spruces, every breeze sent the ripe leaves flying, some lodging in the spruce boughs, making them bloom again, while the fresh snow beneath looked like a fine painting.

Around the dome and well up toward the summit of the main peak, the snow-shed was well marked with tracks of the mule deer and the pretty stitching and embroidery of field mice, squirrels, and grouse; and on the way back to camp I came across a strange track, somewhat like that of a small bear, but more spreading at the toes. It proved to be that of a wolverine. In my conversations with hunters, both Indians and white men assure me that there are no bears in Nevada, notwithstanding the abundance of pine-nuts, of which they are so fond, and the accessibility of these basin ranges from their favorite haunts in the Sierra Nevada and Wahsatch Mountains. The mule deer, antelope, wild sheep, wolverine, and two species of wolves are all of the larger animals that I have seen or heard of in the State.

XV. Glacial Phenomena in Nevada[20]

The monuments of the Ice Age in the Great Basin have been greatly obscured and broken, many of the more ancient of them having perished altogether, leaving scarce a mark, however faint, of their existence—a condition of things due not alone to the long-continued action of post-glacial agents, but also in great part to the perishable character of the rocks of which they were made. The bottoms of the main valleys, once grooved and planished like the glacier pavements of the Sierra, lie buried beneath sediments and detritus derived from the adjacent mountains, and now form the arid sage plains; characteristic U-shaped cañons have become V-shaped by the deepening of their bottoms and straightening of their sides, and decaying glacier headlands have been undermined and thrown down in loose taluses, while most of the moraines and striae and scratches have been blurred or weathered away. Nevertheless, enough remains of the more recent and the more enduring phenomena to cast a good light well back upon the conditions of the ancient ice sheet that covered this interesting region, and upon the system of distinct glaciers that loaded the tops of the mountains and filled the cañons long after the ice sheet had been broken up.

The first glacial traces that I noticed in the basin are on the Wassuck, Augusta, and Toyabe ranges, consisting of ridges and cañons, whose trends, contours, and general sculpture are in great part specifically glacial, though deeply blurred by subsequent denudation. These discoveries were made during the summer of 1876-77. And again, on the 17th of last August, while making the ascent of Mount Jefferson, the dominating mountain of the Toquima range, I discovered an exceedingly interesting group of moraines, cañons with V-shaped cross sections, wide neve amphitheatres, moutoneed rocks, glacier meadows, and one glacier lake, all as fresh and telling as if the glaciers to which they belonged had scarcely vanished.

The best preserved and most regular of the moraines are two laterals about two hundred feet in height and two miles long, extending from the foot of a magnificent cañon valley on the north side of the mountain and trending first in a northerly direction, then curving around to the west, while a well-characterized terminal moraine, formed by the glacier towards the close of its existence, unites them near their lower extremities at a height of eighty-five hundred feet. Another pair of older lateral moraines, belonging to a glacier of which the one just mentioned was a tributary, extend in a general northwesterly direction nearly to the level of Big Smoky Valley, about fifty-five hundred feet above sea level.

Four other cañons, extending down the eastern slopes of this grand old mountain into Monito Valley, are hardly less rich in glacial records, while the effects of the mountain shadows in controlling and directing the movements of the residual glaciers to which all these phenomena belonged are everywhere delightfully apparent in the trends of the cañons and ridges, and in the massive sculpture of the neve wombs at their heads. This is a very marked and imposing mountain, attracting the eye from a great distance. It presents a smooth and gently curved outline against the sky, as observed from the plains, and is whitened with patches of enduring snow. The summit is made up of irregular volcanic tables, the most extensive of which is about two and a half miles long, and like the smaller ones is broken abruptly down on the edges by the action of the ice. Its height is approximately eleven thousand three hundred feet above the sea.

A few days after making these interesting discoveries, I found other well-preserved glacial traces on Arc Dome, the culminating summit of the Toyabe Range. On its northeastern slopes there are two small glacier lakes, and the basins of two others which have recently been filled with down-washed detritus. One small residual glacier lingered until quite recently beneath the coolest shadows of the dome, the moraines and névé-fountains of which are still as fresh and unwasted as many of those lying at the same elevation on the Sierra—ten thousand feet—while older and more wasted specimens may be traced on all the adjacent mountains. The sculpture, too, of all the ridges and summits of this section of the range is recognized at once as glacial, some of the larger characters being still easily readable from the plains at a distance of fifteen or twenty miles.

