American Journal of Science, March.—Trinidad pitch, by S. F. Peckham and Laura A. Linton. This paper gives an account of the physical and chemical properties of pitch from the Pitch Lake of Trinidad, together with a map of the lake itself. A dry sample of the true lake pitch contained 34·2 per cent, petrolene, 18·8 per cent, asphaltene, 11·4 per cent, of other organic matter, and 35·6 per cent. of inorganic matter. The pitch as it occurs is a unique substance found nowhere else in nature. It consists of a mixture of bitumen, water, sand, decayed vegetation, and gas in such definite proportions that within certain limits the composition of the entire mass is uniform.—Proofs of the rising of the land round Hudson Bay, by Robert Bell. The old shorelines in the provinces of Ontario and Quebec slope upward in a north-easterly direction at rates varying in different regions from a few inches to a foot and even two feet per mile. Many former landing-places about the bay are now high and dry. The rising is apparently still in progress.—Experiments upon the kathode rays and their effects, by A. W. Wright. In developing “shadowgraphs,” it is better not to use any alkaline accelerator at all until just at the end of the process. Röntgen rays passing through glass walls do not show magnetic deflection or mutual repulsion; but when they are made to pass through gold-leaf instead, they show traces of these phenomena, probably owing to the fact that they carry with them small portions of volatilised and electrified metal.—Triangulation by means of kathode photography, by John Trowbridge. The principle of triangulation may be applied to kathode photography when determining the situation of metallic particles in the body. By using two vacuum tubes in different positions, two pictures of, say, a bullet embedded in a hand may be obtained, and their distance apart gives the depth at which the bullet may be sought.—Notes of observations on the Röntgen rays, by H. A. Rowland, N. R. Carmichael, and L. J. Briggs. Some photographs of a coin obtained by Röntgen's method, showed no penumbra when the coin was 2 cm. from the plate. In a very high vacuum tube the source of the active rays was distinctly traced to the anode.
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