Although, but a few days' travel above where we now were, the Canadian runs pent up in a narrow channel, scarcely four rods [or 22 yards] across, we here found it spread out to the width of from three to six hundred yards, and so full of sand-bars (only interspersed with narrow rills) as to present the appearance of a mere sandy valley instead of the bed of a river. In fact, during the driest seasons, the water wholly disappears in many places. Captain Boone (Nathan Boone, the youngest son of the noted pioneer Daniel.), of the U. S. Dragoons, being upon an exploring expedition in the summer of 1843, came to the Canadian about the region of our western boundary, where he found the channel perfectly dry. Notwithstanding it presents the face of one of the greatest rivers of the west during freshets, yet even then it would not be navigable on account of its rapidity and shallowness. It would appear almost incredible to those unacquainted with the prairie streams, that a river of about 1500 miles in length, and whose head wears a cap of perennial snow (having its source in the Rocky Mountains), should scarcely be navigable, for even the smallest craft, over fifty miles above its mouth.
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p.212Josiah Gregg
If we take a retrospective view of the country over which we traveled, we shall find but little that can ever present attractions to the agriculturist. Most of the low valleys of the Canadian, for a distance of five hundred miles, are either too sandy or too marshy for cultivation; and the upland prairies are, in many places, but little else than sand-hills. In some parts, it is true, they are firm and fertile, but wholly destitute of timber, with the exception of a diminutive branch of the Cross Timbers, which occupies a portion of the ridge betwixt the Canadian and the North Fork. The Canadian river itself is still more bare of timber than the upper Arkansas. In its whole course through the plains, there is but little except cottonwood, and that very scantily scattered along its banks — in some places, for leagues together, not a stick is to be seen. Except it be near the Mountains, where the valleys are more fertile, it is only the little narrow bottoms which skirt many of its tributary rivulets that indicate any amenity. Some of these are rich and beautiful in the extreme, timbered with walnut, mulberry, oak, elm, hackberry, and occasionally cedar about the bluffs.
Josiah Gregg
The most notable of the great plateaus of the Prairies is that known to Mexicans as El Llano Estacado, which is bounded on the north by the Canadian river — extends east about to the United States boundary, including the heads of the False Washita and other branches of Red River — and spreads southward to the sources of Trinity, Brazos and Colorado rivers, and westward to Rio Pecos. It is quite an elevated and generally a level plain, without important hills or ridges, unless we distinguish as such the craggy breaks of the streams which border and pierce it. It embraces an area of about 30,000 square miles, most of which is without water during three-fourths of the year; while a large proportion of its few perennial streams are too brackish to drink of.
Josiah Gregg
With such inexhaustible mines of salt within two or three days' journey of the Arkansas river, and again within the same distance of the Missouri, which would cost no further labor than the digging it up and the transporting of it to boats for freighting it down those streams, it seems strange that they should lie idle, while we are receiving much of our supplies of this indispensable commodity from abroad. Besides the salines already mentioned, there is one high on the Canadian river, some two hundred miles east of Santa Fé. Also, it is said, there are some to be found on the waters of Red River; and numerous others are no doubt scattered throughout the same regions, which have never been discovered.
Josiah Gregg
After fording the Rio Cármen, which, though usually without a drop of water in its channel, we now found a very turbulent stream, we did not meet with any object particularly worthy of remark, until we reached the Laguna de Encinillas [Lake of Live-Oaks, the size varies greatly with the season of drouth or rain.—Book Editor]. This lake is ten or twelve miles long by two or three in width, and seems to have no outlet even during the greatest freshets, though fed by several small constantly flowing streams from the surrounding mountains. The water of this lake during the dry season is so strongly impregnated with nauseous and bitter salts, as to render it wholly unpalatable to man and beast. The most predominant of these noxious substances is a species of alkali, known there by the title of tequesquite. It is often seen oozing out from the surface of marshy grounds, about the table plains of all Northern Mexico, forming a grayish crust, and is extensively used in the manufacture of soap, and sometimes by the bakers even for raising bread. Here we had another evidence of the alarming effects of the recent flood, the road for several miles along the margin of the lake being completely inundated. It was, however, in the city of Chihuahua itself that the disastrous consequences of the freshet were most severely felt. Some inferior houses of adobe were so much soaked by the rains, that they tumbled to the ground, occasioning the loss of several lives.
Josiah Gregg
After leaving El Paso, our road branched off at an angle of about two points to the westward of the river, the city of Chihuahua being situated nearly a hundred miles to the west of it. At the distance of about thirty miles we reached Los Médanos [The Dunes], a stupendous ledge of sand-hills, across which the road passes for about six miles. As teams are never able to haul the loaded wagons over this region of loose sand, we engaged an atajo of mules at El Paso, upon which to convey our goods across. These Médanos consist of huge hillocks and ridges of pure sand, in many places without a vestige of vegetation. Through the lowest gaps between the hills, the road winds its way.
Josiah Gregg
Gregg, Josiah
Gregory I, Gregory the Great
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