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Hyperbola, by what law of centrifugal force tending from the centre of the figure it is described by a revolving body, 116 |
β by what law of centrifugal force tending from the focus of the figure it is described by a revolving body, 117 |
β by what law of centripetal force tending to the focus of the figure it is described by a revolving body, 118 |
Hypotheses of what kind soever rejected from this philosophy, 508 |
Jupiter, its periodic time, 388 |
β its distance from the sun, 388 |
β its apparent diameter, 386 |
β its true diameter, 399 |
β its attractive force, how great, 398 |
β the weights of b dies on its surface, 399 |
β its density, 399 |
β its quantity of matter, 399 |
β its perturbation by Saturn, how much, 403 |
β the proportion of its diameters exhibited by computation, 409 |
β and compared with observations, 409 |
β its rotation about its axis, in what time performed, 409 |
β the cause of its belts hinted at, 445 |
Light, its propagation not instantaneous, 246 |
β its velocity different in different mediums, 245 |
β a certain reflection it sometimes suffers explained, 245 |
β its refraction explained, 243 |
β refraction is not made in the single point of incidence, 247 |
β an incurvation of light about the extremities of bodies observed by experiments, 246 |
β not caused by the agitation of any ethereal medium, 368 |
Magnetic force, 94, 304, 397, 454 |
Mars, its periodic time, 388 |
β its distance from the sun, 389 |
β the motion of its aphelion, 405 |
Matter, its quantity of matter defined, 73 |
β its vis insita defined, 74 |
β its impressed force defined, 74 |
β its extension, hardness, impenetrability, mobility, vis inertiΓ¦, gravity, how discovered, 385 |
β subtle matter of Descartes inquired into, 320 |
Mechanical Powers explained and demonstrated, 94 |
Mercury, its periodic time, 388 |
β its distance from the sun, 389 |
β the motion of its aphelion, 405 |
Method of first and last ratios, 95 |
β of transforming figures into others of the same analytical order, 141 |
β of fluxions, 261 |
β differential, 447 |
β of finding the quadratures of all curves very nearly true, 448 |
β of converging series applied to the solution of difficult problems, 271, 436 |
Moon, the inclination of its orbit to the ecliptic greatest in the syzygies of the node with the sun, and least in the quadratures, 208 |
β the figure of its body collected by calculation, 454 |
β its librations explained, 405 |
β its mean apparent diameter, 453 |
β its true diameter, 453 |
β weight of bodies on its surface, 453 |
β its density, 453 |
β its quantity of matter, 453 |
β its mean distance from the earth, how many greatest semi-diameters of the earth contained therein, 453 |
β how many mean semi-diameters, 454 |
β its force to move the sea how great, 449 |
β not perceptible in experiments of pendulums, or any statical or hydrostatical observations, 452 |
β its periodic time, 454 |
β the time of its synodical revolution, 422 |
β its motions, and the inequalities of the same derived from their causes, 413, 144 |
β revolves more slowly, in a dilated orbit, when the earth is in its perihelion; and more swiftly in the aphelion the same, its orbit being contracted, 413, 444, 445 |
β revolves more slowly, in a dilated orbit, when the apogΓ¦on is in the syzygies with the sun; and more swiftly, in a contracted orbit, when the apogΓ¦on is in the quadratures, 445 |
β revolves more slowly, in a dilated orbit, when the node is in the syzygies with the sun; and more swiftly, in a contracted orbit, when the node is in the quadratures, 446 |
β moves slower in its quadratures with the sun, swifter in the syzygies; and by a radius drawn to the earth describes an area, in the first case less in proportion to the time, in the last case greater, 413 |
β the inequality of those areas computed, 420 |
β its orbit is more curve, and goes farther from the earth in the first case; in the last case its orbit is less curve, and comes nearer to the earth, 415 |
β the figure of this orbit, and the proportion of its diameters collected by computation, 423 |
β a method of finding the moon s distance from the earth by its horary motion, 423 |
β its apogΓ¦on moves more slowly when the earth is in its aphelion, more swiftly in the perihelion, 414, 445 |
β its apogΓ¦on goes forward most swiftly when in the syzygies with the sun; and goes backward in the quadratures, 414, 446 |
β its eccentricity greatest when the apogΓ¦on is in the syzygies with the sun; least when the same is in the quadratures, 414, 446 |
β its nodes move more slowly when the earth is in its aphelion, and more swiftly in the perihelion, 414, 445 |
β its nodes are at rest in their syzygies with the sun, and go back most swiftly in the quadratures 414 |
Moon the motions of the nodes and the inequalities of its motions computed from the theory of gravity, 427, 430, 434, 436 |
β the same from a different principle, 437 |
β the variations of the inclination computed from the theory of gravity, 441, 443 |
β the equations of the moon s motions for astronomical uses, 445 |
β the annual equation of the moon s mean motion, 445 |
β the first semi-annual equation of the same, 443 |
β the second semi-annual equation of the same, 447 |
β the first equation of the moon s centre, 447 |
β the second equation of the moon s centre, 448 |
Moon's first variation, 425 |
β the annual equation of the mean motion of its apogee, 445 |
β the semi-annual equation of the same, 447 |
β the semi-annual equation of its eccentricity, 447 |
β the annual equation of the mean motion of its nodes, 445 |
β the semi-annual equation of the same, 437 |
β the semi-annual equation of the inclination of the orbit to the ecliptic, 444 |
β the method of fixing the theory of the lunar motions from observations, 464 |
Motion, its quantity defined, 73 |
β absolute and relative, 78 |
β absolute and relative, the separation of one from the other possible, demonstrated by an example 82 |
β laws thereof, 83 |
β of concurring bodies after their reflection, by what experiments collected, 91 |
β of bodies in eccentric sections, 116 |
β in moveable orbits, 172 |
β in given superficies, and of the reciprocal motion of pendulums, 183 |
β of bodies tending to each other with centripetal forces, 194 |
β of very small bodies agitated by centripetal forces tending to each part of some very great body, 233 |
β of bodies resisted in the ratio of the velocities, 251 |
β in the duplicate ratio of the velocity, 258 |