Mr. Wm. McInnes describes the country about Winisk and Attawapiskat rivers, explored by him in 1903, 1904 and 1905, as consisting of three areas, the first a limestone area, along the bay shore, the second a boulder clay area, behind it, and the third in rear of it again, a high interior plateau. As to the latter area, he says:—“Although, considered as a whole, the central, elevated region cannot be spoken of as generally adapted for agriculture, there occur basins covered by heavy deposits of stratified sand and clay that seem to have been laid down in lakes held in between barriers formed by the walls of the retreating glacier and ridges of drift. An examination of some of these clays by Doctor Hoffman shows them to be highly calcareous and somewhat siliceous, a composition that with the admixture of the surface vegetable mould should produce an EXCELLENT SOIL FOR GENERAL AGRICULTURE. The question of climate, which is, of course, of the utmost importance when considering the agricultural possibilities of a district, will be referred to more particularly in another place. It may be said here, however, that the climatic conditions are, if somewhat adverse, not by any means prohibitory to the general cultivation of suitably situated tracts. “Muskeg, alternating with low ridges of gravel and boulders, covers wide tracts. It was noticed that the surface drainage became more perfect in that part of the region extending westerly towards Trout lake. . . . . . . . . . “The tract referred to as the boulder clay area consists of a broad belt of country, about one hundred and fifty-nine miles in width, lying between the Archaean highlands and the edge of the limestones of the basin of Hudson bay, overlapping the latter, however, so that the surface features of the two are generally quite similar. Gently undulating, and with a slight slope northerly and easterly, its general surface aspect is that of a great swamp, sparsely covered with stunted and deformed trees, that reach a growth approaching their normal only along the immediate banks of the rivers where drainage is afforded by frequent short gullies into the trenches that constitute the river valleys. The interior, to within a chain or two of the river-banks, owing to the impervious character of the till, IS QUITE UNDRAINED,