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Updated: May 3, 2025
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.
The quartz grains show secondary growth. 13 Altered Gabbro Thirty-two Miles Above Wuchusk Nipi on Nascaupee River. A coarse dark green rock whose principal constituents are pyroxene plagioclase and magnetite. There is a slightly developed diabasic structure and the rock is much altered by weathering; the resultant product being chlorite. 14 Quartizite Bibiquagin Lake.
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.
First portage opposite Red River S. 45 degrees E. On Caribou Ridge E. At Washkagama Lake S. 70 degrees E. Near Seal Lake N. 85 degrees E. At Wuchusk Nipi S. 75 degrees E. Thirty-two miles above Wuchusk Nipi S. 70 degrees E. By G. M. Richards, Columbia University 1 Pegmatite-Grand Lake. The specimen was taken from a pegmatite dike at its contact with an amphibolite.
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