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Article Images
Dramatic shoreline seen on Titan
 
21 September 2005

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This Synthetic Aperture Radar image of the surface of Saturn's moon Titan was obtained by the NASA/ESA/ASI Cassini spacecraft on 7 September 2005. The bright, rough region on the left side of the image seems to be topographically high terrain that is cut by channels and bays.

The boundary of the bright (rough) region and the dark (smooth) region appears to be a shoreline. The patterns in the dark area indicate that it may once have been flooded, with the liquid having at least partially receded.

The image is 175 kilometres high and 330 kilometres wide, and is located at 66 degrees South, 356 degrees West in the southern hemisphere of Titan. The Cassini-Huygens mission is a cooperative project of NASA, the European

Credits: NASA/JPL

 
 
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This NASA/ESA/ASI Cassini Synthetic Aperture Radar image was acquired as a part of the Titan fly-by observations taken on 7 September 2005, from a distance of about 2000 kilometres. The area is located at about 55 degrees South, 7.5 degrees West longitude and is over 300 kilometres across.

Fluids have flowed and cut these deeply incised channels into the icy surface of Titan. The channels are roughly 1 kilometre across and perhaps 200 metres deep; some can be traced back as far as 200 kilometres. Many of them have angular segments suggesting they may follow faults in Titan's crust. .

Credits: NASA/JPL

 
 
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This NASA/ESA/ASI Cassini Synthetic Aperture Radar image of Titan was taken on 7 September 2005, from a distance of 2000 kilometres from Titan. It is located near 48 degrees South, 14 degrees West and shows an areas about 240 kilometres across.

In contrast to the image of the 'canyonlands' of Titan, this bright terrain is cut by channels that are variable in width; they form both radial and branching networks. Such patterns are reminiscent of networks formed by rainfall on Earth.

At the bottom of the frame, the channels radiate from a possible source into a dark, smooth region that seems flatter and more plain-like. One interpretation is that the higher, rougher terrain has been cleansed of organic debris and eroded by methane rainfall. The removed material has then been deposited into the lower plains.

Credits: NASA/JPL

 


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