Such a panorama justifies Ruskin's bold assertion: "Mountains are the beginning and end of all natural scenery." Without its mountains, the view from Council Crest would be as uninteresting as that from any tower in any prairie city. But all mountains are not alike. In beginning our journey to the three great snow-peaks which we have viewed from Portland heights, it is well to define, if we may, the special character of our Northwestern scene. We sometimes hear the Cascade district praised as "the American Switzerland." Such a comparison does injustice alike to our mountains and to the Alps. As a wild, magnificent sea of ice-covered mountain tops, the Alps have no parallel in America. As a far-reaching system of splendid lofty ranges clothed in the green of dense forests and surmounted by towering, isolated summits of snowy volcanoes, the Cascades are wholly without their equal in Europe. This is the testimony of famous travelers and alpinists, among them Ambassador Bryce, who has written of our Northwestern mountain scenery:
We have nothing more beautiful in Switzerland or Tyrol, in Norway or in the Pyrenees. The combination of ice scenery with woodland scenery of the grandest type is to be found nowhere in the Old World, unless it be in the Himalayas, and, so far as we know, nowhere else on the American continent.
Cone of Mount Hood, seen from Cooper Spur on northwest side. A popular route to the summit leads along this ridge of volcanic scoriæ and up the steep snow slope above.
Cloud Cap Inn, north side of Mount Hood. Elevation 5,900 feet.
In his celebrated chapter of the "Modern Painters" which describes the sculpture of the mountains, Ruskin draws a picture of the Alps that at once sets them apart from the Cascades:
The longer I stayed among the Alps, the more I was struck by their being a vast plateau, upon which nearly all the highest peaks stood like children set upon a table, removed far back from the edge, as if for fear of their falling. The most majestic scenes are produced by one of the great peaks having apparently walked to the edge of the table to look over, and thus showing itself suddenly above the valley in its full height. But the raised table is always intelligibly in existence, even in these exceptional cases; and for the most part, the great peaks are not allowed to come to the edge of it, but remain far withdrawn, surrounded by comparatively level fields of mountain, over which the lapping sheets of glacier writhe and flow. The result is the division of Switzerland into an upper and lower mountain world; the lower world consisting of rich valleys, the upper world, reached after the first steep banks of 3,000 to 4,000 feet have been surmounted, consisting of comparatively level but most desolate tracts, half covered by glacier, and stretching to the feet of the true pinnacles of the chain.
COPYRIGHT, G. M. WEISTER