A Historical Geography of the British Colonies, Vol. V: Canada—Part I, HistoricalLucas, Charles Prestwood, Sir
History
A Historical Geography of the British Colonies, Vol. V: Canada—Part I, Historical
Lucas, Charles Prestwood, Sir
Canada -- History -- To 1763 (New France)
The Hudson river rises in the Adirondack mountains, to {242} the west
of Lake George, and flows in a south-easterly direction, until it
reaches a point south-west by south of the southern end of the lake.
Here for some miles it takes a due easterly course, at right angles
to the line of the lake, until, at Sandy Hill, near where Fort Edward
was founded, it turns due south, and flows due south into the
Atlantic. It appears to prolong to southward the line of Lake George
and Lake Champlain; but the watersheds are distinct, the two lakes in
question drain to the north, and eventually discharge through the
Richelieu river into the St. Lawrence.
[Sidenote: _Lakes George and Champlain._]
They form a long narrow basin running north and south between the
Adirondacks on the west and the Green mountains of Vermont on the
east. No stream of any size feeds Lake George; it stretches for
between thirty and forty miles from south-west to north-east,
overshadowed by the Adirondacks; and, narrowing at the northern end,
finds an outlet into Lake Champlain by a semicircular channel, which
enters the larger lake from west to east. This channel is broken by
rapids, and in the angle which it forms with Lake Champlain stands
Ticonderoga.
Lake Champlain is here a broad river rather than a lake, having
narrowed into the similitude of a river from where, fifteen miles
further north, the isthmus of Crown Point juts out on the western
side of the lake. But it does not end at Ticonderoga, where it meets
the waters of Lake George. It continues southwards in a direct line,
very roughly parallel to Lake George, still narrowing in its upward
course, through the marshes known as the Drowned Lands, past a little
subsidiary lake on the western side known as South Bay, over against
which now stands the small town of Whitehall, and ending in a stream
known as Wood Creek. The sources of Wood Creek are but a few miles
distant from the point, already noted, where the Hudson turns south
to form the central valley of New York State, and where Johnson, in
the summer of 1755, was busy constructing Fort Lyman.
{243} [Sidenote: _Johnson encamps at the end of Lake George._]
Johnson's objective was Crown Point; and to reach it he had a choice
of two parallel routes, either of which involved a portage from the
Hudson watershed to that of Lake Champlain. He could take either the
western line by Lake George, or the eastern line by Wood Creek. He
chose the former, and making a road for fourteen miles from Fort
Lyman to the head--the southern end--of Lake George, encamped there
at the end of August with over 2,000 men, leaving 500 men behind to
garrison Fort Lyman.
[Sidenote: _Dieskau at Crown Point._]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account