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. The Goetha Canal, as before intimated, utilizes and connects several of the great lakes of southern Sweden, the principal ones in Scandinavia being located in this region. Lake Wener, which receives the waters of eighty rivers large and small, has an area of twenty-four hundred square miles, being nearly ten times as large as the famous Lake of Geneva. Lakes Wetter and Maelaren are the next in importance, either of which is fully twice the size of the Swiss lake just named. The canal proper--that is, the portion which has been artificially constructed--is ten feet deep, fifty wide at the bottom, and ninety at the surface. Two hundred and seventy miles of the route traversed by the vessels navigating the canal between Gottenburg and Stockholm are through lakes and rivers, all of which are remarkable for their clear spring-like character and the picturesqueness of their surroundings. Stockholm is situated on the Maelaren lake, where it finds an outlet into the Baltic. This large body of water is studded all over with islands of every form and size, on some of which are quaint old castles, mysterious ruins, and thick woods, haunted only by those rovers of the sky, the eagle and the hawk. Others are ornamented by charming villas, surrounded by fine landscape gardening, with graceful groves of drooping willows and birch-trees. Some contain only fishermen's huts, while here and there clusters of their small cottages form an humble village. The marine shells which are found in the bottom of some of the inland lakes of both Norway and Sweden show that the land which forms their bed was once covered by the sea. This is clearly apparent in Lake Wener and Lake Wetter, which are situated nearly three hundred feet above the present ocean level. The first-named body of water is some eighty miles long by a width of thirty. The latter is as long, but averages only ten miles in width. Complete skeletons of whales have been found far inland, at considerable elevations, during the present century. The oldest shell-banks discovered by scientists in Scandinavia are situated five hundred feet above the present level of the ocean. How significant are these deposits of a prehistoric period! Sweden has comparatively few mountains, but many ranges of hills. Norway monopolizes almost entirely the mountain system of the great northern peninsula; but the valuable large forests of pine, fir, and birch which cover so much of the country are com
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