War Dance in the interior of a Konza Lodge [go to List of Illustrations]
This ceremony, called the dog dance, was performed by the Konzas for the entertainment of their guests. Mr. Seymour took an opportunity to sketch {128} the attitudes and dresses of the principal figures.[158]
Finding it impracticable to obtain horses by purchase, out of their almost exhausted stock of merchandize, to enable them to prosecute their march to Council Bluff, after due deliberation, they saw no alternative, but to endeavour to hire horses on credit, and to make the best of their way for Cow Island, in hopes of meeting the steamboat there. A Frenchman, Mr. Gunville, resident with this nation, agreed to furnish two pack horses, and a saddle horse for Mr. Say, whose state of health would not admit of his continuing the journey on foot. Thus furnished they prepared to depart, and in the meantime two runners were despatched to inform Major Long of their situation by letter. [pg210]
On the 25th of August, Mr. Say and his party again left the Konza village, accompanied by the French trader, who had furnished them two horses, and by a Missouri Indian; but this last had followed them only a few miles, when he repented of his undertaking and returned.
In pursuing the most direct route from the Konza village to the Missouri, they crossed at the distance of seventeen miles, the Vermilion, a small stream bordered with handsome forests. Nineteen miles beyond this they arrived at the sources of Grasshopper Creek, where they encamped on the evening of the 27th.[159] Here the soil changes somewhat abruptly. The high prairies about the Vermilion and Blue Earth creeks are barren, almost naked, and inhabited by some orbicular lizards. About Grasshopper Creek the soil is fertile, the grass dense and luxuriant.
On the 29th they arrived at Isle au Vache, and were hospitably received by Colonel Morgan and the officers of his command, but had the mortification to learn that Major Long, after waiting a sufficient time to enable the Indian agent to complete his negotiations {129} with the Konzas, had departed with the steam-boat before the arrival of the messengers, that had been sent to notify him of their disaster. These runners had been despatched immediately after their arrival, with instructions to overtake the steam-boat, and to deliver Mr. Say's letter, but[pg211] after some days they returned, without having been able to effect any thing.
It was now determined that Mr. Say and Mr. Jessup, who on account of ill health, were unable to travel farther on foot, should for the present remain at Isle au Vache, while the other gentlemen of the detachment should continue their journey. Mr. Dougherty, from his intimate acquaintance with the country, was of opinion that by crossing in the nearest direction from Isle au Vache to the mouth of Wolf river, they might yet overtake the steam-boat. They accordingly placed themselves under his guidance, and, by great exertion, fortunately arrived at the mouth of Wolf river, on the evening of the 1st of September, as the steam-boat was passing.
The country south-west of the Missouri, between the Konzas and the Platte, is drained principally by Wolf river and the Great Nemahaw. These rivers, like the Nodowa and Nishnebottona, which enter the Missouri nearly opposite them from the north-east, rise in the prairies at an elevation probably of forty or fifty feet above the level of the Missouri. As they descend, their vallies becoming gradually wider, embosom a few trees, and at length, near their entrance into the Missouri valley, are forests of considerable extent. The surface of these prairies presents a constant succession of small rounded hills, becoming larger and more abrupt as you approach the beds of the rivers. The soil is deep, reposing usually on horizontal beds of argillaceous sandstone, and secondary limestone. In all the limestones along the Missouri, we observe a tendency to crystalline structure, and they have often a reddish or yellowish white {130} colour. There is,[pg212] however, always something in the arrangement and in the aspect of the crystals to distinguish these sparry varieties from the primitive granular limestone, to which they have something of general resemblance. The horizontal disposition of the strata of this limestone, the great numbers of organic relics contained in it, and its intimate connexion with coal strata, indicate with sufficient clearness its relation to the secondary rocks. No person who shall examine this stratum with the least attention, either about the Nemahaw and the Konzas, or in the mining district at the sources of the Gasconade, the Merameg, and the St. Francis, will for a moment mistake it for any of those varieties of transition or primitive limestone, which it in some respects so closely resembles. The crystalline varieties, no less than the compact blue limestones, embrace numerous masses of chert or hornstone. This occurs of various colours, and these are arranged in spots or stripes. Some specimens have several distinct colours arranged in zigzag lines, somewhat resembling the fortification agate. The hunters use fragments of this stone for gun-flints; the savages also formerly employed it in the manufacture of arrow points and other implements.[160]
The soil superimposed upon these strata of limestone, is a calcareous loam. Near the rivers it is intermixed with sand; this is also the case with the soil of the high prairies about the Konzas village. In ascending the Konzas river, one hundred, or one hundred and twenty miles from the Missouri, you discover numerous indications, both in the soil, and its animal and vegetable productions, of an approach to the borders of that great Sandy Desert, which stretches eastward from the base of the Rocky Mountains.[pg213] You meet there with the orbicular lizard, or "horned frog," an inhabitant of the arid plains of {131} New Mexico. You distinguish also some cacti, as well as many of those plants allied to chenopodium and salsola, which delight in a thirsty muriatiferous soil. The catalogue of the forest trees belonging to the vallies of this region is not very copious. The cotton-wood and the plane tree, every where form conspicuous features of the forests. With these are intermixed the tall and graceful acacia, the honey locust, and the bonduc, or coffee-tree,[161] and several species of juglans, carya and fraxinus, with pinnated or many-parted leaves. Trees of the family of the coniferæ are not of frequent occurrence on the Missouri. About the summits of rocky cliffs are here and there a few cedars or junipers, the only trees that retain their verdure during the winter.
The prairies, for many miles on each side of the Missouri, produce abundance of good pasturage; but as far as our observation has extended, the best soil is a margin from ten to twelve miles in breadth, along the western bank of the river. In the summer very little water is to be found in the prairies, all the smaller streams failing, even though the season be not unusually dry. On account of the want of wood and of water, the settlements will be for a long time confined to the immediate vallies of the Missouri, the Konzas, and the larger rivers; but it is probable, forests will hereafter be cultivated in those vast woodless regions,[pg214] which now form so great a proportion of the country; and wells may be made to supply the deficiency of running water.