verse facts, which are now known to
be undeniable. It may therefore be considered fortunate for the claim of
the United States that the survey was afterwards intrusted to a surveyor
who, in pursuit of the double object of encroachment on the United
States and the enlargement of his native Province at the expense of
Canada, signally failed in the proof of either of his positions.
The knowledge now acquired shows that the idea of Colonel Bouchette is
unsupported by the facts of the case, for the highlands which rise from
the north shore of the Bay of Chaleurs do not meet those in which the
most southerly branch of the Restigouche takes its rise.
The British commissioners, although they give a profile of this ridge,
do not pretend to have examined it except at Mars Hill, near the
Aroostook, and at the Grand Falls of the St. John. It must be remarked
that these profiles (the original one of Colonel Bouchette and that
exhibited by themselves) are contrasted--one British authority with
another--for the purpose of invalidating the ground on which the
American claim is founded.
It is not our business to reconcile these conflicting authorities, but
it is our duty to recall the recollections of the fact that no part
of the American argument laid before the King of the Netherlands was
founded on this or any other estimate of heights. Many elevations,
indeed, were measured with great pains on the part of the Americans
as well as of Great Britain.
On behalf of the United States Captain Partridge made many barometric
observations, while Mr. Johnson took an extensive series of vertical
and horizontal angles. His operations were performed in the presence of
Mr. Odell, the surveyor on behalf of Great Britain, who doubtless made
similar ones, as he visited the same stations with a better instrument
and for the same avowed purpose. Mr. Odell's observations were not
presented by the British agent, and those of Mr. Johnson were objected
to. If received, they would have set aside the pretensions that a
continuous ridge of mountains existed between the Metjarmette portage
and Mars Hill. They are, however, superseded by the operations of the
undersigned, which have yielded satisfactory evidence that no chain of
highlands in the sense of the British commissioners, or even an "axis of
maximum elevation," exists where it is laid down on their map. Nor can
it be doubted that the operations of Mr. Johnson had a decided advantage
in point of
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