Where Rivers and Dunes Collide on Titan

Post contributed by Dr. E. V. Bohacek, European Space Agency (ESA)

In contrast to Earth, where water is cycled through rivers, oceans and the atmosphere, Saturn’s largest moon Titan is a methane world. Liquid methane falls as rain on Titan’s surface, which forms fluvial landforms (rivers), lakes and seas. It is believed that these methane rivers experience episodic activity, with rainfall primarily occurring at the poles and persisting for 10-100 hours per Titan year, equivalent to 30 Earth years (Lorenz, 2014). Another big difference between the fluvial landforms of Titan and the rivers of Earth is their drainage patterns: the distinctive arrangement and organisation of rivers and streams within a river basin. Most rivers on Earth have a dendritic drainage pattern, resembling a branching tree (Image 1 – Yemeni River), whereas on Titan the majority of fluvial landforms branch at right angles in rectangular drainage patterns [Burr et al., 2013] (Image 1 – Titan River). Titan is also covered by vast regions of linear dune fields (Image 1 – Titan Dunes), similar to those observed in the Namib Desert on Earth (Image 1 – Namib Dunes), primarily within the equatorial latitudes [Rodriguez et al., 2014], thought to be composed of hydrocarbon and nitrile sand-sized particles formed from photochemical reactions in Titan’s atmosphere (Hirai et al., 2023). Although observations of Titan are limited to those taken by Cassini-Huygens from 2005-2017, interactions between rivers and dunes have been observed. It is possible that these interactions could partially explain the presence of rectangular drainage patterns. 

Image 1: (Top Left) An example of a typical river valley system on Earth with a dendritic drainage pattern in Yemen [Source: Landsat]. (Top Right) Fluvial landform annotated in blue by Burr et al., (2013) in radar imagery of Titan, showing a rectangular drainage pattern [Source: NASA Cassini]. (Bottom Left) Radar image of linear dunes in the Namib Desert on Earth. The linear dunes, similar in size to those on Titan, are 1-2 km apart. (Bottom Right) Linear dunes in Titan’s sand sea imaged by Synthetic Aperture Radar [Source: NASA Cassini].

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Titan’s labyrinth terrain

Post contributed by Michael J. Malaska, PhD, Scientist, Jet Propulsion Laboratory / California Institute of Technology, USA.

Saturn’s moon Titan is where organic chemistry and surface geomorphology intersect to create an enigmatic landscape with many features in common with Earth, but that are made of completely different materials. Much of Titan’s surface is made up of organic sedimentary materials; recent mapping shows that plains and dunes cover over 80 percent of the globe. The Cassini spacecraft’s Synthetic Aperture Radar (SAR) was able to penetrate Titan’s thick haze and reveal areas of highly dissected plateaux on the surface that are called labyrinth terrain. Image 1 shows an SAR image of an example of this type of terrain, the Sikun Labyrinth. Detailed examination of Titan’s labyrinth terrain can tell us a lot about Titan’s geological history and surface evolution.

Image 1. Top: Image of the Sikun Labyrinth in the south polar terrain of Titan. The blue arrow and number at top left indicates direction of radar illumination and incidence angle for this scene. Bottom: diagram showing how radar illumination interacts with terrain of valleys and plateaux. Image credit: Mike Malaska.
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