Both the northern and southern slopes of the Chilkoot Pass are largely surfaced with shattered rocks, over which, with occasional deflections across more pleasant snow banks, a fairly well-defined trail mounts on either side to the summit. In its grim landscape effects, more particularly on the inner face, where a number of rock-bound tarns--Crater Lake, Long Lake, Deep Lake--afford a certain relief to the degree of desolation which the scene carries, it reminded me much of the famous Grimsel Pass, and here as well as there the modeling of the surface through glacial action was strongly in evidence. The vastly towering Alpine peaks were, however, wanting, and the glaciers that still appeared showed that they had long since passed their better days. The actual summit is trenched by a narrow rocky gap, roughly worn through walls of granite, and by it have passed the thousands who have pressed to the interior. There is no timber growth at or near this summit, nor is there soil sufficient to give support to an arboreal vegetation. Nearest to the top line a prostrate form of scrubby hemlock (_Tsuga Pattoniana_) alone makes pretense to being a tree, but below it of itself grows to majestic proportions, and about "Sheep Camp," with Menzie's spruce, a birch, and cottonwood (_Populus balsamifera_), forms part of the beautiful woodland, which with ever-increasing freshness descends to the lower levels.

Lest I be accused of too freely seeing the beauties of the northern landscape, I venture in my defense the following graphic description of the Dyea Valley from the pen of another traveler and geologist, Prof. Israel Russell: "In the valley of the Taiya the timber line is sharply drawn along the bordering cliffs at an elevation of about twenty-five hundred feet. Above that height the mountain sides are stern and rugged; below is a dense forest of gigantic hemlocks, festooned with long streamers of moss, which grows even more luxuriantly than on the oaks of Florida. The ground beneath the trees and the fallen monarchs of the forest are densely covered with a soft, feathery carpet of mosses, lichens, and ferns of all possible tints of brown and green. The day I traversed this enchanted valley was bright and sunny in the upper regions, but the valley was filled with drifting vapors. At one minute nothing would be visible but the somber forest through which the white mist was hurrying; and the next the veil would be swept aside, revealing with startling distinctness the towering mountain spires, snowy pinnacles, and turquoise cliffs of ice towering heavenward. These views through the cloud rifts seemed glimpses of another world. Below was a sea of surging branches that filled all the valley bottom and dashed high on the bordering cliffs. Much space could be occupied with descriptions of the magnificent scenery about Lynn Canal, and of the wonderful atmospheric effects to be seen there, but the poetry of travel is foreign to these pages, and must be left for more facile pens."

Appletons' Popular Science Monthly, May 1899 — Part 8