Preliminary Report on Gowganda Mining Division District of Nipissing OntarioCollins, W. H. (William Henry)
Science
Preliminary Report on Gowganda Mining Division District of Nipissing Ontario
Collins, W. H. (William Henry)
Geology -- Ontario; Mines and mineral resources -- Ontario
SIR,—I beg to submit the following preliminary report upon work done in
the Gowganda Mining Division during the field season of 1908.
I have the honour to be, sir,
Your obedient servant,
W. H. COLLINS.
CHICAGO, March 8, 1909.
[Illustration: Fig. 1. View at foot of Duncan Lake.]
PRELIMINARY REPORT
ON
GOWGANDA MINING DIVISION
DISTRICT OF NIPISSING, ONTARIO
BY
W. H. COLLINS.
--------------
INTRODUCTION.
LOCATION AND AREA.
The portion of the Montreal River region with which the present report
deals lies in the extreme western part of the District of Nipissing, in
the neighbourhood of N. Lat. 47·45, and about 85 miles north of the town
of Sudbury. It includes an area of 350 square miles, most of which lies
between the two large branches of the Montreal river, which empties into
Lake Timiskaming on the west side.
STATEMENT OF WORK.
The Algoma-Nipissing boundary line was run in 1897 by Alexander Niven,
O.L.S. These surveys, with representations of some of the larger lakes,
had been compiled by the Geological Survey of Canada on a scale of 16
miles to one inch;[1] and on a scale of eight miles by the Crown Lands
Department of Ontario. With these as a guide and summary of the existing
geographical knowledge it was decided to make a micrometer and prismatic
compass survey of both branches.
During the past season a prismatic compass and micrometer survey was
made of both branches of the Montreal river and all navigable waters
adjoining them. This work was done by Messrs. T. Firth, J. R. Marshall
and A. B. Moffatt. Most of the small ponds lying some distance from a
canoe route were located by rapid chain and compass methods, and in a
few instances west of Duncan lake by a compass triangulation from
hilltops; the larger ones have been measured by pacing or chaining, the
smaller ones sketched. Some of the more prominent hills were located by
triangulation, and their heights ascertained by aneroid determinations.
The water levels were obtained in the same way, but cannot as yet be
referred to sea-level.
The geological work was performed by the writer, assisted by Mr. Firth.
Besides a thorough examination of all the surveyed routes, a systematic
examination of the intervening country was carried out as closely as the
time and varied requirements of the area would permit. As this was the
first season spent in the district and a continuation of the work is
anticipated, the present results are offered as incomplete and subject
to revision.
HISTORY OF DEVELOPMENT.
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