Jupiter has dozens of moons orbiting it, as well as a dusty ring. The four biggest moons were first seen by Galileo over four hundred years ago. Each of these four has some unique characteristic about it. Each has a distinctly different interior. •Io the innermost of the group,has a dozen or so volcanoes erupting at any given time. It’s hard to find craters on the surface of Io since the surface is constantly being buried by those eruptions.•Europa has perhaps the smoothest surface of any object in the solar system. It is also the closest thing to a perfect sphere. Beneath its icy surface we suspect an ocean of liquid water. Who knows what might live in that ocean?•Ganymede is the largest moon in the entire solar system. It appears as if Ganymede has an interior active enought to sustain plate tectonics on the surface of this moon.•Callisto, is the outermost of the four. It is heavily battered with craters and apparently dead to the core. There are also many more small moons that orbit the giant planet. Here is a table of their physical characteristics and their orbits.Jupiter was highlighted in the sequel to 2001, “2010 The Year We Make Contact.Let’s rejoin the fictional astronauts of the ‘Voyage to the Planets’ video as they explore Jupiter.
Radius 71,500 kmJupiter is 11.2 times the diameter of Earth, giving it over 1,400 times the volume of Earth. But it is only 318 times as massive.
Rotation 9h 50m Jupiter spins fast enough to make it visibly flattened.
Semi-major axis : 5.2 A.U.Orbital Period : 11.86 years
Mainly hydrogen and helium gas.There are traces of some organic compounds which give the clouds their color
Strongest of all planets. It is thought to be generated by a layer of the interior consisting of liquid metallic hydrogen.Intense radiation zones surround the Jupiter has a metallic hydrogen layer, we think, which might be responsible for the planet's huge magnetic field. The magnetic field traps solar wind particles and makes for a very exciting environment around the planet. Here is how it might sound.
The four big ones ( Io, Europa, Ganymede and Callisto ) were discovered by Galileo. Here's a java applet that will show you the current alignment of these four moons. Some of the remaining moons might be captured minor planets. Jupiter's ring, seen in these images, consists of fine dust particles probably knocked off the inner moons.
The ring of Jupiter is a dusty ring, invisible from Earth. It seems to consist of ground-up asteroid dust. It was first imaged by Voyager I in 1979. Different parts of the ring have different sized particles, giving the ring system a somewhat complicated structure, as seen in these images.