In Norway the rocks often rise almost perpendicularly out of the sea. In the neighbourhood of the coast they reach a considerable height, and then sink gradually towards the east, until they lose themselves in the broad and comparatively low valleys of Sweden. Whole rows of islands lie scattered along the west coast of Norway, round which the sea often whirls in impetuous eddies. On the coast itself, where the land is most exposed to the bleak sea winds, such extensive forests are not to be seen as in the interior of the country; nor do any fertilizing streams wind their way through the short and narrow valleys. It is only here and there that the water from the rocky springs or melted snows, leaps, after a short course, over the edge of the cliff into the open sea, or into the deep fiords with which the coasts are everywhere indented. The greatest rivers in Norway take a more eastern course, and often make their way from the Norwegian highlands through the richly-wooded lowlands of Sweden to the Baltic. In Sweden the coasts are neither so steep nor so indented as in Norway. The waves of the enclosed and comparatively quiet Baltic do not require to be resisted like those of the Atlantic Ocean. Very similar features are found in Scotland. The whole of the northern and western coast lying towards the Atlantic is wild and rocky, with numerous islands, deep firths, and steep shores; behind which, rock towers upon rock, as if to form an impenetrable barrier against the sea. The country is almost without forests, the streams and the valleys are of small extent, and fertility consequently very limited. But by degrees the rocks sink down towards the south-east and east, till they terminate in the broad, well-watered, and fertile coast districts along the North Sea; which, on account of their inconsiderable elevation, are called the Lowlands of Scotland. Thus the Highlands answer very nearly to Norway, and the Lowlands to Sweden. But as the Scandinavian Peninsula is larger than Scotland, so also are its natural features on the whole on a grander scale. The rocks of Norway are mountains of primitive granite, which in some places rise to a height of 8000 feet, and of which large ranges are covered with eternal snow and ice. Scotland, on the contrary, has transition rocks, whose highest peak, Ben Nevis, which is only somewhat more than 4300 feet above the sea, is not even always covered with snow. Nor can the Scottish Lowlands be compared as to extent to the Swedish valleys, with their immense forests and their large rivers and lakes. Nevertheless the natural features of Scotland are in their way no less beautiful than those of the Scandinavian Peninsula. The sea, which indents the coasts on all sides; the well-cultivated, and partly also well-wooded plains, which, particularly towards the mountain districts, undulate in hill and dale; and lastly the Highland itself, with its many streams, waterfalls, firths, and lakes, afford the richest and most