CHAPTER V.

EARLY KNOWLEDGE OF THE YELLOWSTONE.

On the west bank of the Yellowstone River, a quarter of a mile above the Upper Falls, in a ravine now crossed by a lofty wooden bridge, stands a pine tree, on which is the oldest record, except that of Colter, of the presence of white men within the present limits of the Park. It is an inscription, giving the initials of a name and the date when inscribed. It was discovered in 1880 by Col. P. W. Norris, then Superintendent of the Park. It is now practically illegible from overgrowth, although some of the characters can still be made out. Col. Norris, who saw it fifteen years ago, claims to have successfully deciphered it. He verified the date by counting the annual rings on another tree near by, which bore hatchet marks, presumably of the same date. The time that had elapsed since these cuts were made corresponded well with the inscribed date. The inscription was:

J O R Aug 19 1819

Efforts have been made to trace this inscription to some of the early noted trappers, but the attempt can hardly succeed. Even if an identity of initials were established, the identity of individuals would still remain in doubt. Nothing short of some authentic record of such a visit as must have taken place can satisfy the requirements of the case. In the absence of any such record, the most that can be said is that the inscription is proof positive that the Park country was visited by white men, after Colter's time, fully fifty years before its final discovery.

Col. Norris' researches disclosed other similar evidence, although in no other instance with so plain a clue as to date. Near Beaver Lake and Obsidian Cliff, he found, in 1878, a cache of marten traps of an old pattern used by the Hudson's Bay Company's trappers fifty years before. He also examined the ruins of an ancient block-house discovered by Frederick Bottler at the base of Mt. Washburn, near the Grand Cañon of the Yellowstone. Its decayed condition indicated great age. In other places, the stumps of trees, old logs used to cross streams, and many similar proofs, were brought to light by that inveterate ranger of the wilderness.

The Washburn party, in 1870, discovered on the east bank of the Yellowstone, just above Mud Geyser, the remains of a pit, probably once used for concealment in shooting water fowl.

In 1882, there was still living in Montana, at the advanced age of one hundred and two years, a Frenchman by the name of Baptiste Ducharne. This man spent the summers of 1824 and 1826 on the Upper Yellowstone River trapping for beaver. He saw the Grand Cañon and Falls of the Yellowstone and the Yellowstone Lake. He passed through the geyser regions, and could accurately describe them more than half a century after he had seen them.

A book called "The River of the West,"[P] published in 1871, but copyrighted in 1869, before the publication of any modern account of the geyser regions, contains the record of an adventure in the Yellowstone three years after those of Ducharne. The book is a biography of one Joseph Meek, a trapper and pioneer of considerable note. The adventure to which reference is made took place in 1829, and was the result of a decision by the Rocky Mountain Fur Company to retire from competition with the Hudson's Bay Company in the Snake River Valley. In leaving the country, Captain William Sublette, the chief partner, led his party up Henry Fork, across the Madison and Gallatin Rivers, to the high ridge overlooking the Yellowstone, at some point near the present Cinnabar Mountain. Here the party was dispersed by a band of Blackfeet, and Meek, one of its members, became separated from his companions. He had lost his horse and most of his equipment and in this condition he wandered for several days, without food or shelter, until he was found by two of his companions. His route lay in a southerly direction, to the eastward of the Yellowstone, at some distance back from the river. On the morning of the fifth day he had the following experience:

"Being desirous to learn something of the progress he had made, he ascended a low mountain in the neighborhood of his camp, and behold! the whole country beyond was smoking with vapor from boiling springs, and burning with gases issuing from small craters, each of which was emitting a sharp, whistling sound. When the first surprise of this astonishing scene had passed, Joe began to admire its effect from an artistic point of view. The morning being clear, with a sharp frost, he thought himself reminded of the City of Pittsburg, as he had beheld it on a winter morning, a couple of years before. This, however, related only to the rising smoke and vapor; for the extent of the volcanic region was immense, reaching far out of sight. The general face of the country was smooth and rolling, being a level plain, dotted with cone-shaped mounds. On the summit of these mounds were small craters from four to eight feet in diameter. Interspersed among these on the level plain were larger craters, some of them from four to six miles across. Out of these craters, issued blue flames and molten brimstone."[Q]

[P] See Appendix E.

[Q] Page 75, "River of the West."

