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JUDGES OF THE SUPREME COURT.
Edward V. Whiton, Judge of 1st Circuit . . . . 1848. Levi Hubbell, 55 2d 25 . . . . 1848. Charles H. Larrabee, ’’ 3d 35 . . . . 1848. Alexander W. Stow, " 4th 22 . . . . 1848.
M. M. Jackson, 35 5th 22 . . . . 1848. Wiram Knowlton, 55 6th 22 . . . . 1850. Timothy O. Howe, 55 4th '' . . . . 1850. Levi Hubbell, 55 2d 35 . . . . 1851. M. M. Cothren, 55 5th 22 . . . . 1852.
SEPARATE, OR NEW SUPREME COURT.
Edward W. Whiton, Chief Justice . . . . . 1852. Abram D. Smith, Judge . . . . . . . 1852. Samuel Crawford, 55 . . . . . . . 1852.
FACE OF THE COUNTRY, SoTI, AND GEOLOGICAL FEATURES.—The natural features peculiar to Wisconsin, is the uniformity of its elevation, and shape of its surface, which is neither mountainous, hilly or flat, but gently undulating. The country west of Sugar river and south of the Wisconsin, is somewhat broken, principally by the dividing ridge upon which the road from Madison to Prairie du Chien passes. In this section, known as the Mines, are several peculiar elevations called Mounds. West of the Wisconsin river, are a range of high hills, being the only elevations in the State, either deserving or assuming the dignity of mountains. The southeastern portion of the State is marked by ravines at the streams but little depressed below the surrounding level. Its prominent features are the Prairie, destitute of tree or shrub, covered only by a luxuriant growth of grass, interspersed with flowers of every hue; the Oak Opening; the Lake; the woodland, on the border of streams, and the natural meadow. Proceeding north, to the Fox and Wisconsin rivers, and Green Bay, the timber increases, and the soil gradually changes from the vegetable mould of the prairie to a sandy loam. The surface also becomes somewhat depressed and uneven, diversified with timber, rolling prairie, large marshes and extensive swamps, having an abundant growth of cranberries and wild rice. Still north, and west, the surface becomes more uneven, and the streams rapid, affording an abundance of water power for the manufacture of lumber from the immense forests of evergreen, Scarcely surpassed on the western continent. The soil of the prairie consists of a dark brown vegetable mould, from one to two feet in depth, very mellow, and entirely destitute of stone or gravel, and for fertility and agricultural properties, cannot be surpassed. The sub-soil is a clayish loam, similar to the soil of the timbered lands, and is also suitable for cultivation. The soil of the timbered land is less rich than the prairie, not so deep, and contains less carbonate of lime, which enters into the composition of the latter in the proportion of from 20 to 40 per cent. The mining region, unlike that of any other mineral district, promises a liberal reward, as well to the farmer as to the miner. The soil of the evergreen district is mostly sandy, and not so rich as in other portions of the State. It is nevertheless, well adapted to agriculture and grazing. The prairies of Wisconsin are not so extensive as those of other states, and are so skirted and belted by timber, that they are well adapted to immediate and profitable occupation. The openings, which comprise a large portion of the finest land of the State, owe their present condition to the action of the annual fires which have kept under all other forest growth, except those varieties of oak which can withstand the sweep of that element, This annual burning of an exuberant growth of grasses and of under-brush, has been adding, perhaps for ages, to the productive power of the soil, and preparing it for the plough-share. It is the great fact, nature has thus “cleared up” Wisconsin to the hand of the settler, and enriched it by yearly burnings, and has at the same time left sufficient timber on the ground for fence and firewood, that explains, in a great measure, the capacity it has
exhibited, and is now exhibiting for rapid settlement and early maturity. There is another fact important to be noticed in this connection. The low level prairie, or natural meadow, of moderate extent, is so generally distributed over the face of the country, that the settler on a fine section of arable land, finds on his own farm, or in his immediate neighborhood, abundant pasturage for his stock in summer, on the open range; and hay for the winter, for the cutting—the bounty of Nature supplying his need in this behalf, till the cultivated grasses may be introduced and become sufficient for his use. The limestone, underlying the coal fields of Illinois, forms the immediate basis of the alluvion of Southern Wisconsin. This geological district, in addition to that portion of the State which lies southerly of the valley of the Wisconsin river, comprises the whole of the slope towards Lake Michigan. In many portions of this district, the lime rock disappears, and the out-cropping sand stone furnishes a fine material for building. The lead bearing rock of the mineral region, is a porous lime stone, prevailing throughout Grant, Lafayette and Iowa Counties, comprising four-fifths of the “Lead District” of the upper Mississippi; the remaining one-fifth being in the States of Illinois and Iowa. Deposites of iron ore, water lime stone, and beds of gypsum, together with other varieties of minerals, are found in localities more or less numerous, throughout the lime stone region. All of that section of the State, which lies between Lake Superior on the North, and the falls of St. Anthony on the Mississippi, and the falls of the other rivers flowing southerly, is primitive in its prevailing geological character; and it is within this primitive region, that the copper mines of Lake Superior are found—probably the richest in the world, and apparently inexhaustible. In all that portion of the State, lying between the primitive region just described, and the lime stone formation of the South and East, the transition sand stone prevails; interspersed with lime stone, and more sparsely, with rock of a primitive character. This formation comprises that section of the country drained by the Wisconsin and other rivers tributary to the upper Mississippi, and below the falls of those streams. Within this Geological District, are found quarries of white marble, which promise to be abundant and valuable.
