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Klondyke Nuggets - A Brief Description of the Great Gold Regions in the Northwest by Joseph Ladue
page 49 of 97 (50%)
the numerous glaciers on the head of the tributaries of Lake Lindeman.

[Footnote 3: A small saw-mill has been erected at the head of Lake
Bennet; lumber for boat building sells at $100 per M. Boats 25 feet long
and 5 feet beam are $60 each. Last year the ice broke up in the lake on
the 12th June, but this season is earlier and the boats are expected to
go down the lake about the 1st of June.]

"A stream which flows into Lake Bennet at the south-west corner is also
very dirty, and has shoaled quite a large portion of the lake at its
mouth. The beach at the lower end of this lake is comparatively flat and
the water shoal. A deep, wide valley extends northwards from the north
end of the lake, apparently reaching to the caƱon, or a short distance
above it. This may have been originally a course for the waters of the
river. The bottom of the valley is wide and sandy, and covered with
scrubby timber, principally poplar and pitch-pine. The waters of the
lake empty at the extreme north-east angle through a channel not more
than one hundred yards wide, which soon expands into what Schwatka
called Lake Nares.[4] Through this narrow channel there is quite a
current, and more than 7 feet of water, as a 6 foot paddle and a foot of
arm added to its length did not reach the bottom.

[Footnote 4: The connecting waters between Lake Bennet and Tagish Lake
constitute what is now called Caribou Crossing.]

"The hills at the upper end of Lake Lindeman rise abruptly from the
water's edge. At the lower end they are neither so steep nor so high.

"Lake Nares is only two and a half miles long, and its greatest width is
about a mile; it is not deep, but is navigable for boats drawing 5 or 6
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