[1] A Short Spear.

The dryness and purity of the air roused the admiration of the explorers, who noticed that the woodwork of

The cases of their instruments shrank, and the joints opened, although the wood was old and perfectly seasoned. A tablespoonful of water, exposed to the air in an open saucer, would wholly evaporate in thirty-six hours, when the thermometer did not mark higher than the "Temperate" point at the warmest hour of the day. Contrary to their expectations, they had not yet met with any Indians, although they saw many signs of their having recently been in that vicinity. The journal says:

"In the course of the day [May 30] we passed several encampments of Indians, the most recent of which seemed to have been evacuated about five weeks since; and, from the several apparent dates, we supposed that they were formed by a band of about one hundred lodges, who were travelling slowly up the river. Although no part of the Missouri from the Minnetarees to this place exhibits signs of permanent settlements, yet none seem exempt from the transient visits of hunting-parties. We know that the Minnetarees of the Missouri extend their excursions on the south side of the river as high as the Yellowstone, and the Assiniboins visit the northern side, most probably as high as Porcupine River. All the lodges between that place and the Rocky Mountains we supposed to belong to the Minnetarees of Fort de Prairie, who live on the south fork of the Saskashawan."

The party now entered upon some of the natural wonders of the West, which have since become famous. Their journal says: -

"These hills and river-cliffs exhibit a most extraordinary and romantic appearance. They rise in most places nearly perpendicular from the water, to the height of between two hundred and three hundred feet, and are formed of very white sandstone, so soft as to yield readily to the impression of water, in the upper part of which lie imbedded two or three thin horizontal strata of white freestone, insensible to the rain; on the top is a dark rich loam, which forms a gradually ascending plain, from a mile to a mile and a half in extent, when the hills again rise abruptly to the height of about three hundred feet more. In trickling down the cliffs, the water has worn the soft sandstone into a thousand grotesque figures, among which, with a little fancy, may be discerned elegant ranges of freestone buildings, with columns variously sculptured, and supporting long and elegant galleries, while the parapets are adorned with statuary. On a nearer approach they represent every form of elegant ruins - columns, some with pedestals and capitals entire, others mutilated and prostrate, and some rising pyramidally over each other till they terminate in a sharp point. These are varied by niches, alcoves, and the customary appearances of desolated magnificence. The illusion is increased by the number of martins, which have built their globular nests in the niches, and hover over these columns, as in our country they are accustomed to frequent large stone structures. As we advance there seems no end to the visionary enchantment which surrounds us.

"In the midst of this fantastic scenery are vast ranges of walls, which seem the productions of art, so regular is the workmanship. They rise perpendicularly from the river, sometimes to the height of one hundred feet, varying in thickness from one to twelve feet, being as broad at the top as below. The stones of which they are formed are black, thick, durable, and composed of a large portion of earth, intermixed and cemented with a small quantity of sand and a considerable proportion of talk [talc] or quartz. These stones are almost invariably regular parallelopipeds of unequal sizes in the wall, but equally deep and laid regularly in ranges over each other like bricks, each breaking and covering the interstice of the two on which it rests; but though the perpendicular interstice be destroyed, the horizontal one extends entirely through the whole work. The stones are proportioned to the thickness of the wall in which they are employed, being largest in the thickest walls. The thinner walls are composed of a single depth of the parallelopiped, while the thicker ones consist of two or more depths. These walls pass the river at several places, rising from the water's edge much above the sandstone bluffs, which they seem to penetrate; thence they cross in a straight line, on either side of the river, the plains, over which they tower to the height of from ten to seventy feet, until they lose themselves in the second range of hills. Sometimes they run parallel in several ranges near to each other, sometimes intersect each other at right angles, and have the appearance of walls of ancient houses or gardens."

The wall-like, canyon formations were charted by Lewis and Clark as "The Stone Walls." Their fantastic outlines have been admired and described by modern tourists, and some of them have been named "Cathedral Rocks," "Citadel Rock," "Hole in the Wall," and so on.

Passing out of this wonderful region, the expedition entered upon a more level country, here and there broken by bluffy formations which extended along the river, occasionally interspersed with low hills. Their journal says:

"In the plains near the river are the choke-cherry, yellow and red currant bushes, as well as the wild rose and prickly pear, both of which are now in bloom. From the tops of the river-hills, which are lower than usual, we enjoyed a delightful view of the rich, fertile plains on both sides, in many places extending from the river-cliffs to a great distance back. In these plains we meet, occasionally, large banks of pure sand, which were driven apparently by the southwest winds and there deposited. The plains are more fertile some distance from the river than near its banks, where the surface of the earth is very generally strewed with small pebbles, which appear to be smoothed and worn by the agitation of the waters with which they were, no doubt, once covered."

Under date of June 2d, the journal says:

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