John Muir

Wrangell Island is about fourteen miles long, separated from the mainland by a narrow channel or fiord, and trending in the direction of the flow of the ancient ice-sheet. Like all its neighbors, it is densely forested down to the water's edge with trees that never seem to have suffered from thirst or fire or the axe of the lumberman in all their long century lives.

I left San Francisco for Glacier Bay on the steamer City of Pueblo, June 14, 1890, at 10 A.M., this being my third trip to southeastern Alaska and fourth to Alaska, including northern and western Alaska as far as Unalaska and Pt. Barrow and the northeastern coast of Siberia. The bar at the Golden Gate was smooth, the weather cool and pleasant. The redwoods in sheltered coves approach the shore closely, their dwarfed and shorn tops appearing here and there in ravines along the coast up to Oregon. The wind-swept hills, beaten with scud, are of course bare of trees.

The most interesting of the short excursions we made from Fort Wrangell was the one up the Stickeen River to the head of steam navigation. From Mt. St. Elias the coast range extends in a broad, lofty chain beyond the southern boundary of the territory, gashed by stupendous canyons, each of which carries a lively river, though most of them are comparatively short, as their highest sources lie in the icy solitudes of the range within forty or fifty miles of the coast.

I started off the morning of July 11 on my memorable sled-trip to obtain general views of the main upper part of the Muir Glacier and its seven principal tributaries, feeling sure that I would learn something and at the same time get rid of a severe bronchial cough that followed an attack of the grippe and had troubled me for three months. I intended to camp on the glacier every night, and did so, and my throat grew better every day until it was well, for no lowland microbe could stand such a trip. My sled was about three feet long and made as light as possible.

All California has been glaciated, the low plains and valleys as well as the mountains. Traces of an ice-sheet, thousands of feet in thickness, beneath whose heavy folds the present landscapes have been molded, may be found everywhere, though glaciers now exist only among the peaks of the High Sierra. No other mountain chain on this or any other of the continents that I have seen is so rich as the Sierra in bold, striking, well-preserved glacial monuments. Indeed, every feature is more or less tellingly glacial.

One-Day Excursions

No. 1.

In the wild gold years of 1849 and '50, the Indian tribes along thus western Sierra foothills became alarmed at the sudden invasion of their acorn orchard and game fields by miners, and soon began to make war upon them, in their usual murdering, plundering style. This continued until the United States Indian Commissioners succeeded in gathering them into reservations, some peacefully, others by burning their villages and stores of food.

The good old pioneer, Lamon, was the first of all the early Yosemite settlers who cordially and unreservedly adopted the Valley as his home.

Galen Clark was the best mountaineer I ever met, and one of the kindest and most amiable of all my mountain friends. I first met him at his Wawona ranch forty-three years ago on my first visit to Yosemite. I had entered the Valley with one companion by way of Coulterville, and returned by what was then known as the Mariposa trail. Both trails were buried in deep snow where the elevation was from 5000 to 7000 feet above sea level in the sugar pine and silver fir regions. We had no great difficulty, however, in finding our way by the trends of the main features of the topography.