Ontario Sessional Papers, 1901, . [63]. Approaching rapids, north of Kenogami Lake. Party No. 7. [64 J 1900 ] EXPLORATION SURVEY PARTY Xo. 10. 253 northerly part of Wabigoon River is distinguished physically from the first division justdescribed by its comparatively flit and low-lying surface whb. its extensive areas ofclay soil and conseqaenty heavy growth of large timber, this feature being apparentlydue to the more eflFective glaciation of the rocks, by which they were planed down, andleft with a comparatively even surface The Keewatin shore aiso, from the mouth of theWabifeoon Riv
Ontario Sessional Papers, 1901, . [63]. Approaching rapids, north of Kenogami Lake. Party No. 7. [64 J 1900 ] EXPLORATION SURVEY PARTY Xo. 10. 253 northerly part of Wabigoon River is distinguished physically from the first division justdescribed by its comparatively flit and low-lying surface whb. its extensive areas ofclay soil and conseqaenty heavy growth of large timber, this feature being apparentlydue to the more eflFective glaciation of the rocks, by which they were planed down, andleft with a comparatively even surface The Keewatin shore aiso, from the mouth of theWabifeoon River, north-easterly, is of the same flit character, and is also, I may add,densely timbered with poplar, spruce, etc., a circumstance, by the way, which adds tothe value of the Ontario forest, because it will permit lumbering operations to be carriedon in a larger way, and, therefore, at less cost per unit of output. As we go down theWabigoon River this level tract, being our second division, is met with on the east shoreof Clay Lake, an expansi
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