as to have suffered Mr. Fidler to come as low as 45
degrees along the eastern borders without touching
that river: yet the general course of Maria’s
river from this place for fifty-nine miles, as far
as captain Lewis ascended, was north 69 degrees west,
and the south branch, or what we consider the Missouri,
which captain Clarke had examined as far as forty-five
miles in a straight line, ran in a course south 29
degrees west, and as far as it could be seen went
considerably west of south, whence we conclude that
the Missouri itself enters the Rocky mountains to
the north of 45 degrees. In writing to the president
from our winter quarters, we had already taken the
liberty of advancing the southern extremity of Mr.
Fidler’s discoveries about a degree to the northward,
and this from Indian information as to the bearing
of the point at which the Missouri enters the mountain;
but we think actual observation will place it one
degree still further to the northward. This information
of Mr. Fidler however, incorrect as it is, affords
an additional reason for not pursuing Maria’s
river; for if he came as low even as 47 degrees and
saw only small streams coming down from the mountains,
it is to be presumed that these rivulets do not penetrate
the Rocky mountains so far as to approach any navigable
branch of the Columbia, and they are most probably
the remote waters of some northern branch of the Missouri.
In short, being already in latitude 47 degrees 24’
we cannot reasonably hope by going farther to the
northward to find between this place and the Saskashawan
any stream which can, as the Indians assure us the
Missouri does, possess a navigable current for some
distance in the Rocky mountains: the Indians
had assured us also that the water of the Missouri
was nearly transparent at the falls; this is the case
with the southern branch; that the falls lay a little
to the south of sunset from them; this too is in favour
of the southern fork, for it bears considerably south
of this place which is only a few minutes to the northward
of fort Mandan; that the falls are below the Rocky
mountains and near the northern termination of one
range of those mountains: now there is a ridge
of mountains which appear behind the South mountains
and terminates to the southwest of us, at a sufficient
distance from the unbroken chain of the Rocky mountains
to allow space for several falls, indeed we fear for
too many of them. If too the Indians had ever
passed any stream as large as this southern fork on
their way up the Missouri, they would have mentioned
it; so that their silence seems to prove that this
branch must be the Missouri. The body of water
also which it discharges must have been acquired from
a considerable distance in the mountains, for it could
not have been collected in the parched plains between
the Yellowstone and the Rocky mountains, since that
country could not supply nourishment for the dry channels
which we passed on the south, and the travels of Mr.
Fidler forbid us to believe that it could have been
obtained from the mountains towards the northwest.