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ut you can well understand that such an extensive country, even though it is thinly peopled, especially in its cold, northern parts, must yield much that is valuable to its owners." "Yes, certainly; so it is in Siberia, where the population is also scanty." "Just so. In Canada fields, mountains, forests, and water yield an immense revenue. Think only of all the agricultural produce which is shipped from here, not to speak of gold, fish, and furs. The wheat produced in Canada is alone worth over 22 million pounds sterling a year. There are also huge areas which are worthless. We get little advantage from the northern coasts, where the Eskimos live." "You are quite at home on these lakes?" "Oh yes. When a man has sailed to and fro over them for ten years, he knows all about the roadsteads and channels, and about when the ice forms and breaks up, and when there is a prospect of a storm." "But the storms cannot be very dangerous?" "Ah, you do not believe in them. All the same they may be just as dangerous as in the Atlantic, and when a real hurricane comes, the skipper will do well to seek shelter, or at the best he will lose his cargo. You will soon have opportunities of seeing, hearing, and feeling how the surge beats just as on the coast of the ocean. But then, all these lakes have an aggregate area more than half as large as the Baltic, and if we take the depth into account we shall find that the volume of water is the same as in the Baltic. Lake Superior is the largest lake in the world. Beyond the point yonder lies Lake Huron. You must acknowledge that this scenery is beautiful. Have you ever seen anything to equal this sheet of dark-blue water, the dark-green woods, and the grand peaceful shores? It is a pity that we do not go to Lake Erie, for at its eastern extremity is one of the wonders of the world and the most famous spectacle in North America." [Illustration: PLATE XXXIII. NIAGARA FALLS.] "You mean the Falls of Niagara, which I have heard described so many times?" "Yes. Think of a steamboat on Lake Erie sucked along by the stream that flows to Ontario. This lake lies 300 feet lower than Erie, and about half-way between the two lakes the water passes over a sharp bar and plunges with a thundering roar into the depth below (Plate XXXIII.). The barrier itself, which is a thousand yards broad, is formed of a huge stratum of sandstone, and the rocks under it are loose slates. Erosion proceeds m
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