A portion of the specimen was selected for analysis to which the crust was attached on the convex or outer surface only, and which was comparatively free from crust on the opposite surface; the quantity operated on was 15·786 grains. By repeated treatment with warm moderately strong ammonia-water, gentle rubbing, and washing with warm water, the crust was easily removed; most of it being dissolved by the ammonia-water, which became pale blue, while the insoluble part was left as a brownish black powder, intermixed with some particles of metallic silver. The metal, after this treatment and drying, weighed 11·823 grains. The metal itself (a), the portion of the crust soluble in ammonia-water (b), and the residue insoluble in ammonia-water (c) were separately analysed, with the following results:—

COMPOSITION PER CENT.

(a) Metal. Silver 71·60
Gold 0·22
Copper 2·42
Lead 0·33
Iron 0·09
Chlorine traces
74·66
(b) Crust. Chloride of Silver 19·98
Portion
soluble in
ammonia-water.
Protoxide of Copper
(Black Oxide)
} 0·56
Chlorine 0·15
Copper 0·13
Sulphuric Acid traces
Carbonic Acid
Water
} 1·15
21·97
(c) Crust. Gold 0·05
Portion Silver 1·36
insoluble in
ammonia-water.
Protoxide of Copper
(Black Oxide)
} 0·09
Carbonate of Lime 1·36
Silica
Peroxide of Iron
Alumina
} 0·30
3·16
99·79

The composition per cent. of the metal, exclusive of the crust, as calculated from the above analysis, is given underneath; but it certainly cannot be inferred that the original metal had the exact composition shown in that analysis, because some of the ingredients may not have been carried away during corrosion in the same relative proportions in which they were present in the original alloy.

COMPOSITION PER CENT.

Silver95·59
Gold0·30
Copper 3·23
Lead0·44
Iron0·12
99·68

A portion of the crust when heated in a glass tube gave off water, and the glass was stained yellow.

A portion of the crust treated with dilute hydrochloric acid effervesced, the acid became pale blue, and was found to contain copper and lime.

The crust was examined under the microscope, but no trace of crystalline structure could be detected. A qualitative examination was made of a portion of the inner crust, from which it appeared that its composition was similar to that of the outer crust.