"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.
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