Preliminary Report on Gowganda Mining Division District of Nipissing Ontario — Edition Insights
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When italics were used in the original book, the corresponding text has been surrounded by _underscores_.
Some corrections have been made to the printed text. These are listed in a second transcriber’s note at the end of the text.
GEOLOGICAL SURVEY BRANCH
HON. W. TEMPLEMAN, MINISTER; A. P. LOW, LL.D., DEPUTY MINISTER; R. W. BROCK, DIRECTOR.
GOWGANDA MINING DIVISION
DISTRICT OF NIPISSING
PRINTED BY C. H. PARMELEE, PRINTER TO THE KING’S MOST EXCELLENT MAJESTY
1. Location and area 5
2. Statement of work 5
3. History of development 6
II. Summary and Conclusions 8
III. General Character of District 10
1. Means of access 10
4. Flora and fauna 15
IV. General Geology 16
1. Outline of Geological history 16
2. Table of formations 18
Relations to other formations 24
Basal conglomerate 26
Greywacke slate and quartzite 27
Upper conglomerate 27
Structural features and disturbances 28
Relations to other formations 29
Origin and correlation 31
6. Post-Huronian eruptives 32
Character of intrusion and distribution relative to older systems 32
Macroscopic character 33
Microscopic character 34
V. Economic Geology 40
Surface indications 40
Structure of veins 41
Composition of veins 41
Future possibilities 44
1. Frontispiece—View at Foot of Duncan Lake 5
2. Diagram illustrating the structure of large hills 12
3. Diagram illustrating geological relationships 16
4. View looking north from middle of Duncan Lake, 550 ft. hill in distance 20
5. West Branch Montreal River, near Mosher Lake 22
6. Fifth portage on West Branch of Montreal River, showing Huronian slate 30
7. Inclined Huronian Beds, Duncan Lake 32
Director Geological Survey Branch, Department of Mines.
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,
CHICAGO, March 8, 1909.
GOWGANDA MINING DIVISION
DISTRICT OF NIPISSING, ONTARIO
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.
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.
W. H. Collins's 1909 report, submitted to the Director of the Geological Survey Branch, opens with a precise location and area statement for the Gowganda Mining Division in the District of Nipissing, Ontario. The document is structured as a formal government publication, with numbered sections covering introduction, summary, general character of the district, general geology, and economic geology. The excerpts reveal a methodical approach: Collins describes rock types, their macroscopic and microscopic characters, and their economic potential, often noting limitations such as decomposed samples that prevented complete analysis.
Field Observations and Petrological Detail
The report's strength lies in its detailed petrological descriptions, grounded in field observations. Collins notes that diabase bodies present a surprising variety of types, with end members very unlike each other. He describes how magmatic differentiation produced a range from dark green diabase to fine-grained pink aplite, observable within small areas. At the Lett properties on Wapus creek, extensive stripping and trenching allowed him to trace an unbroken gradation from gabbro to aplite. He also remarks on the practical difficulty of distinguishing diabase from gabbro in hand specimens, as ophitic structure is not visible without a microscope. Such candid assessments of field limitations are a recurring feature.
Economic Geology: Silver, Copper, and Iron
Collins devotes a section to economic geology, covering silver, copper, iron ores, and asbestos. For silver, he discusses distribution, surface indications, vein structure, and composition, but the excerpts provide only a brief local description and future possibilities. Copper and iron ores are treated more succinctly: hematite and magnetite are mentioned, but no detailed assays or production figures appear in the excerpts. The asbestos section notes distribution and origin. The report's tone is cautious—Collins often states that a knowledge of all veins could not be obtained, and he recommends further study. This restraint aligns with the report's preliminary nature.
Structure and Illustrations: A Visual Guide
The report includes several illustrations: a frontispiece view at Duncan Lake, diagrams of hill structure and geological relationships, and photographs of the Montreal River and Huronian slate. These visuals complement the text, which frequently references specific locations like Duncan Lake, Mosher Lake, and Wapus creek. Collins uses diagrams to clarify structural features, such as the inclination of Huronian beds. The combination of written description and visual aids reflects the report's dual purpose: to document geological findings and to guide future prospectors and geologists in the field.
Readers approaching this report should note its preliminary status: Collins explicitly states that some analyses are incomplete due to decomposed samples, and he does not claim to have examined all mineral occurrences. The text is best read as a snapshot of early 20th-century geological practice in Canada, with an emphasis on systematic observation and cautious inference. Those interested in the history of mining in Ontario will find value in the detailed descriptions of rock types and the candid assessment of economic potential.
That old survey report left me thinking about how people once saw promise in bare rock. It felt like reading someone’s patient, hopeful notes. Something similar lingers in Makers of Many Things — A Reader’s Guide, where everyday objects become quiet stories of craft and care. Both feel like gentle reminders that attention itself is a kind of treasure, unnoticed but enduring.
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