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T w o field gravity meters were read continuously for a period of 14 days, one at Peebles in South Scotland, the other at Kirklington near Nottingham. The experiments have shown that the observed variations of gravity were proportional to the predicted tide-raising force to within a standard deviation of &,milligal. The factors of proportionality are 1-02 for Kirklington, and 1 -1 0 for Peebles. There were no significant phase Herencea on the average; the individual phase differences were rather irregular.