Antiquities—The mounds and antiquities of this State are similar to those in other Western States. I. A. LAPHAM, Esq., who has made this subject his study for several years, in speaking of them in his work on the Geography and Topography of Wisconsin, says:
“Wisconsin does not fall behind the other portions of the western country in the monuments it affords of the existence of an ancient people who once inhabited North America, but of whom nothing is known except what can be gathered from some of the results of their labors. The works at Aztalan, in Jefferson County, are most known and visited, but there are many other localities which are said to equal them in interest and importance. The substance called brick at this place, is evidently burned clay, showing marks of having been mixed with straw, but they were not moulded into regular forms. There is a class of ancient earth-works in Wisconsin, not before found in any other country, being made to represent quadrupeds, birds, reptiles, and even the human form. These representations are rather rude, and it is often difficult to decide for what species of animal they are intended ; but the effects of time may have modified their appearance very much since they were originally formed. Some have a resemblance to the buffalo, the eagle, or crane, or to the turtle or lizard. One representing the human form, near the Blue Mounds, is, according to R. C. TAYLOR, Esq., one hundred and twenty feet in length: it lies in an east and west direction, the head towards the west, with the arms and legs extended. The body or trunk is thirty feet in breadth, the head twenty-five, and its elevation above the general surface of the prairie is about six feet. Its conformation is so distinct that there can be no possibility of mistake in assigning it to the human figure.” A mound at Prairieville, representing a turtle, is about five feet high ; the body is fifty-six feet in length; it represents the animal with its legs extended, and its feet turned backwards. It is to be regretted that this interesting mound is now nearly destroyed. The ancient works are found in all parts of the Territory, but are most abundant at Aztalan, on Rock river, near the Blue Mounds, along the Wisconsin, the Neenah and the Pishtaka rivers, and near Lake Winnebago. “The mounds are generally scattered about without any apparent order or arrangement, but are occasionally arranged in irregular rows, the animals appearing as if drawn up in a line of march. An instance of this kind is seen near the road seven miles east from the Blue Mounds, in Iowa County. At one place near the Four Lakes, it is said that one hundred tumuli, of various shapes and dimensions, may be counted—those representing animals being among others that are round or oblong. “Fragments of ancient pottery of a very rude kind are often found in various localities. They were formed by hand, or moulded, as their appearance shows evidently that these vessels were not turned on a ‘potter's wheel.” Parts of the rim of vessels usually ornamented with small notches or figures, are most abundant. “A mound is said to have been discovered near Cassville, on the Mississippi, which is supposed to represent an animal having a trunk like the elephant, or the now extinct Mastodon. Should this prove true, it will show that the people who made these animal earthworks, were contemporaries with that huge monster whose bones are still occasionally found; or that they had then
* The reader is referred to the “Notice of Indian Mounds, &c., in Wisconsin,” in Silliman's Journal, vol. 34, p. 88, by R. C. Taylor; and to the “Description of Ancient Remains in Wisconsin,” by S. Taylor, vol. 44, p. 21, of the same work, for more detailed descriptions and drawings of these interesting animal mounds.