Steep Trails

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, canyons, and roches moutonnees, 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 neve-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 canyons, 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 canyon 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 canyon glaciers, and which have been overflowed or pastflowed, while in many of the smaller valleys roches moutonnees 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 Towns21

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 canyon 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 canyon 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 canyon 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.

The dim old ruins of Europe, so eagerly sought after by travelers, have something pleasing about them, whatever their historical associations; for they at least lend some beauty to the landscape. Their picturesque towers and arches seem to be kindly adopted by nature, and planted with wild flowers and wreathed with ivy; while their rugged angles are soothed and freshened and embossed with green mosses, fresh life and decay mingling in pleasing measures, and the whole vanishing softly like a ripe, tranquil day fading into night. So, also, among the older ruins of the East there is a fitness felt. They have served their time, and like the weather-beaten mountains are wasting harmoniously. The same is in some degree true of the dead mining towns of California.

But those lying to the eastward of the Sierra throughout the ranges of the Great Basin waste in the dry wilderness like the bones of cattle that have died of thirst. Many of them do not represent any good accomplishment, and have no right to be. They are monuments of fraud and ignorance—sins against science. The drifts and tunnels in the rocks may perhaps be regarded as the prayers of the prospector, offered for the wealth he so earnestly craves; but, like prayers of any kind not in harmony with nature, they are unanswered. But, after all, effort, however misapplied, is better than stagnation. Better toil blindly, beating every stone in turn for grains of gold, whether they contain any or not, than lie down in apathetic decay.

The fever period is fortunately passing away. The prospector is no longer the raving, wandering ghoul of ten years ago, rushing in random lawlessness among the hills, hungry and footsore; but cool and skillful, well supplied with every necessary, and clad in his right mind. Capitalists, too, and the public in general, have become wiser, and do not take fire so readily from mining sparks; while at the same time a vast amount of real work is being done, and the ratio between growth and decay is constantly becoming better.

XVII. Puget Sound

Washington Territory, recently admitted22 into the Union as a State, lies between latitude 46 degrees and 49 degrees and longitude 117 degrees and 125 degrees, forming the northwest shoulder of the United States. The majestic range of the Cascade Mountains naturally divides the State into two distinct parts, called Eastern and Western Washington, differing greatly from each other in almost every way, the western section being less than half as large as the eastern, and, with its copious rains and deep fertile soil, being clothed with forests of evergreens, while the eastern section is dry and mostly treeless, though fertile in many parts, and producing immense quantities of wheat and hay. Few States are more fertile and productive in one way or another than Washington, or more strikingly varied in natural features or resources.

Within her borders every kind of soil and climate may be found—the densest woods and dryest plains, the smoothest levels and roughest mountains. She is rich in square miles (some seventy thousand of them), in coal, timber, and iron, and in sheltered inland waters that render these resources advantageously accessible. She also is already rich in busy workers, who work hard, though not always wisely, hacking, burning, blasting their way deeper into the wilderness, beneath the sky, and beneath the ground. The wedges of development are being driven hard, and none of the obstacles or defenses of nature can long withstand the onset of this immeasurable industry.

Puget Sound, so justly famous the world over for the surpassing size and excellence and abundance of its timber, is a long, many-fingered arm of the sea reaching southward from the head of the Strait of Juan de Fuca into the heart of the grand forests of the western portion of Washington, between the Cascade Range and the mountains of the coast. It is less than a hundred miles in length, but so numerous are the branches into which it divides, and so many its bays, harbors, and islands, that its entire shoreline is said to measure more than eighteen hundred miles. Throughout its whole vast extent ships move in safety, and find shelter from every wind that blows, the entire mountain-girt sea forming one grand unrivaled harbor and center for commerce.

The forest trees press forward to the water around all the windings of the shores in most imposing array, as if they were courting their fate, coming down from the mountains far and near to offer themselves to the axe, thus making the place a perfect paradise for the lumberman. To the lover of nature the scene is enchanting. Water and sky, mountain and forest, clad in sunshine and clouds, are composed in landscapes sublime in magnitude, yet exquisitely fine and fresh, and full of glad, rejoicing life. The shining waters stretch away into the leafy wilderness, now like the reaches of some majestic river and again expanding into broad roomy spaces like mountain lakes, their farther edges fading gradually and blending with the pale blue of the sky. The wooded shores with an outer fringe of flowering bushes sweep onward in beautiful curves around bays, and capes, and jutting promontories innumerable; while the islands, with soft, waving outlines, lavishly adorned with spruces and cedars, thicken and enrich the beauty of the waters; and the white spirit mountains looking down from the sky keep watch and ward over all, faithful and changeless as the stars.

All the way from the Strait of Juan de Fuca up to Olympia, a hopeful town situated at the head of one of the farthest-reaching of the fingers of the Sound, we are so completely inland and surrounded by mountains that it is hard to realize that we are sailing on a branch of the salt sea. We are constantly reminded of Lake Tahoe. There is the same clearness of the water in calm weather without any trace of the ocean swell, the same picturesque winding and sculpture of the shoreline and flowery, leafy luxuriance; only here the trees are taller and stand much closer together, and the backgrounds are higher and far more extensive. Here, too, we find greater variety amid the marvelous wealth of islands and inlets, and also in the changing views dependent on the weather. As we double cape after cape and round the uncounted islands, new combinations come to view in endless variety, sufficient to fill and satisfy the lover of wild beauty through a whole life.

Oftentimes in the stillest weather, when all the winds sleep and no sign of storms is felt or seen, silky clouds form and settle over all the land, leaving in sight only a circle of water with indefinite bounds like views in mid-ocean; then, the clouds lifting, some islet will be presented standing alone, with the tops of its trees dipping out of sight in pearly gray fringes; or, lifting higher, and perhaps letting in a ray of sunshine through some rift overhead, the whole island will be set free and brought forward in vivid relief amid the gloom, a girdle of silver light of dazzling brightness on the water about its shores, then darkening again and vanishing back into the general gloom. Thus island after island may be seen, singly or in groups, coming and going from darkness to light like a scene of enchantment, until at length the entire cloud ceiling is rolled away, and the colossal cone of Mount Rainier is seen in spotless white looking down over the forests from a distance of sixty miles, but so lofty and so massive and clearly outlined as to impress itself upon us as being just back of a strip of woods only a mile or two in breadth.