The trail leaves Lake Nipishish near the head of the large bay, continuing in a direction between north and northwest, through several insignificant lakes, all drained indirectly by the Crooked River, until it reached Otter Lake, which is eight miles long, running nearly north and south, and is five hundred and fifty feet below the summits of the surrounding hills.
From Otter Lake, the course is west through five diminutive lakes, and across a series of sandy ridges to a small shallow lake, which is the source of Babewendigash River. Between this lake and Seal Lake intervene a high range of mountains—the highest seen on the journey to Lake Michikamau—rising fully one thousand feet above the level of Seal Lake. They are visible for miles in any direction, and were seen from Caribou Ridge nearly a month before we reached them.
They are glaciated to their summits, which are entirely destitute of vegetation and in August were still, in places, covered with snow. Babewendigash River winds to and fro between the mountains, its course being determined to a great extent by esker ridges that follow it on either side and which are often more than one hundred feet high. Throughout its length of twenty-five miles there are five rapids and three small lake expansions.
Seal Lake, into which the river flows, is in part an expansion of the Nascaupee River and fills a basin surrounded on every side by mountains, rising several hundred feet above the water. The lake is comparatively shallow, and has a perceptible current. There are several small islands of drift, covered by a scanty growth of spruce and willow. The main lake has direction N. 45 degrees W., and is ten miles long and two and one-half miles wide. The northwestern arm is fifteen miles long, with the same width, and a course N. 80 degrees W.
The steep rocky shores have precluded the formation of terraces. Above Seal Lake the course of the Nascaupee River varies between N. 40 degrees W. and N. 80 degrees W.
Five miles above the lake there is an expansion of the river, called Wuchusk Nipi, or Muskrat Lake, which is eight miles long and a mile and a half wide, with a course N. 40 degrees W. Except for a channel along the western shore, the lake is very shallow, being nearly filled with sand carried down by the river. There is a small stream flowing into this lake expansion near its head, called Wuchusk Nipishish.
For fifty miles above Muskrat Lake, the river flows between sandy banks, marked on either side by two well-defined terraces. The river valley gradually becomes more narrow and the current stronger and with the exception of a few small expansions, progress is only possible by means of tracking. There are, however, in this distance but two rapids necessitating portages.
Opposite the point where the portage leaves the Nascaupee to make a second long detour around rapids, a small river flows in from the southwest, having a sheer fall of almost fifty feet, just above its junction with the main stream.
The trail, after leaving the river, has a course N. 35 degrees W. for two miles; it then turns N. 85 degrees W. six miles, and again N. 55 degrees W. four miles.
In its course are four small lakes, but there is an unbroken portage of eight miles between the last two. Nearly the whole country has been denuded by fire, and the prospect is desolate in the extreme. The end of the portage is on the high rolling plateau of the interior, timbered by a sparse and stunted second growth of spruce, covered everywhere with white reindeer moss, and strewn with lakes innumerable.