The Hot Creek Mountains, lying to the east of the Toquima and Monito ranges, reach the culminating point on a deeply serrate ridge at a height of ten thousand feet above the sea. This ridge is found to be made up of a series of imposing towers and pinnacles which have been eroded from the solid mass of the mountain by a group of small residual glaciers that lingered in their shadows long after the larger ice rivers had vanished. On its western declivities are found a group of well-characterized moraines, cañons, and _roches moutonnées_, all of which are unmistakably fresh and telling. The moraines in particular could hardly fail to attract the eye of any observer. Some of the short laterals of the glaciers that drew their fountain snows from the jagged recesses of the summit are from one to two hundred feet in height, and scarce at all wasted as yet, notwithstanding the countless storms that have fallen upon them, while cool rills flow between them, watering charming gardens of arctic plants—saxifrages, larkspurs, dwarf birch, ribes, and parnassia, etc.—beautiful memories of the Ice Age, representing a once greatly extended flora.

In the course of explorations made to the eastward of here, between the 38th and 40th parallels, I observed glacial phenomena equally fresh and demonstrative on all the higher mountains of the White Pine, Golden Gate, and Snake ranges, varying from those already described only as determined by differences of elevation, relations to the snow-bearing winds, and the physical characteristics of the rock formations.

On the Jeff Davis group of the Snake Range, the dominating summit of which is nearly thirteen thousand feet in elevation, and the highest ground in the basin, every marked feature is a glacier monument—peaks, valleys, ridges, meadows, and lakes. And because here the snow-fountains lay at a greater height, while the rock, an exceedingly hard quartzite, offered superior resistance to post-glacial agents, the ice-characters are on a larger scale, and are more sharply defined than any we have noticed elsewhere, and it is probably here that the last lingering glacier of the basin was located. The summits and connecting ridges are mere blades and points, ground sharp by the glaciers that descended on both sides to the main valleys. From one standpoint I counted nine of these glacial channels with their moraines sweeping grandly out to the plains to deep sheer-walled névé-fountains at their heads, making a most vivid picture of the last days of the Ice Period.

I have thus far directed attention only to the most recent and appreciable of the phenomena; but it must be borne in mind that less recent and less obvious traces of glacial action abound on _all_ the ranges throughout the entire basin, where the fine striae and grooves have been obliterated, and most of the moraines have been washed away, or so modified as to be no longer recognizable, and even the lakes and meadows, so characteristic of glacial regions, have almost entirely vanished. For there are other monuments, far more enduring than these, remaining tens of thousands of years after the more perishable records are lost. Such are the cañons, ridges, and peaks themselves, the glacial peculiarities of whose trends and contours cannot be hid from the eye of the skilled observer until changes have been wrought upon them far more destructive than those to which these basin ranges have yet been subjected.

It appears, therefore, that the last of the basin glaciers have but recently vanished, and that the almost innumerable ranges trending north and south between the Sierra and the Wahsatch Mountains were loaded with glaciers that descended to the adjacent valleys during the last glacial period, and that it is to this mighty host of ice streams that all the more characteristic of the present features of these mountain ranges are due.

But grand as is this vision delineated in these old records, this is not all; for there is not wanting evidence of a still grander glaciation extending over all the valleys now forming the sage plains as well as the mountains. The basins of the main valleys alternating with the mountain ranges, and which contained lakes during at least the closing portion of the Ice Period, were eroded wholly, or in part, from a general elevated tableland, by immense glaciers that flowed north and south to the ocean. The mountains as well as the valleys present abundant evidence of this grand origin.

The flanks of all the interior ranges are seen to have been heavily abraded and ground away by the ice acting in a direction parallel with their axes. This action is most strikingly shown upon projecting portions where the pressure has been greatest. These are shorn off in smooth planes and bossy outswelling curves, like the outstanding portions of cañon walls. Moreover, the extremities of the ranges taper out like those of dividing ridges which have been ground away by dividing and confluent glaciers. Furthermore, the horizontal sections of separate mountains, standing isolated in the great valleys, are lens-shaped like those of mere rocks that rise in the channels of ordinary cañon glaciers, and which have been overflowed or pastflowed, while in many of the smaller valleys _roches moutonnées_ occur in great abundance.

Again, the mineralogical and physical characters of the two ranges bounding the sides of many of the valleys indicate that the valleys were formed simply by the removal of the material between the ranges. And again, the rim of the general basin, where it is elevated, as for example on the southwestern portion, instead of being a ridge sculptured on the sides like a mountain range, is found to be composed of many short ranges, parallel to one another, and to the interior ranges, and so modeled as to resemble a row of convex lenses set on edge and half buried beneath a general surface, without manifesting any dependence upon synclinal or anticlinal axes—a series of forms and relations that could have resulted only from the outflow of vast basin glaciers on their courses to the ocean.

