SEC. Vlll.J OF NATURAL PHILOSOPHY. VJ61 body, VP the thread, V the point of suspension, RPQS the cycloid whicL ii L N the pendulum describes, P its lowest point, PQ an arc equal to the neight AE. The force with which the motion of the water is accelerated and re tarded alternately is the excess of the weight of the water in one leg above the weight in the other; and, therefore, when the water in the leg KL ascends to EF, and in the other leg descends to GH, that force is double the weight of the water EABF, and therefore is to the weight of the whole water as AE or PQ, to VP or PR. The force also with which the body P is accelerated or retarded in any place, as Q, of a cycloid, is (by Cor. Prop. LI) to its whole weight as its distance PQ, from the lowest place P to the length PR of the cycloid. Therefore the motive forces of the water and pendulum, describing the equal spaces AE, PQ, are as the weights to be moved ; and therefore if the water and pendulum are quiescent at first, those forces will move them in equal times, and will cause them to go and return together with a reciprocal motion. Q.E.D. COR. 1. Therefore the reciprocations of the water in ascending and de scending are all performed in equal times, whether the motion be more or less intense or remiss. COR. 2. If the length of the whole water in the canal be of 6J feet oi French measure, the water will descend in one second of time, and will ascond in another second, and so on by turns in infinitum ; for a pendulum of Sy'-j such feet in length will oscillate in one second of time. COR. 3. But if the length of the water be increased or diminished, the time of the reciprocation will be increased or diminished in the subduplicate ratio of the length. PROPOSITION XLY. THEOREM XXXVI. The velocity of waves is in the subduplicate ratio of the breadths. This follows from the construction of the following Proposition. PROPOSITION XLVI. PROBLEM X. To find the velocity of waves. Let a pendulum be constructed, whose length between the point of sus pension and the centre of oscillation is equal to the breadth of the waves