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I have examined many minerals in my apparatus; certain of them gave evidence of radio-activity, e.g., pitchblende, thorite, orangite, fergusonite, cleveite, chalcolite, autunite, monazite, &c. The following is a table giving in ampères the intensity, i, of the current obtained with metallic uranium and with different minerals:—

	i × 1011.
Uranium	2·3
Pitchblende from Johanngeorgenstadt	8·3
Pitchblende from Joachimsthal	7·0
Pitchblende from Pzibran	6·5
Pitchblende from Cornwallis	1·6
Cleveite	1·4
Chalcolite	5·2
Autunite	2·7
Various thorites	0·1
0·3
0·7
1·3
1·4
Orangite	2·0
Monazite	0·5
Xenotime	0·03
Æschynite	0·7
Fergusonite (two samples)	0·4
0·1
Samarskite	1·1
Niobite (two samples)	0·1
0·3
Tantalite	0·02
Carnotite	6·2

The current obtained with orangite (native oxide of thorium) varied greatly with the thickness of the layer. By increasing this thickness from 0·25 m.m. to 6 m.m. the current increased from 1·8 to 2·3.

All the minerals which showed radio-activity contained uranium or thorium: their activity is therefore not surprising, but the intensity of the action in certain cases is unexpected. Thus pitchblendes (ores of uranium oxide) are found which are four times as active as metallic uranium. Chalcolite (double phosphate of copper and uranium) is twice as active as uranium. Autunite (phosphate of uranium and calcium) is as active as uranium. These facts do not accord with previous conclusions, according to which no mineral should be so active as thorium or uranium.

To throw light on this point, I prepared artificial chalcolite by the process of Debray, starting with the pure products. The process consists in mixing a solution of uranium nitrate with a solution of copper phosphate in phosphoric acid and warming to 50° or 60°. After some time, crystals of chalcolite appear in the liquid.

Chalcolite thus obtained possesses a perfectly normal activity, given by its composition; it is two and a-half times less active than uranium.

It therefore appeared probable that if pitchblende, chalcolite, and autunite possess so great a degree of activity, these substances contain a small quantity of a strongly radio-active body, differing from uranium and thorium and the simple bodies actually known. I thought that if this were indeed the case, I might hope to extract this substance from the ore by the ordinary methods of chemical analysis.