Making some allowance for the trapper's tendency to exaggeration, we recognize in this description the familiar picture of the hot springs districts. The precise location is difficult to determine; but Meek's previous wanderings, and the subsequent route of himself and his companions whom he met here, show conclusively that it was one of the numerous districts east of the Yellowstone, which were possibly then more active than now.

This book affords much other evidence of early knowledge of the country immediately bordering the present Park. The Great Bend of the Yellowstone where Livingston now stands, was already a famous rendezvous. The Gardiner and Firehole Rivers were well known to trappers; and a much-used trail led from the Madison across the Gallatin Range to the Gardiner, and thence up the Yellowstone and East Fork across the mountains to the Bighorn Valley.

In Vol. I, No. 17, August 13, 1842, of _The Wasp_, a Mormon paper published at Nauvoo, Ill., occurs the first, as it is by far the best, of all early accounts of the geyser regions prior to 1870. It is an extract from an unpublished work, entitled _Life in the Rocky Mountains_. Who was the author will probably never be known; but that he was a man of culture and education, altogether beyond the average trader, is evident from the passing glimpse which we have of his work. He apparently made his visit from some point in the valley of Henry Fork not far west of the Firehole River, for, at the utmost allowance, he traveled only about sixty or seventy miles to reach the geyser basins. The evidence is conclusive that the scene of this visit was the Upper Geyser Basin. It fits perfectly with the description, while numerous insuperable discrepancies render identification with the Lower Basin, which some have sought to establish, impossible. Following is this writer's narrative:

"I had heard in the summer of 1833, while at rendezvous, that remarkable boiling springs had been discovered on the sources of the Madison, by a party of trappers, in their spring hunt; of which the accounts they gave, were so very astonishing, that I determined to examine them myself, before recording their description, though I had the united testimony of more than twenty men on the subject, who all declared they saw them, and that they really were as extensive and remarkable as they had been described. Having now an opportunity of paying them a visit, and as another or a better might not occur, I parted with the company after supper, and taking with me two Pend d'Oreilles (who were induced to take the excursion with me, by the promise of an extra present,) set out at a round pace, the night being clear and comfortable. We proceeded over the plain about twenty miles, and halted until daylight, on a fine spring, flowing into Camas Creek. Refreshed by a few hours' sleep, we started again after a hasty breakfast, and entered a very extensive forest, called the Pine Woods; (a continued succession of low mountains or hills, entirely covered with a dense growth of this species of timber;) which we passed through and reached the vicinity of the springs about dark, having seen several lakes or ponds on the sources of the Madison, and rode about forty miles; which was a hard day's ride, taking into consideration the rough irregularity of the country through which we traveled.

"We regaled ourselves with a cup of coffee, the materials for making which we had brought with us, and immediately after supper, lay down to rest, sleepy and much fatigued. The continual roaring of the springs, however, (which was distinctly heard,) for some time prevented my going to sleep, and excited an impatient curiosity to examine them, which I was obliged to defer the gratification of until morning, and filled my slumbers with visions of waterspouts, cataracts, fountains, _jets d'eau_ of immense dimensions, etc., etc.

"When I arose in the morning, clouds of vapor seemed like a dense fog to overhang the springs, from which frequent reports or explosions of different loudness, constantly assailed our ears. I immediately proceeded to inspect them, and might have exclaimed with the Queen of Sheba, when their full reality of dimensions and novelty burst upon my view, 'the half was not told me.'

"From the surface of a rocky plain or table, burst forth columns of water, of various dimensions, projecting high in the air, accompanied by loud explosions, and sulphurous vapors, which were highly disagreeable to the smell. The rock from which these springs burst forth was calcareous, and probably extends some distance from them, beneath the soil. The largest of these beautiful fountains projects a column of boiling water several feet in diameter, to the height of more than one hundred and fifty feet, in my opinion; but the party of Alvarez, who discovered it, persist in declaring that it could not be less than four times that distance in height--accompanied with a tremendous noise. These explosions and discharges occur at intervals of about two hours. After having witnessed three of them, I ventured near enough, to put my hand into the waters of its basin, but withdrew it instantly, for the heat of the water in this immense cauldron was altogether too great for my comfort; and the agitation of the water, the disagreeable effluvium continually exuding, and the hollow unearthly rumbling under the rock on which I stood, so ill accorded with my notions of personal safety, that I retreated back precipitately to a respectful distance. The Indians, who were with me, were quite appalled, and could not by any means be induced to approach them. They seemed astonished at my presumption in advancing up to the large one, and when I safely returned, congratulated me upon my 'narrow escape.' They believed them to be supernatural and supposed them to be the production of the Evil Spirit. One of them remarked that hell, of which he had heard from the whites, must be in that vicinity. The diameter of the basin into which the waters of the largest jet principally fall, and from the center of which, through a hole in the rock, of about nine or ten feet in diameter, the water spouts up as above related, may be about thirty feet. There are many other smaller fountains, that did not throw their waters up so high, but occurred at shorter intervals. In some instances the volumes were projected obliquely upward, and fell into the neighboring fountains, or on the rock or prairie. But their ascent was generally perpendicular, falling in and about their own basins or apertures.

