Earth and its Moon

Earth and its Moon — page 9
EARTHANDITs MoON Johannes Kepler of Germany assumed this basic view in developing his three laws of planetary motion in the early 17th century One of these laws states that a planet s orbit or path around the Sun is an ellipse with the Sun not at the exact center but at one of two points called foci Earth's orbit turns out to be more nearly a circle than the orbits of most of the other planets Earth's distance from the Sun varies by only a small percent age from about 91 4 million miles 147 1 million kilometers in early January to some 94 5 million miles 152 1 million kilometers in early July THE EFFECT OF GRAVITY In 1687 Isaac Newton of England published his law of universal gravitation in his major work the Principia This explained the plan ets motions as being caused by the Sun s gravitational pull on the planets By this point almost all scientists accepted the heliocentric theory Newton showed that any two objects attract each other with this gravitational force Its strength is proportional to the mass of each object and it becomes weaker with increasing distance between the objects 14