BOOK 111.] OF NATURAL PHILOSOPHY. 401 longitude of the comet at the time of the last observation. The angle, therefore, FQG, which is the difference of the longitude, proceeds from the inequality of the motions of the comet and the earth ; and this angle, if the earth and cornet move contrary ways, is added to the angle TQ,G, and accelerates the apparent motion of the comet ; but if the comet move the same way with the earth, it is subtracted, and either retards the motion ol the comet, or perhaps renders it retrograde, as we have but now explained. This angle, therefore, proceeding chiefly from the motion of the earth, is justly to be esteemed the parallax of the comet; neglecting, to wit, some little increment or decrement that may arise from the unequal motion of the comet in its orbit : and from this parallax we thus deduce the distance of the comet. Let S represent the sun, acT v the orbis tnagnus, a the earth's place in the first observatiun, c the place of the earth in the third observation, T the place of the earth in the last observation, and TT a right line drawn to the beginning of Aries. Set off the angle TTV equal to the angle TQF, that is, equal to the longitude of the comet at the time when the earth is in T ; join ac, and produce it to g1, so as ag may be to ac as AG to AC ; and g will be the place at which the earth would have arrived in the time of the last observation, if it had con tinued to move uniformly in the right line ac. Wherefore, if we draw g'T parallel to TT, and make the angle T^V equal to the angle TQ,G, this angle Tg\ will be equal to the longitude of the comet seen from the place g, and the angle TVg- will be the parallax which arises from the earth's being transferred from the place g into the place T ; and therefore V will be the place of the comet in the plane of the ecliptic. And this place V is commonly lower than the orb of Jupiter. The same thing may be deduced from the incurvation of the way of the comets ; for these bodies move almost in great circles, while their velocity is great ; but about the end of their course, when that part of their appa rent motion which arises from the parallax bears a greater proportion to their whole apparent motion, they commonly deviate from those circles, and when the earth goes to one side, they deviate to the other : and this deflex ion, because of its corresponding with the motion of the earth, must arise chiefly from the parallax ; and the quantity thereof is so considerable, as, by my computation, to place the disappearing comets a good deal lower than Jupiter. Whence it follows that when they approach nearer to us in their perigees and perihelions they often descend below the orbs of Mare and the inferior planets.