Tethys
Saturn III


 

Tethys [TEE-this] was discovered by Giovanni Cassini in 1684. It is an icy body similar in nature to Dione and Rhea. The density of Tethys is 1.21 gm/cm3, indicating that it is composed almost entirely of water-ice. Tethys's icy surface is heavily cratered and contains cracks caused by faults in the ice. There is one enormous trench on Tethys about 65 kilometers (40 miles) wide and extending from above the center to the extreme left. It covers three-fourths of Tethys' circumference. The fissure is about the size scientists would predict if Tethys were once fluid and its crust hardened before the interior. The canyon has been named Ithaca Chasma. A vast expanse of relative young plains also exists on Tethys. Tethys' surface temperature is -187° C (-305° F).

Tethys Statistics
 Discovered byGiovanni Domenico Cassini 
 Date of discovery1684 
 Mass (kg)7.55e+20 
 Mass (Earth = 1)1.2634e-04 
 Equatorial radius (km)530 
 Equatorial radius (Earth = 1)8.3098e-02 
 Mean density (gm/cm^3)1.21 
 Mean distance from Saturn (km)294,660 
 Rotational period (days)1.887802 
 Orbital period (days)1.887802 
 Mean orbital velocity (km/sec)11.36 
 Orbital eccentricity0.0000 
 Orbital inclination (degrees)1.09 
 Escape velocity (km/sec)0.436 
 Visual geometric albedo0.9 
 Magnitude (Vo)10.2 
 Mean surface temperature-187°C 

Views of Tethys

Tethys
This view of Tethys was taken by Voyager 2 on August 26, 1981. It is the highest resolution image acquired by the Voyager spacecraft. An enormous trench named Ithaca Chasma extends from the left side of this image to the upper center. (Credit: Calvin J. Hamilton)

Tethys Color Composite
This view of Tethys is a color composite of three images taken by Voyager 2 on August 25, 1981. (Credit: Calvin J. Hamilton)

 

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Copyright © 1997 by Calvin J. Hamilton. All rights reserved.