With the exception of the comets, all bodies of the Solar System orbit the Sun in the same direction as the Earth, along orbits that lie close to the plane of the Earth's orbit and the Sun's equator. Most objects in the Solar System spin in the same direction as their orbital motion. This motion reflects the common origin postulated for the Solar System by the contraction of a rotating cloud of interstellar gas and dust about 4600 million years ago (see Solar System, origin).
The Sun and its entire retinue are moving in a nearly circular orbit around the center of the Galaxy, which lies about 8500 parsecs away in the constellation Sagittarius. They have a mean velocity of about 220 km s–1 (see galactic rotation). In relation to the stars in its neighborhood, the Solar System is moving with a velocity of 19.4 km s–1 toward a point in the constellation Hercules – the solar apex.
The solar system is formed by the Sun and all of the various heavenly bodies held within its gravitational field, namely, the planets, their moons, and the asteroids. The orbits of the planets and the asteroids all lie within roughly the same geometric plane, and all move in the same direction around the Sun (all clockwise or all counterclockwise, depending on the position from which they are viewed from outside the system). If the various elements of the solar system were not all within the same plane, it would be difficult to represent astrological influences on a two-dimensional chart. With the exception of some of the fixed stars, all of the influences taken into account by contemporary astrology are confined to our solar system.
the system of celestial bodies moving in the region where the sun’s gravitational influence is dominant. The solar system includes the sun, planets, planetary satellites, asteroids, comets, meteoroids, and cosmic dust. The observed dimensions of the solar system are determined by the orbit of Pluto, which is approximately 40 astronomical units (AU) from the sun (see Figure 1). On the other hand, the sphere within which stable motion of celestial bodies around the sun is possible extends almost to the closest stars (230,000 AU). Information on the distant outer region of the solar system is obtained through observation of long-period comets that approach the sun and through study of the cosmic dust that fills the entire solar system.
The overall structure of the solar system was uncovered by N. Copernicus in the mid-16th century. He provided evidence for the motion of the earth and the other planets around the sun. His heliocentric system made it possible for the first time to determine the relative distances of the planets from the sun and, consequently, from the earth. The laws governing the motion of the planets were discovered by J. Kepler in the early 17th century, and the law of universal gravitation was formulated by I. Newton in the late 17th century. These laws formed the basis of celestial mechanics, which investigates the motion of the bodies of the solar system. The study of the physical characteristics of bodies in the solar system became possible only after the invention of the telescope by Galileo. In 1609 he first turned the small telescope he had constructed toward the moon, Venus, Jupiter, and Saturn

and made a number of discoveries that were remarkable for his time. While observing sunspots, he detected the sun’s rotation about its axis.
In their physical characteristics the planets are divided into the inner planets (Mercury, Venus, the earth, and Mars) and the outer, giant planets (Jupiter, Saturn, Uranus, and Neptune). Since the physical characteristics of Pluto are qualitatively different from those of the giant planets, it cannot be classified as a giant planet. Figure 2 shows the relative sizes of the sun and planets.
An extensive program of observations conducted in 1963 by the American astronomer C. Tombaugh in search of planets lying beyond the orbit of Pluto failed to yield positive results. Table 1 gives the osculating elements of the planetary orbits (seeORBIT OF A CELESTIAL BODY) according to Oesterwinter and Cohen of the USA (1972). The orbits of the planets are slightly inclined with respect to each other and to the invariable plane of the solar system.
Approximately 90 percent of the natural satellites of the planets are grouped around the outer planets. Indeed, Jupiter and Saturn, together with their satellites, make up, as it were, miniature solar systems. Some satellites are extremely large; for example, Jupiter’s satellite Ganymede is bigger than the planet Mercury. In addition to ten satellites, Saturn has a system of rings consisting of a large number of small bodies whose motion obeys Kepler’s laws; these bodies are also essentially satellites of Saturn. The radius of the outermost ring is 2.3 radii of Saturn—that is, the rings lie within Roche’s limit.
