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C. and myself to kill as much meat as the party can consum; I hope it may continue thus through our whole rout, but this I do not much expect. two beaver were taken in traps this morning and one since shot by one of the party. saw numbers of these anamals peeping at us as we passed out of their wholes which they form of a cilindric shape, by burrowing in the face of the abbrupt banks of the river.

The Muscle Shell river falls into the Missouri 2270 miles above it's mouth, and is 110 yards in width, it affords much more water than streams of it's width generally do below, it's courant is by no means rappid, and from appearances it might be navigated with canoes a considerable distance; it's bed is coarse sand and gravel principally with an occasion mixture of black mud; it's banks abbrupt and about 12 feet high yet never appear to overflow; the waters of this river is of a greenish yellow cast, much more transparent than the Missouri, which last is also much more transparent than below but still retains it's whiteish hue and a proportion of it's sedement. the Missouri opposite to this point is deep, gentle in it's courant, and 222 yards in width.

I walked up this river about three miles and ascended an eminence from which I could perceive it many miles; it's course about South for 10 or 12 miles, when it viered around to the E of S. E. as far as I could see. the valley of this river is wide and possesses but a scanty proportion of timber; the hills which border it are not very high nor is the country very broken; it is what may properly be designated a wavy or roling country intersperced with some handsom level plains. the bank are low and abbrupt, seldom more than 6 or eight feet above the level of the bed, yet show but little appearance of being overflown; they are of black or yellow clay or a rich sandy loam. the bed is entirely composed of a light brown sand the particles of which as well as that of the Missoury are remarkably fine. this river I presume must extend back as far as the black hills and probably is the channel through which a great extent of plain country discharge their superfluous waters in the spring season. it had the appearance of having recently discharged it's waters; and from the watermark, it did not appear that it had been more than 2 feet deep at it's greatest hight.

Set out at an early hour under a gentle brieze from the East. a black cloud which suddonly sprung up at S. E. soon over shaddowed the horizon; at 8 A.M. it gave us a slight sprinke of rain, the wind became much stronger but not so much so as to detain us. we nooned it just above the entrance of a large river which disimbogues on the Lard. side; I took the advantage of this leasure moment and examined the river about 3 miles; I found it generally 150 yards wide, and in some places 200. it is deep, gentle in it's courant and affords a large boddy of water; it's banks which are formed of a dark rich loam and blue clay are abbrupt and about 12 feet high. it's bed is principally mud.