The Yellowstone National Park: Historical and Descriptive. Hiram Martin Chittenden

The Yellowstone National Park: Historical and Descriptive - Hiram Martin Chittenden


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countries.”

      Of the Yellowstone River, he was told that it had its source “in a lake in the impenetrable fastnesses of the Rocky Mountains;” and that for some distance below the lake it flowed through a narrow gorge, up which “no one has ever been able to travel.”

Sources of the Yellowstone

      Opp. page 62.

      Click on image to view larger size.

      

      But it is the map prepared by Captain Raynolds that tells a more interesting story even than his written report. It reveals at once to the eye what was known as well as what was unknown of the Upper Yellowstone. Extending in a south-easterly and north-westerly direction, is a large elliptical space, within which geographical features are represented by dotted lines, indicating that they are put in by hearsay only. In the midst of a surrounding country, which is already mapped with great accuracy, there is a region wholly unknown to the geographer. A cordon of mountains encircles it, and shows the limit of official effort to gain a correct knowledge of it. Within this enchanted inclosure lies the region approximately defined by the 44th and 45th parallels of latitude and the 110th and 111th meridians of longitude, which now constitutes the Yellowstone National Park. There one may catch glimpses, through the uncertain haze of tradition, of the geysers, hot springs, Lake, Falls, Grand Cañon, Mammoth Hot Springs, and Two-Ocean Pass. This was the net result of fifty years' desultory wandering in and about and over this “mystic” region.

      Raynolds' report, it must be remembered, was the first official recognition in any form of the probable existence of extensive volcanic phenomena in the region of the Upper Yellowstone. Had it been published immediately after the expedition, and had not public attention been totally engrossed with other matters of overshadowing importance, this region must have become fully known in the early Sixties. But within a month after the return of Captain Raynolds to civilization there had taken place the national election which was the signal for attempted armed disruption of the Union. A year later found every officer of the Army called to new fields of duty. Western exploration entirely ceased until 1865, and was not vigorously resumed for some years thereafter. Captain Raynolds' report did not appear until 1868, although his map was published several years earlier in order to meet a demand for it by the new settlers in western Montana, Nothing transpired in the meantime to make the general public familiar with this region, and the picture here given is therefore substantially correct down to the date of the celebrated Washburn expedition.

      

      CHAPTER VIII.

      GOLD IN MONTANA.

      Perhaps the most fascinating pages of American history are those which recount the annals of the discoveries of gold and silver. No one can appreciate the magnitude of those various movements by a simple perusal of statistics of the mineral wealth which they disclosed. He must pass through the mining belts and note how almost every rod of ground, over vast tracts of country, is filled with prospect holes that attest the miner’s former presence. If the trapper carried the tools of his trade to haunts remote and inaccessible, the miner, with his pick and shovel, certainly outdid him. One can readily understand that, as soon as such a movement should be directed toward the region of the Upper Yellowstone, the wonders of that region would speedily be revealed.

      The presence of gold in the mountains of Montana was first noticed as far back as 1852. Later, in 1858, the Stuart brothers, James and Granville, founders of Montana, discovered gold in the Deer Lodge Valley; but they were destitute of equipments, and so constantly exposed to the hostility of the Blackfeet, that they went to Fort Bridger in the south-west corner of Wyoming, and did not return until late in 1860.

      It was in 1860 and 1861 that the rich mines on the Salmon and Boisé rivers were discovered. In 1862 the tide of discovery swept across the mountains into Montana. The rich mines on Pioneer Creek, the Big Prickly Pear, the Big Hole River, North Boulder Creek, and at Bannock and other points, became known. Although there were scarcely a thousand people in Montana in the winter of 1862–3, the news of the great discoveries marshaled a host of immigrants ready to enter the territory in the following spring. These were largely re-enforced by adventurers from both the northern and southern states, who, with little credit to their courage or patriotism, sought in these remote regions exemption from the tributes and levies of war. The immigrants were welcomed in the spring of 1863 by the news of the discovery of Alder Gulch, the richest of all gold placers. The work of prospecting, already being pushed with vigor, was stimulated to an extraordinary degree by this magnificent discovery. Prospecting parties scoured the country in all directions, often with loss of life through the Indians, but rarely, after the first two or three years, with any substantial success. Some of these expeditions have a particular connection with our narrative because they passed across portions of what is now the Yellowstone Park.

      The most important of them occurred in August and September, 1863. It was led by Walter W. DeLacy, an engineer and surveyor of some distinction in the early history of Montana. The party at one time numbered forty-two men, although this number did not continue constant throughout the expedition. Its sole object was to “prospect” the country. Evidently nothing in the line of topographical reconnaissance was thought of, for Captain DeLacy says “there was not a telescope, and hardly a watch, in the whole party.”

      The expedition left Virginia City, August 3d; passed south into Idaho until it struck the Snake River, and then ascended that stream to the region about Jackson Lake. Near the mouth of Buffalo Fork a halt was made, a corral was built to hold the stock, and a miners' meeting held at which rules were adopted to govern the miners in the contemplated examination of the country. The party then broke up into small groups and set out in different directions so as to cover as much ground as possible. The last four days of August were spent in this search, but with failure in every direction. This discouragement led to the abandonment of the expedition. Fifteen men set out for home by the way they had come, while DeLacy and twenty-seven men resolved to reach the Madison River and the settlements by going north. A day later this party entered the territory which is now the Yellowstone Park.

      The route lay up the Snake River to its junction with Lewis River where the hot springs of that locality were discovered. Here another separation occurred. About half the party went back down the river to re-examine a locality where they thought they had found some fair prospects. They soon returned, however, unsuccessful. The main party under DeLacy ascended the hills to the west of the river to seek a more practicable route. They soon reached the summit of the plateau where they discovered what are now Hering and Beula lakes, and noted their divergent drainage. Thence they passed north over Pitchstone Plateau until they struck the valley of Moose Creek. They descended this stream for a few miles and came to a large lake, which they supposed to be tributary to either the Madison or the Yellowstone Rivers. To their great surprise they found, upon rounding its southern point, that it drained south into the Snake. This is what is now called Shoshone Lake.

      From the outlet of the lake, DeLacy sent a man down stream to examine the river. This reconnaissance resulted in the discovery of Lewis Lake and the hot springs basin there. When DeLacy resumed his route, he followed along the east shore of the lake to its northern extremity, and then ascended the beautiful open valley of DeLacy Creek. He crossed the Continental Divide at the head of the valley, and camped on the evening of September 8th some miles beyond the Divide toward the Firehole River. The next morning, September 9, 1863, he came upon the considerable stream of hot water which flows down a mountain ravine into the Lower Geyser Basin close by the Great Fountain Geyser. The reader will learn with some amazement that our party thought little enough of this wonderful locality to pass directly through it without halt or perceptible delay. Before the camping hour of the afternoon had arrived, they were many miles away at the junction of the Gibbon and Firehole rivers.

      The other section of the party, which had gone down the Snake from its junction with Lewis River, soon returned, followed up the river to Lewis and Shoshone lakes, passed around the western end of the latter lake discovering its extensive geyser basin, and thence crossed over to the Madison. This stream they descended through the geyser basins, and followed the main party to the settlements.

      DeLacy


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