First Across the Continent: The Story of the Exploring Expedition of Lewis and Clark in 1804-5-6Brooks, Noah
History
First Across the Continent: The Story of the Exploring Expedition of Lewis and Clark in 1804-5-6
Brooks, Noah
Lewis and Clark Expedition (1804-1806); United States -- Discovery and exploration; West (U.S.) -- Description and travel
“The game is in great quantities, but the buffalo are not so numerous as
they were some days ago; two rattlesnakes were seen to-day, and one of
them was killed. It resembles those of the Middle Atlantic States, being
about thirty inches long, of a yellowish brown on the back and sides,
variegated with a row of oval dark brown spots lying transversely on the
back from the neck to the tail, and two other rows of circular spots of
the same color on the sides along the edge of the scuta; there are one
hundred and seventy-six scuta on the belly, and seventeen on the tail.”
Two days later, the journal records that one of the party killed a
grizzly bear, “which, though shot through the heart, ran at his usual
pace nearly a quarter of a mile before he fell.”
The mouth of the Musselshell River, which was one of the notable points
that marked another stage in the journey, was reached on the twentieth
of May. This stream empties into the Missouri two thousand two hundred
and seventy miles above its mouth, and is still known by the name given
it by its discoverers. The journal says:
“It is one hundred and ten yards wide, and contains more water than
streams of that size usually do in this country; its current is by no
means rapid, and there is every appearance of its being susceptible of
navigation by canoes for a considerable distance. Its bed is chiefly
formed of coarse sand and gravel, with an occasional mixture of black
mud; the banks are abrupt and nearly twelve feet high, so that they are
secure from being overflowed; the water is of a greenish-yellow cast,
and much more transparent than that of the Missouri, which itself,
though clearer than below, still retains its whitish hue and a portion
of its sediment. Opposite the point of junction the current of the
Missouri is gentle, and two hundred and twenty-two yards in width;
the bed is principally of mud, the little sand remaining being wholly
confined to the points, and the water is still too deep to use the
setting-pole.
Public-domain text, read in full here on John Shaqi.
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