Description
Transcript: Tidal heating is another consequence of gravity acting on moons of planets. The tidal force is the differential force or stretching force on a moon orbiting a planet. Tidal force increases with increasing moon size and decreasing distance from the planet. If the tidal force is too large, the moon will be disrupted, but even a moderate tidal force is enough to cause heating of a moon. Basically the stretching force, in particular in an elliptical orbit where the stretching force changes during the orbit, will cause a flexing of the moon which leads to an increase in its temperature inside. Imagine flexing a tennis ball by squeezing it and letting it go, squeezing it and letting it go. Eventually the tennis ball would warm up. In the same way, tidal forces can cause heating of moons in close orbits around planets, and in extreme cases this tidal heating can lead to volcanic activity.
Transcript: Jupiter's Ganymede is the largest moon in the solar system, just under 5,300 kilometers in diameter. That's 8 percent larger than Mercury and twice the size of tiny Pluto. Ganymede has an old fractured surface covered in groves and fissures. This dark surface is heavily cratered...
Published 07/21/11
Transcript: There are many types of interplanetary bodies, and they contain important clues as to the formation and evolution of the solar system. Interplanetary bodies range in size from 1,000 kilometers to chunks of rock the size of a house and smaller. They range in composition from icy to...
Published 07/21/11
Transcript: Several hundred years ago the astronomer J. Bode noticed a peculiar thing about the spacings and distances of the planets from the Sun. If, for example, you take a sequence of numbers that double, add four to each one and divide by ten you end up almost exactly predicting the...
Published 07/21/11