Jupiter's Moons 2


Intro
 Callisto
Ganymede

Io
Europa

Adrastea

Amalthea

Ananke

Carme

Elara

Himalia

Leda

Lysithea

Metis

Pasiphae
Sinope
Thebe
   
  IO: 
Courtesy of NASA/NSSDC/JPL.        Io is the most volcanic moon in the Solar System. It has many different surfaces including volcanic craters, lakes of molten sulfur, mountains, and lava flows. Some spots may reach 1,000 degrees Fahrenheit. When viewed by the Voyager, there were 9 erupting volcanoes all concentrated towards the equator. A detection of water ice or even steam on Io was not found. There were spectral lines of double ionized sulfur. Sulfur was abundant on the surface and because of this the surface of Io, seems white. It is slightly larger than our moon and orbits Jupiter every 1.75 days at a distance of 262,000 miles. As Io orbits Jupiter, the planet's gravity stretches Io slightly. This heats the moon's inner rock, causing the rock to melt and explode in eruptions that shoot gas and sulfur in to the sky. 

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EUROPA
Courtesy of NASA/NSSDC/JPL.        Europa is the smallest of the Galilean moons. It is about 1,942 miles across and 417,000 miles from Jupiter. It completes one orbital every three and a half days. The surface is covered with ice. From a distance, it looks like a smooth, white ball. Compared to our moon, Europa is much brighter with a 64 percent reflectivity compared to the moon's seven percent. The ground based infrared spectra has shown that there is a lot of water ice present on the surface. Europa is covered with brown tinted ice. Scientists believe that more ice or water may like beneath the icy crust. A detailed inspection has shown that there are fewer than twelve circular craters that have been formed from meteoric impacts. This information leads to the belief that Europa's surface is mobile and can erase all but the most recent impacts. There are several types of terrain on the surface. These include plains cut by grooves and ridges. The mottled terrains are either brown or gray, The brown tint is due to angular structures and vertical ridges. The gray regions show less distinction. There are many linear grooves and macula (brown regions). This satellite consists of a rock core covered by a crust of ice. Fractures that have formed may be the result of tidal stresses.

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ADRASTEA
      This satellite was discovered in 1979 by the Voyager. It is third in distance from the planet, about 128,980 km away. Adrastea's period of revolution is 0.298 days and has a 0 degree of inclination as well as an eccentricity of 0. Adrastea's radius is 96 km.

AMALTHEA:
Taken by Voyager 1. Courtesy of NASA/NSSDC/JPL.       This satellite was discovered in 1892. It is 181,300 km away from Jupiter. Amalthea's period of revolution is 0.498 days and has a 0.4 degree of inclination. Its eccentricity is 0 as well. Almathea's orbit of Jupiter takes about twelve hours. It is an irregular ellipsoidal satellite with a cratered surface. It is aligned with Jupiter's shortest axis and the axis of rotation is perpendicular to the plane of the orbit or Jupiter's equator. Amalthea's diameter is 270 km along the longest axis and 155 km along the shortest axis. This moon is the largest among the four inner moons. There may be sulfur rich material on Amalthea because it's reflectivity is very low and its color is a dark red. 

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ANANKE:
       This satellite was discovered in 1951. It is the 14th in distance from the planet, about 21,200,000 km away. Ananke's period of revolution is 631 days and has a 147^2 degree of inclination. Ananke's eccentricity is 0.17. It's radius is 3375 km.

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Jupiter and its moon Io. Courtesy of NASA/NSSDC.

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