Revealing Titan's rugged surface (Forwarded)

ESA News
http://www.esa.int

1 June 2007

Revealing Titan's rugged surface

During its two and a half hour descent, the cameras on Huygens showed
eager scientists on Earth spectacular regions of bright highlands with
river drainages and canyons, bounded by dark plains on Titan. New
information about the composition of the landing region is now ready for
the public.

Since the mission, planetary scientists have been using the Radar System
and the Visible and Infrared Mapping Spectrometer (VIMS), on board the
orbiting Cassini spacecraft to investigate the composition of the region
Huygens flew over.

Before Huygens, Titan's surface was a total mystery. The reason was
simple: it was covered by a very opaque haze. As the probe penetrated the
layer of haze within the atmosphere, "Huygens revealed a previously
invisible world," says Jean-Pierre Lebreton, ESA's Huygens Project
Scientist.

Laurence Soderblom, US Geological Survey, has been trying to make sense
out of what Huygens saw. Surprisingly, one of the things that proved
unexpectedly difficult was locating the Huygens landing site on the images
from Cassini. "When we looked at the SAR images (Synthetic Aperture Radar)
and compared them to the VIMS data, we saw little correlation," reveals
Soderblom.

The boundary between the bright highlands and dark plains that Huygens
drifted over simply did not show up in the radar images. Finally, the clue
came in the form of two isolated dark sands dunes about 30 kilometres
north of the landing site visible in both SAR and Huygens' images. They
are probably composed of sugar-size hydrocarbon grains between 100 and 300
microns in diameter.

Most of Titan's dunes are giants, each one stretching for up to 100
kilometres in length across the dark plains and separated by 10
kilometres. Most importantly, two dunes that showed up in both the radar
and optical images gave the scientists the clue they needed to get to
work. "We started to piece together a model of the way we think the
surface behaves," says Soderblom.

In this model, the area around the Huygens landing site is a huge plain of
dirty water ice over which lie blankets of organic (carbon-bearing)
deposits that make up the bright highlands and dark dunes. The bright
layers are invisible to radar waves, so Cassini SAR images see through to
the lower, dirty water ice layer that is rugged in some places and smooth
in others.

The deposits form when solar ultraviolet radiation and charged particles
react at high altitudes with Titan's abundant methane to produce carbon-
and hydrogen-bearing (hydrocarbon) molecules like ethane and acetylene,
and more complex nitrogen-bearing molecules generally called tholins.
These products drift down to the surface as aerosols much in the same way
smog particles on Earth form and coat surfaces. On Titan however these
deposits may accumulate to thicknesses of hundreds of metres deep.

The dunes are composed of sand-sized material that agglomerated, either
during its descent or when reworked by geological processes on the
surface. The ice and organic landforms are as different from one another
as they are spectacular. To the north of Huygens' landing site are the
bright highlands, displaying channels in a very ramified pattern,
branching four or five times as they climb into the hills.

Stereoscopic images from the Descent Imager/Spectral Radiometer (DISR)
camera on Huygens have now been analysed and show that some of the ridges
between the channels rise to 150-200 metres in height, with slopes of
thirty degrees. "This is extremely rugged terrain," says Soderblom. The
shape suggests that they are drainage channels, cut by liquid methane
falling as rain.

Close-by are stubby canyons with only a few branches. They have probably
been formed by 'spring sapping', whereby methane flows through the
subsurface before emerging as a spring near the base of a hill. The spring
erodes the hillside, causing it to collapse and form a cliff face.

The third area is the flat dark plain. This is mostly water ice mixed with
tholin grit. "Titan's river channels, canyons, and flood plains rival the
variety seen on Earth," says Soderblom. The dark plains show markings that
suggest the region occasionally experiences flash flooding, but not from
the highland drainage channels. Instead large quantities of liquid methane
appear to flow from east to west.

Planetary scientists can now begin to piece together the sequence of
events that led to the formation of this exotic landscape. "Huygens and
Cassini have taken giant steps forward in our understanding of Titan,"
says Soderblom.

For more images of the surface of Titan,
http://www.esa.int/SPECIALS/Cassini-...GM9RR1F_0.html

Note for editors

This article is based on two papers that will appear in a special issue of
the Planetary and Space Science magazine dedicated to Huygens results:
'Correlation between Cassini VIMS spectra and Radar SRA images:
implications for Titan's surface composition and the character of the
Huygens probe landing site', and 'Topography and geomorphology of the
Huygens landing site on Titan', by L. Soderblom et al.

Cassini-Huygens is a joint mission between NASA, ESA and the Italian Space
Agency (ASI).

For more information

L. Soderblom
U.S. Geological Survey, Flagstaff, Arizona, USA
Email: Lsoderblom @ usgs.gov

Jean-Pierre Lebreton, ESA Huygens Project Scientist
Email : Jean.Pierre.Lebreton @ esa.int

[NOTE: Images and weblinks supporting this release are available at
http://www.esa.int/SPECIALS/Cassini-...3F9RR1F_1.html ]