PHYS 1000 Lecture 8: Chapter 8 – Moons, Rings, and Plutoids
Document Summary
All four jovian planets have extensive moon systems, and more are continually being discovered. We split them into three groups based on the diameter: The formation of jupiter and its moon is a reference of how the sun brought together the solar system. Io, europa, ganymede, callisto are the big moons of jupiter. Io and callisto are simplistic interiors and ganymede and europa are more complex interiors and may have water. Io is the innermost of jupiter"s moons and the most geologically active object in the solar system. It has many active volcanoes, and its surface can be changed in a few weeks. Io has no craters; they fill in too fast youngest surface of any solar system object. The tidal forces are huge, and provide the energy for the volcanoes. Europa has few craters; surface is water ice, possibly with liquid water below. Tidal forces stress and crack ice; water flows, keeping the surface relatively flat.