By 1976, the exact orbits of more than 2,000 asteroids had been calculated; the orbits lie for the most part between the orbits of Mars and Jupiter. In some cases, the orbits of the asteroids differ considerably in shape and position from the orbits of the planets. The inclinations of the asteroids’ orbits to the plane of ecliptic can be as great as 52°, and the eccentricities of their orbits can be as great as 0.83. Because of their large eccentricities, some asteroids approach the sun closer than does Mercury and move as far away from the sun as Saturn’s orbit. The total number of asteroids observable by present-day telescopes is estimated at 40,000.
When viewed from the north celestial pole, the motion of the planets and planetary satellites and the rotation of these bodies about their axes are counterclockwise—that is, in the direction customarily referred to as direct. Exceptions are the rotation of Venus and Uranus and the retrograde motion of some satellites around their primaries. The distances between the orbits of the planets are described by the empirical Titius-Bode law.
Comets differ markedly in appearance, dimensions, and orbital characteristics from other bodies in the solar system. The periods of revolution of comets can be as great as several million years; at aphelion such comets approach the boundaries of the solar system and experience gravitational perturbations from nearby stars. The orbits of comets vary in inclination from 0° to 180°. The total number of comets is estimated to be hundreds of billions.
Meteoroids (seeMETEOR) and cosmic dust fill all space in the solar system. The motion of cosmic dust is influenced not only by
| Table 1. Elements of the planetary orbits (1973 data) | ||||
|---|---|---|---|---|
| Planet | Mean distance from sun (AU) | Eccentricity of orbit | Inclination of orbital plane to ecliptic (degrees) | Period of revolution about sun (years) |
| Mercury ............... | 0387 | 0.206 | 7.00 | 0.24 |
| Venus ............... | 0.723 | 0.007 | 3.39 | 0.62 |
| Earth ............... | 1.000 | 0.016 | 1.00 | |
| Mars ............... | 1.524 | 0.093 | 1.85 | 1.88 |
| Jupiter ............... | 5.203 | 0.043 | 1.31 | 11.86 |
| Saturn ............... | 9.539 | 0.056 | 2.49 | 29.46 |
| Uranus ............... | 19.19 | 0.046 | 0.77 | 84.02 |
| Neptune ............... | 30.06 | 0.008 | 1.77 | 164.79 |
| Pluto ............... | 39.75 | 0.253 | 17.15 | 250.6 |
the attraction of the sun and planets but also by solar radiation; the motion of electrically charged particles is influenced also by the magnetic fields of the sun and planets. Inside the earth’s orbit the density of the cosmic dust increases, and the dust forms a cloud surrounding the sun that is visible from the earth as the zodiacal light.

The question of the stability of the solar system is closely connected with the presence of secular terms in the semimajor axes, eccentricities, and inclinations of the planetary orbits (seePERTURBATIONS OF CELESTIAL BODIES). Classical methods of celestial mechanics, however, do not take into account small dissipa-tive factors, such as the continuous loss of mass by the sun, that may play an important role in the evolution of the solar system over long periods of time. The solar system participates in the rotation of the Galaxy and moves in an approximately circular orbit at a speed of about 250 km/sec. The solar system’s period of revolution about the center of the Galaxy has been determined to be about 200 million years. The problem of the origin of the solar system is one of the most important questions in modern science (seeCOSMOGONY). The solution of this problem is particularly difficult because the solar system is the only such system we have knowledge of. Suppositions have been advanced that the nearest stars have dark companions of planetary dimensions. The existence of such companions is extremely likely, but conclusive confirmation has not yet been provided. The age of the solar system is estimated at 5 billion years.
The space age has furnished astronomy with new means of studying the solar system. Soviet and American space probes are intensively investigating the inner planets of the solar system. Soviet space probes have made soft landings on the moon, Venus, and Mars. The first manned landing on the surface of the moon was made in 1969 by American astronauts. Between 1972 and 1974 the American space probes Pioneer 10 and Pioneer 11 were launched, crossed the asteroid belt, and made close passes of Jupiter. Plans are being made for flights to periodic comets and for the soft landing of a spacecraft on an asteroid approaching close to the earth. Mankind is beginning to gain practical mastery of the inner region of the solar system.
G. A. CHEBOTAREV