miles too far west. At the mouth of the river the water was found to be shallow—in some places not more than three or four feet in depth—and for some distance out into the lake shoals were observed. Small sailing vessels or York boats would, however, have no difficulty in getting in, but it would be difficult to take the former any great distance up the river on account of the rapids. Large properly constructed river boats might be taken up stream without difficulty for a distance of 150 miles to the confluence of the west branch, and how far they might be able to ascend that large stream it is impossible for me to say. With the exception of perhaps one spot—the canyon rapid north of Tobaunt Lake—I believe the whole river from the Height of Land to Baker Lake might be navigated by river or York boats with comparative ease. At the rapid a portage could be made or possibly a navigable channel might be discovered.
I think it important to mention the above possibilities of access to this country, on account of the fact that from Tobaunt Lake to Baker Lake there stretches an extended area of promising mineral-bearing Huronian schists and trappean rocks, a series precisely similar to the silver, copper and gold bearing rocks of the north shore of Lake Superior and Lake of the Woods districts. The time must come—it may not be far distant—when the prospector and the miner will occupy all this vast field of mineral wealth.[1]
From the head of Baker Lake we were now to com-*
- ↑ For full geological and mineralogical details regarding this district, see J. B. Tyrrell's report for 1893, published by the Geological Survey Department of Canada.
