balt, indigo, peacock, ultra-marine, shading at the top into lilac and amethyst. The base of the glacier-face, next to the dark-green water of the bay, resembled a great mass of vitriol, while the top, where it swept out of the canyon, had the curves and tints and delicate lines of the iris.
But the glacier front was not still; in form and color it was changing every minute. The descent was so steep that the glacial rapids above the bay must have flowed forward eighty or a hundred feet a day. The ice cliff, towering a thousand feet over the water, would present a slight incline from the perpendicular inwards toward the canyon, the face being white from powdered ice, the result of the grinding descent of the ice masses. Here and there would be little cascades of this fine ice spraying out as they fell, with glints
