Mysterious Raisin’s Mountain on Titan Observed
August 30, 2010 1 Comment
Saturn’s moon Titan ripples with mountains, and scientists have been trying to figure out how they form. The best explanation, it turns out, is that Titan is shrinking as it cools, wrinkling up the moon’s surface like a raisin.
A new model developed by scientists working with radar data obtained by NASA’s Cassini spacecraft shows that differing densities in the outermost layers of Titan can account for the unusual surface behavior. Titan is slowly cooling because it is releasing heat from its original formation and radioactive isotopes are decaying in the interior. As this happens, parts of Titan’s subsurface ocean freeze over, the outermost ice crust thickens and folds, and the moon shrivels up. The model is described in an article now online in the Journal of Geophysical Research. Giuseppe Mitri, the lead author of the paper said:
Titan is the only icy body we know of in the solar system that behaves like this,” said But it gives us insight into how our solar system came to be. An example of this kind of process can also be found on Earth, where the crumpling of the outermost layer of the surface, known as the lithosphere, created the Zagros Mountains in Iran.
[Image Details: This mosaic, made from radar images obtained by NASA’s Cassini spacecraft, shows mountainous terrain on Saturn’s moon Titan in the moon’s northern hemisphere, north of the Aaru region. The annotated version shows topographic profiles measured by the radar instrument, with red-orange areas showing the highest elevation (in this image, 600 meters, or 2,000 feet, above the mean radius of Titan) and purple showing the lowest (in this image, 800 meters, or 2,600 feet, below the mean radius of Titan). That version also shows a grid for latitude and longitude. This region presents a mountain block near 52 degrees north latitude and 13 degrees east longitude. The tallest features in this image are about 1,400 meters higher than the valley next to it.
Cassini’s radar instrument obtained the black and white images making up the mosaic on July 22, Sept. 22, and Oct. 9, 2006. In radar images, objects appear bright when they are tilted toward the spacecraft or have rough surfaces. The topographical data were derived from the same flybys. The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate. The Cassini orbiter was designed, developed and assembled at JPL. The radar instrument was built by JPL and the Italian Space Agency, working with team members from the United States and several European countries.]
Titan’s highest peaks rise up to about two kilometers (6,600 feet), comparable to the tallest summits in the Appalachian Mountains. Cassini was the first to spot Titan’s mountains in radar images in 2005. Several mountain chains on Titan exist near the equator and are generally oriented west-east. The concentration of these ranges near the equator suggests a common history.
While several other icy moons in the outer solar system have peaks that reach heights similar to Titan’s mountain chains, their topography comes from extensional tectonics — forces stretching the ice shell — or other geological processes. Until now, scientists had little evidence of contractional tectonics — forces shortening and thickening the ice shell. Titan is the only icy satellite where the shortening and thickening are dominant.
[Image Details: This mosaic, made from radar images obtained by NASA’s Cassini spacecraft, shows parallel mountain chains on Saturn’s moon Titan. The mountains appear along the northwest border of a region known as Xanadu, two degrees south latitude and minus 127 degrees west longitude. The annotated version shows a grid for latitude and longitude. The tallest features in this image, which were mapped by the radar instrument, are about 1,900 meters taller than the surrounding plains. Scientists believe the structures rose up because the lithosphere, the outermost layer of the surface, folded up during deformation of the outer water ice shell. Cassini’s radar instrument obtained the images on Feb. 15, 2005 and May 12, 2008. In radar images, objects appear bright when they are tilted toward the spacecraft or have rough surfaces.
For another view of this terrain, see PIA10654.]
Mitri and colleagues fed data from Cassini’s radar instrument into computer models of Titan developed to describe the moon’s tectonic processes and to study the interior structure and evolution of icy satellites. They also made the assumption that the moon’s interior was only partially separated into a mixture of rock and ice, as suggested by data from Cassini’s radio science team.
Scientists tweaked the model until they were able to build mountains on the surface similar to those Cassini had seen. They found the conditions were met when they assumed the deep interior was surrounded by a very dense layer of high-pressure water ice, then a subsurface liquid-water-and-ammonia ocean and an outer water-ice shell. So the model, Mitri explained, also supports the existence of a subsurface ocean.
Each successive layer of Titan’s interior is colder than the one just inside it, with the outermost surface averaging a chilly 94 Kelvin (minus 290 degrees Fahrenheit). So cooling of the moon causes a partial freezing of the subsurface liquid ocean and thickening of the outer water ice shell. It also thickens the high-pressure ice. Because the ice on the crust is less dense than the liquid ocean and the liquid ocean is less dense than the high-pressure ice, the cooling means the interior layers lose volume and the top “skin” of ice puckers and folds.
Since the formation of Titan, which scientists believe occurred around four billion years ago, the moon’s interior has cooled significantly. But the moon is still releasing hundreds of gigawatts of power, some of which may be available for geologic activity. The result, according to the model, was a shortening of the radius of the moon by about seven kilometers (four miles) and a decrease in volume of about one percent.
These results suggest that Titan’s geologic history has been different from that of its Jovian cousins, thanks, perhaps, to an interior ocean of water and ammonia. As Cassini continues to map Titan, we will learn more about the extent and height of mountains across its diverse surface.