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
On May 8 the party discovered the largest and most important of the
northern tributaries of the Upper Missouri. The journal thus describes
the stream:--
“Its width at the entrance is one hundred and fifty yards; on going
three miles up, Captain Lewis found it to be of the same breadth and
sometimes more; it is deep, gentle, and has a large quantity of water;
its bed is principally of mud; the banks are abrupt, about twelve
feet in height, and formed of a dark, rich loam and blue clay; the
low grounds near it are wide and fertile, and possess a considerable
proportion of cottonwood and willow. It seems to be navigable for boats
and canoes; by this circumstance, joined to its course and quantity of
water, which indicates that it passes through a large extent of
country, we are led to presume that it may approach the Saskaskawan
(Saskatchewan) and afford a communication with that river. The water has
a peculiar whiteness, such as might be produced by a tablespoonful of
milk in a dish of tea, and this circumstance induced us to call it Milk
River.”
Modern geography shows that the surmise of Captain Lewis was correct.
Some of the tributaries of Milk River (the Indian name of which
signifies “The River that Scolds at all Others”) have their rise near
St. Mary’s River, which is one of the tributaries of the Saskatchewan,
in British America.
The explorers were surprised to find the bed of a dry river, as deep and
as wide as the Missouri itself, about fifteen miles above Milk River.
Although it had every appearance of a water-course, it did not discharge
a drop of water. Their journal says:--
“It passes through a wide valley without timber; the surrounding country
consists of waving low hills, interspersed with some handsome level
plains; the banks are abrupt, and consist of a black or yellow clay,
or of a rich sandy loam; though they do not rise more than six or eight
feet above the bed, they exhibit no appearance of being overflowed; the
bed is entirely composed of a light brown sand, the particles of which,
like those of the Missouri, are extremely fine. Like the dry rivers we
passed before, this seemed to have discharged its waters recently, but
the watermark indicated that its greatest depth had not been more than
two feet. This stream, if it deserve the name, we called Bigdry (Big
Dry) River.”
And Big Dry it remains on the maps unto this day. In this region the
party recorded this observation:--
“The game is now in great quantities, particularly the elk and buffalo,
which last is so gentle that the men are obliged to drive them out
of the way with sticks and stones. The ravages of the beaver are very
apparent; in one place the timber was entirely prostrated for a space of
three acres in front on the river and one in depth, and great part of it
removed, though the trees were in large quantities, and some of them as
thick as the body of a man.”
Public-domain text, read in full here on John Shaqi.
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