A New Guide for Emigrants to the West. John Mason Peck

north as the falls of St. Anthony, exhibits striking marks of a diluvial formation, by a gradual retiring of the waters. From the summit level that divides the waters of the lakes from those of the Mississippi, through Ohio, Indiana, Illinois, and Wisconsin, which is scarcely a perceptible ridge, to the south point of Illinois at the junction of the Ohio and Mississippi, appears to have once been a plane with an inclination equal to 12 or 15 inches per mile. The ravines and vallies appear to have been gradually scooped out by the abrasion of the waters.

      "The Lower Mississippi Valley, has a length of 1,200 miles, from northwest to southeast, considering the source of the Arkansas, and the mouth of the Mississippi river as extreme points; reaching from north latitude 29° to 42°, and without estimating mountains, ridges, or peaks, differs in relative elevation at least 500 feet.

      "The Arkansas river rises near north latitude 42°, and longitude 32° west from Washington, and falls into the Mississippi at 33° 56', passing over eight degrees of latitude.

      "Red River rises in the mountainous country of Mexico, north of Texas, in north latitude 34°; and west longitude 28° from Washington, and falls into the Mississippi in latitude 31°. They are both remarkable rivers for their extent, the number of their branches, the volume of their waters, the quantity of alluvion they carry down to the parent stream, and the color of their waters. Impregnated by saline particles, and colored with ocherous earth, the waters of these two rivers are at once brackish and nauseous to the taste, particularly near their mouths; that of Red river is so much so at Natchitoches at low water that it cannot be used for culinary purposes.

      "At a short distance below the mouth of the Red river, a large bayou, (as it is called,) or outlet, breaks from the Mississippi on the west; by which, it is believed, that as large a volume of water as the Red river brings to the parent river, is drained off, and runs to the gulf of Mexico, fifty miles from the mouth of the Mississippi. The name of this bayou is Atchafalaya, or as it is commonly called, Chaffalio. Below this bayou, another of large dimensions breaks forth on the same side, and finally falls into the Atchafalaya. This is the Placquemine. Still lower, at Donaldsonville, ninety miles above New Orleans, on the same side, the Lafourche bayou breaks out, and pursues a course parallel to the Mississippi, fifty miles west of the mouth of that river. On the east side, the Ibberville bayou drains off a portion of the waters of the Mississippi, into lakes Maurepas, Ponchartrain, Borgnes, and the gulf of Mexico, and thus forms the long and narrow island of Orleans.

      "In the lower Valley of the Mississippi there is a great extent of land of the very richest kind. There is also much that is almost always overflown with waters, and is a perpetual swamp. There are extensive prairies in this Valley; and towards the Rocky mountains; on the upper waters of the Arkansas and Red rivers, there are vast barren steppes or plains of sand, dreary and barren, like the central steppes of Asia. On the east of the Mississippi, are extensive regions of the densest forests, which form a striking contrast with the prairies which stretch on the west of that great river.

"The Valley of the Missouri extends 1200 miles in length, and 700 in width, and embraces 253,000 square miles. The Missouri river rises in the Chippewan mountains, through eight degrees, or nearly 600 miles. The Yellow Stone is its longest branch. The course of the Missouri, after leaving the Rocky mountains, is generally southeast, until it unites with the Mississippi. The principal branches flow from the southwest. They are the Osage, Kansas, Platte, &c. The three most striking features of this Valley are, 1st. The turbid character of its waters. 2d. The very unequal volumes of the right and left confluences. 3d. The immense predominance of the open prairies, over the forests which line the rivers. The western part of this Valley rises to an elevation towards the Chippewan mountains, equal to ten degrees of temperature. Ascending from the lower verge of this widely extended plain, wood becomes more and more scarce, until one naked surface spreads on all sides. Even the ridges and chains of the Chippewan, partake of these traits of desolation. The traveller, who has read the descriptions of central Asia, by Tooke or Pallas, will feel on the higher branches of the Missouri, a resemblance, at once striking and appalling; and he will acknowledge, if near to the Chippewan mountains in winter, that the utmost intensity of frost over Siberia and Mongolia, has its full counterpart in North America, on similar, if not on lower latitudes. There is much fertile land in the Valley of the Missouri, though much of it must be forever the abode of the buffalo and the elk, the wolf and the deer.[2]

FOOTNOTES:

      [1] Why the names Huron, Mandan, Sioux, Osage, and Ozark have been applied by Darby and other authors, to the extensive regions on the Upper Mississippi, the Upper Missouri, and the Arkansas rivers, I am not able to solve. Osage is a French corruption of Wos-sosh-ee, and Ozark is an awkward, illiterate corruption of Osage. Sioux is another French corruption, the origin of which is not now easily ascertained. Carver and other travellers, call this nation of Indiana Nau-do-wes-sees. Chiefs of this nation have repeatedly disclaimed the name of Sioux, (pronounced Soos.) They sometimes call themselves Da-co-tah.

[2] Darby.

CHAPTER II.

       Table of Contents

GENERAL VIEW OF THE VALLEY OF THE MISSISSIPPI.

       Table of Contents

      (CONTINUED.)

      Productions.

      Minerals.—But few mines exist in the Lower Valley of the Mississippi. Louisiana, being chiefly alluvion, furnishes only two specimens, sulphuret of antimony, and meteoric iron ore. It is supposed that the pine barrens towards Texas, if explored, would add to the number.

      The only minerals in Mississippi, are amethyst, of which one crystal has been found; potter's clay, at the Chickasaw Bluffs, and near Natchez; sulphuret of lead in small quantities, about Port Gibson; and sulphate of iron. Petrified trunks of trees are found in the bed of the Mississippi, opposite Natchez. In Arkansas Territory are various species. Here may be found the native magnet, or magnetic oxide of iron, possessing strong magnetic power. Iron ores are very abundant. Sulphate of copper, sulphuret of zinc, alum, and aluminous slate are found about the cove of Washitau, and the Hot Springs. Buhr stone of a superior quality exists in the surrounding hills. The hot springs are interesting on account of the minerals around them, the heat of their waters, and as furnishing a retreat to valetudinarians from the sickly regions of the south. They are situated on the Washitau, a large stream that empties itself into Red river.

      The lead mines of Missouri have been worked for more than a century. They are distributed through the country from thirty to one hundred miles southwest from St. Louis, and probably extend through the Gasconade country. Immense quantities of iron ore exist in this region. Lead is found in vast quantities in the northern part of Illinois, the south part of the Wisconsin Territory, and the country on the opposite side of the Mississippi. These mines are worked extensively. Native copper in large quantities is found in the same region. Large quantities of iron ore is found in the mountainous parts of Tennessee and Kentucky, where furnaces and forges have been erected. Also, in the hilly parts of Ohio, particularly at the falls of Licking four miles west of Zanesville, and in Adams and Lawrence counties near the Ohio river. With iron ore the West is profusely supplied.

      Bituminous coal exists in great profusion in various parts of the Western Valley. The hills around Pittsburg are inexhaustible. It extends through many portions of Ohio and Indiana. Nearly every county in Illinois is supplied with this valuable article. Missouri, Kentucky, and Tennessee have their share.