Titan's surface dissolves like sinkholes on Earth

June 18, 2015
A radar image of Titan’s north polar regions (centre), with close ups of numerous lakes (left) and a large sea (right). The sea, Ligeia Mare, measures roughly 420 x 350 km and is the second largest known body of liquid hydrocarbons on Titan. Its shorelines extend for some 2000 km and many rivers can be seen draining into the sea. By contrast, the numerous lakes are typically less than 100 km across and have more rounded shapes with steep sides. The radar images were created using data collected by the international Cassini spacecraft. Credit: Centre: NASA/JPL-Caltech/ASI/USGS; left and right: NASA/ESA. Acknowledgement: T. Cornet, ESA

Saturn's moon Titan is home to seas and lakes filled with liquid hydrocarbons, but what makes the depressions they lie in? A new study suggests that the moon's surface dissolves in a similar process that creates sinkholes on Earth.

Apart from Earth, Titan is the only body in the Solar System known to possess lakes and seas, as seen by the international Cassini mission. But at roughly –180°C, the surface of Titan is very cold and liquid methane and ethane, rather than water, dominate the 'hydrological' cycle.

Indeed, methane and ethane-filled topographic depressions are distinctive features near the moon's poles. Two forms have been identified by Cassini. There are vast seas several hundred kilometres across and up to several hundred metres deep, fed by river-like dendritic channels. Then there are numerous smaller, shallower lakes, with rounded edges and steep walls, and generally found in flat areas. Many empty depressions are also observed.

The lakes are generally not associated with rivers, and are thought fill up by rainfall and liquids flooding up from underneath. Some of the lakes fill and dry out again during the 30-year seasonal cycle on Saturn and Titan.

But quite how the depressions hosting the lakes came about in the first place is poorly understood.

A team of scientists have turned to home for the answer and discovered that Titan's lakes are reminiscent of 'karstic' landforms seen on Earth. These are terrestrial landscapes that result from erosion of soluble rocks such as limestone and gypsum in groundwater and rainfall percolating through rocks. Over time, this leads to features including sinkholes and caves under humid climates, and salt-pans under more arid climates.

Close-up radar image showing both empty and liquid-filled depressions (coloured blue) on Saturn’s largest moon, Titan. The radar image was created using data collected by the international Cassini spacecraft. Credit: NASA/ESA. Acknowledgement: T. Cornet, ESA

The rate of erosion depends on factors such as the chemistry of the rocks, the rainfall rate and the surface temperature. While all of these aspects clearly differ between Titan and Earth, the underlying process may be surprisingly similar.

A team lead by ESA's Thomas Cornet calculated how long it would take for patches of Titan's surface to dissolve to create these features. They assumed that the surface is covered in solid organic material, and that the main dissolving agent is liquid hydrocarbons, and took into account present-day models of Titan's climate.

The scientists found that it would take around 50 million years to create a 100 m-deep depression at Titan's relatively rainy high polar latitudes, consistent with the youthful age of the moon's surface.

"We compared the erosion rates of organics in on Titan with those of carbonate and evaporite minerals in liquid water on Earth," describes Thomas.

"We found that the dissolution process occurs on Titan some 30 times slower than on Earth due to the longer length of Titan's year and the fact it only rains during Titan summer.

Close-up radar image of Ligeia Mare, the second largest known body of liquid hydrocarbons on Titan. It measures roughly 420 x 350 km and many rivers can be seen draining into the sea. The radar image was created using data collected by the international Cassini spacecraft. Credit: NASA/ESA. Acknowledgement: T. Cornet, ESA

"Nevertheless, we believe that dissolution is a major cause of landscape evolution on Titan, and could be the origin of its lakes."

In addition, the scientists calculated how long it would take to form depressions at lower latitudes, where the rainfall is reduced. The much longer timescale of 375 million years is consistent with the relative absence of depressions in these geographical locations.

"Of course, there are a few uncertainties: the composition of Titan's surface is not that well constrained, and neither are the long-term precipitation patterns, but our calculations are still consistent with the features we see today on Titan's relatively youthful billion-year-old surface," says Thomas.

"By comparing Titan's surface features with examples on Earth and applying a few simple calculations, we have found similar land-shaping processes that could be operating under very different climate and chemical regimes," says Nicolas Altobelli, ESA's Cassini–Huygens project scientist.

"This is a great comparative study between our home planet and a dynamic world more than a billion kilometres away in the outer Solar System."

Explore further: Titan's subsurface reservoirs modify methane rainfall

More information: "Dissolution on Titan and on Earth: Towards the age of Titan's karstic landscapes," Journal of Geophysical Research – Planets, DOI: 10.1002/2014JE004738

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