Two routes may be chosen to the gold-fields.
1. By way of the Yukon River. This is all the way by water, and means nearly 4,500 miles of voyaging.
2. By way of the seaports of Dyea or Shkagway, over mountain passes, afoot or a-horseback, and down the upper Yukon River and down the lakes and rivers by raft, skiff and steamboat.
To describe these routes is the next task—first, that by the way of St. Michael, and second—up the Yukon River.
Route, via St. Michael and the Yukon River.—This begins by a sea-voyage, which may be direct, or along the coast. The special steamers (and future voyages, no doubt) usually take a direct course across the North Pacific and through the Aleutian Islands to St. Michael, in Norton Sound, a bight of Bering Sea. The distance from San Francisco is given as 2,850 miles; from Victoria or Seattle, about 2,200 miles. The inside course would be somewhat longer, would follow the route next to be described as far as Juneau and Sitka, then strike northwest along the coast to St. Michael.
This town, on an island near shore in Norton Sound, was established in 1835 by Lieut. Michael Tébenkoff, of the Russian navy, who named it after his patron saint. Though some distance to the mouth of the Yukon entrance, St. Michael has always been the controlling center and base of supplies for the great valley. The North American Trading and Transportation Company and the Alaska Commercial Company have their large warehouses here, and provide the miners with tools, clothing and provisions. Recently the wharf and warehouse accommodations have been extended, and the population has increased, but if, as is probable, any considerable number of men are stopped there this fall by the freezing of the river, and compelled to pass the winter on the island, they will find it a dreary, if not dangerous experience.
The vessels supplying this depot can seldom approach the anchorage of St. Michael before the end of June on account of large bodies of drifting ice that beset the waters of Norton Sound and the straits between St. Lawrence and the Yukon Delta.
A temporary landing-place is built out into water deep enough for loaded boats drawing five feet to come up at high tide, this is removed when winter approaches, as otherwise it would be destroyed by ice. The shore is sandy and affords a moderately sloping beach, on which boats may be drawn up. A few feet only from high water mark are perpendicular banks from six to ten feet high, composed of decayed pumice and ashes, covered with a layer about four feet thick of clay and vegetable matter resembling peat. This forms a nearly even meadow with numerous pools of water, which gradually ascends for a mile or so to a low hill, of volcanic origin, known as the Shaman Mountain.