I cannot, however, present all the evidence here bearing upon these interesting questions, much less discuss it in all its relations. I will, therefore, close this letter with a few of the more important generalizations that have grown up out of the facts that I have observed. First, at the beginning of the glacial period the region now known as the Great Basin was an elevated tableland, not furrowed as at present with mountains and valleys, but comparatively bald and featureless.

Second, this tableland, bounded on the east and west by lofty mountain ranges, but comparatively open on the north and south, was loaded with ice, which was discharged to the ocean northward and southward, and in its flow brought most, if not all, the present interior ranges and valleys into relief by erosion.

Third, as the glacial winter drew near its close the ice vanished from the lower portions of the basin, which then became lakes, into which separate glaciers descended from the mountains. Then these mountain glaciers vanished in turn, after sculpturing the ranges into their present condition.

Fourth, the few immense lakes extending over the lowlands, in the midst of which many of the interior ranges stood as islands, became shallow as the ice vanished from the mountains, and separated into many distinct lakes, whose waters no longer reached the ocean. Most of these have disappeared by the filling of their basins with detritus from the mountains, and now form sage plains and “alkali flats.”

The transition from one to the other of these various conditions was gradual and orderly: first, a nearly simple tableland; then a grand _mer de glace_ shedding its crawling silver currents to the sea, and becoming gradually more wrinkled as unequal erosion roughened its bed, and brought the highest peaks and ridges above the surface; then a land of lakes, an almost continuous sheet of water stretching from the Sierra to the Wahsatch, adorned with innumerable island mountains; then a slow desiccation and decay to present conditions of sage and sand.

XVI. Nevada’s Dead Towns[21]

Nevada is one of the very youngest and wildest of the States; nevertheless it is already strewn with ruins that seem as gray and silent and time-worn as if the civilization to which they belonged had perished centuries ago. Yet, strange to say, all these ruins are results of mining efforts made within the last few years. Wander where you may throughout the length and breadth of this mountain-barred wilderness, you everywhere come upon these dead mining towns, with their tall chimney stacks, standing forlorn amid broken walls and furnaces, and machinery half buried in sand, the very names of many of them already forgotten amid the excitements of later discoveries, and now known only through tradition—tradition ten years old.

While exploring the mountain ranges of the State during a considerable portion of three summers, I think that I have seen at least five of these deserted towns and villages for every one in ordinary life. Some of them were probably only camps built by bands of prospectors, and inhabited for a few months or years, while some specially interesting cañon was being explored, and then carelessly abandoned for more promising fields. But many were real towns, regularly laid out and incorporated, containing well-built hotels, churches, schoolhouses, post offices, and jails, as well as the mills on which they all depended; and whose well-graded streets were filled with lawyers, doctors, brokers, hangmen, real estate agents, etc., the whole population numbering several thousand.

A few years ago the population of Hamilton is said to have been nearly eight thousand; that of Treasure Hill, six thousand; of Shermantown, seven thousand; of Swansea, three thousand. All of these were incorporated towns with mayors, councils, fire departments, and daily newspapers. Hamilton has now about one hundred inhabitants, most of whom are merely waiting in dreary inaction for something to turn up. Treasure Hill has about half as many, Shermantown one family, and Swansea none, while on the other hand the graveyards are far too full.

In one cañon of the Toyabe range, near Austin, I found no less than five dead towns without a single inhabitant. The streets and blocks of “real estate” graded on the hillsides are rapidly falling back into the wilderness. Sagebrushes are growing up around the forges of the blacksmith shops, and lizards bask on the crumbling walls.

While traveling southward from Austin down Big Smoky Valley, I noticed a remarkably tall and imposing column, rising like a lone pine out of the sagebrush on the edge of a dry gulch. This proved to be a smokestack of solid masonry. It seemed strangely out of place in the desert, as if it had been transported entire from the heart of some noisy manufacturing town and left here by mistake. I learned afterwards that it belonged to a set of furnaces that were built by a New York company to smelt ore that never was found. The tools of the workmen are still lying in place beside the furnaces, as if dropped in some sudden Indian or earthquake panic and never afterwards handled. These imposing ruins, together with the desolate town, lying a quarter of a mile to the northward, present a most vivid picture of wasted effort. Coyotes now wander unmolested through the brushy streets, and of all the busy throng that so lavishly spent their time and money here only one man remains—a lone bachelor with one suspender.

