The placer deposits of the Nome district are in the form of shallow, largely or mostly unfrozen gravels, which occupy varying heights, partly in disrupted or overhanging benches, of the valleys and gulches which trench the slate and limestone mountains. Perhaps the most favored ones are those of Anvil and Glacier Creeks (with Snow Gulch as an affluent of the latter), tributaries of Snake River, and Dexter Creek, a tributary of Nome River. My time and the conditions of weather permitted only of a visit to Anvil Creek, and an examination mainly of the properties about “Discovery.” The diggings here are all shallow, from four to seven feet, when bed-rock, a steeply pitching and highly fissile slate, is reached. As before remarked, the gravels are not frozen, and thereby present a marked contrast to the condition that prevails in the Klondike region, and one, it is hardly necessary to state, which is eminently to the favor of economy in mining. A layer of ice, about eight inches in thickness, covers one side of the layers in claim “No. 1 below,” but beneath this the matrix is again open. In all these claims the pay-streak was at first reported to be very broad, but it seems that the later work has narrowed down the probabilities of extension very measurably--at any rate, in the condition of a rich producer. Of the wealth contained in these claims there is no question, but it would probably be straining the truth to say that it is the equal of that of the best or even the better claims of the Klondike region. A two days’ clean-up from “No. 1 below” is reported to have yielded thirteen thousand dollars, while the entire product of that claim from July 26th, when the first wash was made, to September 21st, was placed at one hundred and twenty-five thousand dollars. Claim “No. 1 above” appears to be equally good, and “Discovery” falls perhaps not very far below either. A nugget of the value of three hundred and twelve dollars--a magnificent specimen, measuring upward of four inches in length--was obtained from the tailings of “No. 1 below”; a larger one, of the value of four hundred and thirty-four dollars, is to the credit of “No. 1 above.” It is interesting to note that these rich claims are located at the very issuance of Anvil Creek from the mountains--i. e., at the contact with the upper rise of the tundra--and other good properties are found still lower down, a condition which makes it certain that the inner reaches of the tundra, whatever the whole tundra may be, must yield largely in gold. [Illustration: “DIGGING” THE SEASHORE SANDS FOR GOLD.]