Astronomers typically estimate the ages of the surfaces of planets and moons in our solar system by counting the number of craters there. More craters means an older surface. But if the planet or moon has hydrological processes like stream erosion – or wind and weather that cause sand dunes, for example, to fill in the craters – then it’s possible for a world’s surface to appear younger than it actually is. That is the case with Saturn’s largest moon Titan. While most of Saturn’s moons display their ancient faces pockmarked by “thousands and thousands” of craters, scientists say, Titan looks younger than it really is because its craters are being erased.
New research from NASA’s Cassini spacecraft suggests that dunes of exotic, hydrocarbon sand are slowly but steadily filling in Titan’s craters. Catherine Neish, a Cassini radar team associate based at NASA’s Goddard Space Flight Center in Greenbelt, Maryland said in a press release:
So far on Titan, of the 50 percent of the surface that we’ve seen in high resolution, we’ve only found about 60 craters. It’s possible that there are many more craters on Titan, but they are not visible from space because they are so eroded.
Neish said this research is the first quantitative estimate of how much the weather on Titan has modified its surface.
Titan is the only moon in the solar system with a thick atmosphere. It’s the only world besides Earth known to have lakes and seas on its surface. But Titan is in the outer solar system, where temperatures are much colder than on Earth. Its surface temperature is around minus 290 degrees Fahrenheit (94 kelvins). Thus the “hydrological cycle” on Titan doesn’t utilize water. Instead, the rain that falls from Titan’s skies is a mixture of liquid methane and ethane, compounds that are gases at Earth’s temperatures.
Neish and her team compared craters on Titan to craters on Jupiter’s moon Ganymede. Ganymede is a giant moon with a water ice crust, similar to Titan, so craters on the two moons should have similar shapes. However, Ganymede has almost no atmosphere and thus no wind or rain to erode its surface. Neish said:
We found that craters on Titan were on average hundreds of yards [meters] shallower than similarly sized craters on Ganymede, suggesting that some process on Titan is filling its craters.
Bottom line: Using data from NASA’s Cassini spacecraft, which has been orbiting in the Saturn system since 2004, space scientists have made the first quantitative estimate of how much the weather on Titan has modified its surface. Catherine Neish, a Cassini radar team associate based at NASA’s Goddard Space Flight Center, led this research.
Deborah Byrd created the EarthSky radio series in 1991 and founded EarthSky.org in 1994. Today, she serves as Editor-in-Chief of this website. She has won a galaxy of awards from the broadcasting and science communities, including having an asteroid named 3505 Byrd in her honor. A science communicator and educator since 1976, Byrd believes in science as a force for good in the world and a vital tool for the 21st century. "Being an EarthSky editor is like hosting a big global party for cool nature-lovers," she says.