"These wonderful productions of nature are situated near the center of a small valley, surrounded by pine-covered hills, through which a small fork of the Madison flows."

Here we have a description, as from the pen of some earlier Doane or Langford, free from exaggeration and true to the facts. No one who has seen the Upper Geyser Basin will question its general correctness. The writer then goes on to relate what he has learned from others, but here exaggeration creeps in and this part of his narrative is less reliable. It continues:

"From several trappers who had recently returned from the Yellow Stone, I received an account of boiling springs that differ from those seen on Salt River only in magnitude, being on a vastly larger scale; some of their cones are from twenty to thirty feet high, and forty to fifty paces in circumference. Those which have ceased to emit boiling, vapor, etc., of which there were several, are full of shelving cavities, even some fathoms in extent, which give them, inside, an appearance of honey-comb. The ground for several acres extent in vicinity of the springs is evidently hollow, and constantly exhales a hot steam or vapor of disagreeable odor, and a character entirely to prevent vegetation. They are situated in the valley at the head of that river near the lake, which constitutes its source.

"A short distance from these springs, near the margin of the lake, there is one quite different from any yet described. It is of a circular form, several feet in diameter, clear, cold and pure; the bottom appears visible to the eye, and seems seven or eight feet below the surface of the earth or water, without meeting any resistance. What is most singular with respect to this fountain is the fact that at regular intervals of about two minutes, a body or column of water bursts up to the height of eight feet, with an explosion as loud as the report of a musket, and then falls back into it; for a few seconds the water is roily, but it speedily settles and becomes transparent as before the effusion. A slight tremulous motion of the water, and a low rumbling sound from the caverns beneath, precede each explosion. This spring was believed to be connected with the lake by some subterranean passage, but the cause of its periodical eruptions or discharges, is entirely unknown. I have never before heard of a cold spring, whose waters exhibit the phenomena of periodical explosive propulsion, in form of a jet. The geysers of Iceland, and the various other European springs, the waters of which are projected upwards, with violence and uniformity, as well as those seen on the head waters of the Madison, are invariably hot."

The cold water geyser above described, although, apparently a myth, may not have been so after all. In many places along the west shore of the Yellowstone Lake there are visible protuberances in the water surface where boiling springs from beneath force the cold water upward. It is quite possible that this spring was so connected with the lake as to keep constantly filled with cold water to a considerable depth; and that the eruptive energy of the spring was expended in lifting the superincumbent mass without giving any visible indication of the thermal action below.

The whole article forms the most interesting and authentic reference to the geyser regions published prior to 1870. It proves beyond question that a knowledge of this region existed among the early trappers, and confirms our previous deduction that the wide range of the fur business could not have left it unexplored.

In a letter addressed by General Bonneville to the Montana Historical Society,[R] since the creation of the Yellowstone Park, he states that, at the time of his sojourn in the mountains, in 1831-4, the geyser regions were known to his men, although he had not personally seen them. He also remembered having seen the trader Alvarez, referred to in the above article.

[R] See Appendix E, "Transactions Montana Historical Society."

In 1844, a large party of trappers entered the Upper Yellowstone Valley from the south, passed around the west shore of the Yellowstone Lake to the outlet, where they had a severe battle with the Blackfeet Indians, in a broad open tract at that point. The remains of their old corral were still visible as late as 1870.

There are numerous other interesting, though less definite, references to an early knowledge of the Yellowstone; but those we have given show their general character. The important fact to remember is that this knowledge was barren of result. For the most part it existed only in the minds of illiterate men, and perished with them. It never caught the public ear and did not in the least degree hasten the final discovery. Historically interesting these early adventures will always be; as are also the Norse voyages to America; but they are very far from being the Columbus voyage of discovery.