the far distance to the east, and out of it sprung the Snake River Indians.
Such is the native physiography and anthropogenesis of the land of the Oregon.
If now one could rise on the pinions of the Chinook wind (the warm south wind of the Columbia Basin, of which more anon), and from the southern springs of the Owyhee and the Malheur could wing his way to the snowy peaks in British Columbia, from whose fastnesses there issues the foaming torrent of Canoe River, the most northerly of all the tributaries of the Great River, he would obtain, in a noble panorama, a view of the land where the River flows, in its present aspect, as fashioned by the elemental forces of which we have spoken. But not to many is it given thus to be "horsed on the sightless couriers of the air," and we must needs use imagination in lieu of them. Even a map will be the safest guide for most. Inspection of the map will show that the distance to which we have referred covers twelve degrees of latitude, while the distance from the source of the Snake River in the Yellowstone National Park to the Pacific requires a span of fifteen degrees of longitude. The south-eastern part of this vast area occupying Southern Idaho is mainly an arid plain; arid, indeed, in its natural condition, but, when touched by the vivifying waters in union with the ardent sun, it blossoms like a garden of the Lord. Upon these vast plains where the volcanic dust has drifted for ages, now looking so dismal in their monotonous garb of sage-brush, the millions of the future will some time live in peace and plenty, each under his own vine and apple-tree. On the eastern boundary, all the way from Western