Mining discoveries and progress, retrogression and decay, seem to have been crowded more closely against each other here than on any other portion of the globe. Some one of the band of adventurous prospectors who came from the exhausted placers of California would discover some rich ore—how much or little mattered not at first. These specimens fell among excited seekers after wealth like sparks in gunpowder, and in a few days the wilderness was disturbed with the noisy clang of miners and builders. A little town would then spring up, and before anything like a careful survey of any particular lode would be made, a company would be formed, and expensive mills built. Then, after all the machinery was ready for the ore, perhaps little, or none at all, was to be found. Meanwhile another discovery was reported, and the young town was abandoned as completely as a camp made for a single night; and so on, until some really valuable lode was found, such as those of Eureka, Austin, Virginia, etc., which formed the substantial groundwork for a thousand other excitements.

Passing through the dead town of Schellbourne last month, I asked one of the few lingering inhabitants why the town was built. “For the mines,” he replied. “And where are the mines?” “On the mountains back here.” “And why were they abandoned?” I asked. “Are they exhausted?” “Oh, no,” he replied, “they are not exhausted; on the contrary, they have never been worked at all, for unfortunately, just as we were about ready to open them, the Cherry Creek mines were discovered across the valley in the Egan range, and everybody rushed off there, taking what they could with them—houses machinery, and all. But we are hoping that somebody with money and speculation will come and revive us yet.”

The dead mining excitements of Nevada were far more intense and destructive in their action than those of California, because the prizes at stake were greater, while more skill was required to gain them. The long trains of gold-seekers making their way to California had ample time and means to recover from their first attacks of mining fever while crawling laboriously across the plains, and on their arrival on any portion of the Sierra gold belt, they at once began to make money. No matter in what gulch or cañon they worked, some measure of success was sure, however unskillful they might be. And though while making ten dollars a day they might be agitated by hopes of making twenty, or of striking their picks against hundred- or thousand-dollar nuggets, men of ordinary nerve could still work on with comparative steadiness, and remain rational.

But in the case of the Nevada miner, he too often spent himself in years of weary search without gaining a dollar, traveling hundreds of miles from mountain to mountain, burdened with wasting hopes of discovering some hidden vein worth millions, enduring hardships of the most destructive kind, driving innumerable tunnels into the hillsides, while his assayed specimens again and again proved worthless. Perhaps one in a hundred of these brave prospectors would “strike it rich,” while ninety-nine died alone in the mountains or sank out of sight in the corners of saloons, in a haze of whiskey and tobacco smoke.

The healthful ministry of wealth is blessed; and surely it is a fine thing that so many are eager to find the gold and silver that lie hid in the veins of the mountains. But in the search the seekers too often become insane, and strike about blindly in the dark like raving madmen. Seven hundred and fifty tons of ore from the original Eberhardt mine on Treasure Hill yielded a million and a half dollars, the whole of this immense sum having been obtained within two hundred and fifty feet of the surface, the greater portion within one hundred and forty feet. Other ore masses were scarcely less marvelously rich, giving rise to one of the most violent excitements that ever occurred in the history of mining. All kinds of people—shoemakers, tailors, farmers, etc., as well as miners—left their own right work and fell in a perfect storm of energy upon the White Pine Hills, covering the ground like grasshoppers, and seeming determined by the very violence of their efforts to turn every stone to silver. But with few exceptions, these mining storms pass away about as suddenly as they rise, leaving only ruins to tell of the tremendous energy expended, as heaps of giant boulders in the valley tell of the spent power of the mountain floods.

In marked contrast with this destructive unrest is the orderly deliberation into which miners settle in developing a truly valuable mine. At Eureka we were kindly led through the treasure chambers of the Richmond and Eureka Consolidated, our guides leisurely leading the way from level to level, calling attention to the precious ore masses which the workmen were slowly breaking to pieces with their picks, like navvies wearing away the day in a railroad cutting; while down at the smelting works the bars of bullion were handled with less eager haste than the farmer shows in gathering his sheaves.

The wealth Nevada has already given to the world is indeed wonderful, but the only grand marvel is the energy expended in its development. The amount of prospecting done in the face of so many dangers and sacrifices, the innumerable tunnels and shafts bored into the mountains, the mills that have been built—these would seem to require a race of giants. But, in full view of the substantial results achieved, the pure waste manifest in the ruins one meets never fails to produce a saddening effect.