Preliminary Report on Gowganda Mining Division District of Nipissing Ontario — Edition Insights

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Collins, W. H. (William Henry), 1878-1937 Project Gutenberg 2021 Not confirmed
Geology -- Ontario; Mines and mineral resources -- Ontario Readers of public-domain and historical texts
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Edition facts

Words 21,451
Reading time 94 min
Text sections 7

Before opening Preliminary Report on Gowganda Mining Division District of Nipissing Ontario — Edition Insights, the edition data offers a quick orientation: 21,451 words, 1 hr 34 min estimated reading time, and 7 detected text sections.

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Project Gutenberg metadata also associates the work with “Geology -- Ontario,” connecting these edition facts with the source record’s subject description.

A 1909 geological survey report on Ontario's Gowganda Mining Division, detailing rock formations, mineral deposits, and field observations. The text combines technical descriptions of diabase and aplite with practical assessments of silver, copper, and iron prospects, offering a window into early 20th-century Canadian economic geology.
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Editorial Edition Score 4.7/5

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Edition quality

Read the Text

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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