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The morning being fair and pleasant and wind favourable we set sale at an early hour, and proceeded on very well the greater part of the day; the country still continues level fertile and beautifull, the bottoms wide and well timbered comparitively speaking with other parts of the river; no appearance of birnt hills pumice stone or coal, the salts of tartar or vegitable salts continues to appear on the river banks, sand bars and in many parts of the plains most generally in the little revines at the base of the low hills. passed three streames today which discharged themselves on the Lard. side; the first of these we call little dry creek it contained some water in standing pools but discharged none, the 2ed 50 yards wide no Water, we called it Big dry Creek, the 3rd is bed of a conspicuous river 200 yards wide which we called little dry river; the banks of these streams are low and bottoms wide with but little timber, their beds are almost entirely formed of a fine brown sand intermixed with a small proportion of little pebbles, which were either transparent, white, green, red, yellow or brown. these streams appeared to continue their width without diminution as far as we could perceive them, which with rispect to the river was many miles, they had recenly discharged their waters. from the appearance of these streams, and the country through which they passed, we concluded that they had their souces in level low dry plains, which probably is the character of the country for a great distance west of this, or to the vicinity of the black hills, that the country being low on the same level nearly and in the same parallel of latitude, that the rains in the spring of the year suddonly melts the snow at the same time and causes for a few days a vast quantity of water which finds it's way to the Missouri through those channels; by reference to the diary of the weather &c it will be percieved that there is scarcely any rain during the summer Autumn and winter in this open country distant from the mountains.
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