Description
Transcript: For most planets in the solar system the orbital inclination is very small. That is, the axis defined by the north and south poles of the planet is almost exactly perpendicular to the plane of the planet’s orbit of the Sun. The only two exceptions to this are the Earth and Uranus. In the case of the Earth, the orbital axis is tilted by twenty-three and a half degrees, giving Earth its seasons. In the case of Uranus the tilt is even more extreme, more than ninety degrees, so Uranus is tilted almost on its side as it orbits the sun. The causes of these tilts for two of the planets in the solar system are almost certainly collisions with large bodies early in the history of the solar system. In the case of the Earth it was probably the collision that lead to the formation of the Moon.
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