Abstract
I have pleasure in furnishing herewith tables of magnetic values of declination, horizontal and vertical intensity for the Agincourt Magnetic Observatory and of declination for the Meanook Magnetic Observatory, these values being the results of our magnetic observations made in connection with the solar eclipse of June 8, 1918. The values furnished in each case for Agincourt and Meanook are from eye readings at minute intervals reduced to I. M. S.: at Agincourt, eye readings of differential magnetometers, and at Meanook, eye readings of magnetometer 48. The observer at Meanook was late starting owing to his having accidentally broken suspension in Elliott Magnetometer 48 on the morning of June 8.[Tables 1–8 are based upon the data transmitted to the Journal. The data are plotted and discussed in the report by L. A. Bauer, H. W, Fisk and S. J. Mauchly, begun in this issue.‐Ed.]
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