Remote Sensing Tutorial Page 19-19


We continue with our exploration of three more larger saturnian satellites - Rhea, Iapetus, and Titan, and representatives of the smaller, irregular ones. Rhea and Iapetus are both cratered, and have terrains of differing darkness. Titan is a “maverick”, being surrounded by a nitrogen atmosphere and some organic molecules that give it a distinctive reddish-orange color.


Rhea (1,530 km [951 miles] in diameter) is very similar to Dione, in having a leading hemisphere that has crater densities comparable to the Moon and Mercury, as is hinted at in this full disk view, and a trailing hemisphere with few craters, streaks (ejecta rays?), and fractures.

Full view natural color image of Saturn�s Rhea; the surface to the right is more cratered than that to the left; Voyager.

This is the heavily cratered side of Rhea:

Voyager image of the heavily crater region of Rhea.

This same theme repeats at Iapetus (1,460 km [907 miles] in diameter), which is further from Saturn. The leading hemisphere has a very low albedo (0.03-0.06), in sharp contrast to previously described satellites, and with abrupt boundaries, against the trailing edge terrain (albedo about 0.5), which is heavily cratered. The nature of this dichotomy between satellites is still unknown. This trailing-edge material may have emerged from within Iapetus during crustal foundering. But, the dark terrain is consistent with silicates that have high carbon content, such as those that comprise carbonaceous chondrite meteorites. Thus, this part of Iapetus could have formed as ejecta, which came from another satellite or even from infall of a similar, asteroid-like body.

Voyager image of Iapetus with its two-toned terrains.

  Between Rhea and Iapetus is the large (5,150 km [3,200 mi]) satellite Titan, which is a “maverick” among the icy group, in that it is quite different in its appearance owing to the presence of an atmosphere with a distinctive color described as a brownish-orange.

Color-enhanced Voyager image of Titan, a satellite of Saturn with a dense atmosphere.

Some of the variations in the atmosphere can be discerned as Titan rotates. Here are four views obtained through the Hubble Space Telescope:

Four views of Titan taken at different times by the HST>.

The color version can be enhanced to bring out as many details as possible - rendered in reds and yellows - rather than in the natural color that is a medium brownish-yellow. Titan appears unlike the others because its dense atmosphere (with surface pressures of 1.5 atm, about 50% higher than Earth’s) hides its surface. We show some of this atmospheric structure here:

Color-enhanced Voyager closeup image of the atmosphere on Titan, which consists of about 90% molecular nitrogen, 6% argon, with the remainder methane and organic derivatives

This atmosphere consists of about 90% molecular nitrogen, 6% argon, with the remainder being methane and organic derivatives, such as hydrogen cyanide, ethane, acetylene, and CO2. Solar radiation breaks some of these constituents into colored compounds, analogous to urban smogs on Earth. Ammonia, now a trace constituent, may once have been more abundant, until dissociating into carbon-nitrogen compounds.

What is below the clouds is uncertain. At Titan’s surface temperatures (-179° C), the ethane may condense into a liquid “ocean” that is up to a kilometer deep. Below this, Titan probably consists of a layered mix of silicates and water ice. An infrared image, acquired by the Hubble Space Telescope, suggests that there may be several upwellings of (solid?) material, similar to “continents” (see yellow area in the image above).

This mysterious satellite (larger than Mercury and Pluto) - totally disparate, compared to the other saturnian moons - may harbor still other organic molecules of unusual nature. This surmise just cries out for follow-up study, since no other planet besides Earth or planetary satellite in the Solar System seems so promising for finding and identifying the more complex molecules that may be present.

` <>`__19-66: What is the main implication of this unusual subsurface liquid and the chemical compounds found at Titan? `ANSWER <Sect19_answers.html#19-66>`__

Typical of appropriate small satellites is Phoebe (200 km ]134 miles] diameter), orbiting nearly 4x as far out as Iapetus.

Voyager image of Phoebe, a small irregular satellite orbiting Saturn at about four times the distance of Iapetus to the parent planet.

Slightly larger (286 km; 179 miles) than Phoebe is the more angular Hyperion:

Color view of Hyperion, a small saturnian satellite.

` <>`__19-67: Now that you have been introduced to the saturnian satellites, let’s see how well you can recall and identify each of the larger ones. Examine this montage gallery of 9 satellites and name each one. `ANSWER <Sect19_answers.html#19-67>`__

A montage of the 9 larger satellites of Saturn; the large colored one

shows a more natural color than does the view presented earlier on this page.|

Just as the Galileo spacecraft has added significant knowledge of Jupiter, a sophisticated mission to Saturn is underway. That probe is part of the Cassini mission, named for the 17th Century French-Italian astronomer who pioneered telescopic observations of Saturn. The Cassini spacecraft successfully launched from Cape Canaveral at 4 AM, on October 15, 1997, to begin a 6.7 year journey to the Ringed Planet. The size of a school bus, this vehicle will take a round-about trip to gain velocity by gravity assist “kicks”. By passing Venus twice, then Earth again, and Jupiter later, the spacecraft will use their gravitational pulls to increase its speed enough to reach Saturn. JPL manages the mission, with experiments from NASA, the European Space Agency, the Italian Space Agency, and other participants.

The Cassini Orbiter will explore Saturn’s magnetosphere, its rings, its icy satellites, and eject the Huygens probe to land on Titan. The Orbiter contains a variety of instruments, including a magnetometer, visible imager, radar, UV and IR spectrometers, ion and mass spectrometers, a plasma spectrometer, a dust analyzer, and radio science instruments.

Near the end of 2004, the Cassini Orbiter will release Huygens to descend through the atmosphere of Titan onto its surface. Named for a Dutch astronomer, who discovered this large satellite, the probe will use a large parachute deployed at 175 km (109 mi) to slow its fall. Then, after jettisoning that one, it will deploy a smaller parachute for the final drop onto the surface, postulated to be liquid, but if solid, then the probe should survive the landing. Huygens will carry a descent imager, spectral radiometer, a Doppler wind measuring device, an aerosol collector, a Gas Chromatograph, a Mass Spectrometer, and a surface science package.

Cassini, which cost in excess of a billion dollars (and raised protests from some environmentalists fearful of its 77 grams of plutonium that will serve as a power source), is the most sophisticated and ambitious probe yet sent to explore the planets.


Primary Author: Nicholas M. Short, Sr. email: nmshort@nationi.net