Ever since we discovered dunes on Titan, whose nature was made apparent
by comparison with a space shuttle picture of the Namib sand sea whose
dunes are just the same size and shape as Titan's, I've wanted to visit.
Together with some Titan colleagues (
Prof. Jani Radebaugh of BYU,
Prof. Jason Barnes of U.Idaho, and
Prof. Alex Hayes of Cornell
, we eventually got the
opportunity to go (organizing logistics and permits took many months).
Further images by Jani
here
Starting in Windhoek, we drove (with a ridiculous amount of gear packed
into two VW Polos) via Swakopmund to Gobabeb. From there we made two 4x4
day trips into the north part of the sand sea, getting as far as Tsondab
Vlei. Then back to Windhoek via Swakopmund. In Windhoek we met up with
Roy Miller, former Director of the Geological Survey, who guided us
(with Vernon Swanepoel of Frantic Naturalist tours) down to the mining
town of Rosh Pinah, some 900km to the south. From there we ventured into
the Sperrgebeit, the Forbidden Zone, a designated diamond mining area
and now a national park, to spend two days surveying the Roter Kamm
impact stucture. From there north to Aus (a town set up as a POW camp
for German prisoners in 1915) and thence to the dunes at Sossuvlei and
back to Windhoek. All in all about 2500km in 12 days.
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Windhoek is a very manageably small city, with a notable German
influence (decent beer for a start!). It was a German colony until
1915, when South Africa took control. Because of that there is a bit of
British influence too (e.g. you drive on the left).
While best-known to geomorphologists for its sand dunes, there is a
bonus planetary connection.
There is a striking display of a dozen or so masses of the
Gibeon meteorite (a large iron) in the mall.
Photo:Jani
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The Gobabeb Research and Training Center , right at the edge of the sand
sea, and just south of the Tropic of Capricorn, was a great base for our
dune survey operations. They are self-contained with wind and solar
power, internet access etc., but are right at the edge of the sand sea.
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Among our dune operations were ground-penetrating radar surveys. Here
Karl Arnold (a student at BYU) drags the 250 MHz GPR antenna, while
Clayton Chandler (another student) monitors the data quality. Their
advisor, Prof Radebaugh supervises alongside. This dune is
transverse to the main set, a transitional feature sometimes referred to
as a 'raked' dune.
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Returning from Gobabeb, we visited the corridor of dunes between Walvis
Bay and Swakopmund. With the kite camera I captured these barchans
spalling off the linears. The Atlantic Ocean is just visible in the
background.
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We took a scenic flight over the sand sea, which was an excellent way to
see and understand the different dune types. A number of outfits run
affordable flights from Swakopmund, using high-winged Cessna 210s that give
you a great view. Here I gaze over the near-endless linears in the main
part of the sand sea. Photo by Jani.
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Probably one of the most striking impressions was of the role of the
(usually dry) Kuiseb river, which sharply truncates the dunes at the
northern edge of the sand sea. We suspect that analogous (but unseen,
and usually dry) rivers may define the edges of many dunefields on
Titan, which comprise the same type of dune (linear/longitudinal) as
here.
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Another feature seen on Titan is the deviation of linear dunes by
inselbergs ('island mountains') as here. The horizontal distance out to
which the mountain influences the dune pattern is remarkable, presumably
something to do with the thickness of the planetary boundary layer
(which determines the ultimate height of dunes, and appears to be
similar in the Namib and on Titan).
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We indulged in an afternoon of R&R, exploring the trafficability of
dunes and thus the suitability of rovers for Titan exploration. L-R:
Jani, Clayton, Alex Hayes, myself, Jason Barnes, Karl.
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After getting laundry done, 5 hours drive back to Windhoek, meeting with
the present director of the Geological Survey to get our special
Sperrgebeit permits, some extensive loading operations into a pickup
truck and Roy Miller's custom Land Cruiser kitted out for the field with
2 spares, water tanks, rooftop tent etc., we drove south for about 9
hours to Rosh Pinah (site of a large Zinc mine) and then a couple of
hours cross-country to the Roter Kamm impact crater. It was in fact
quite cold in the evenings, here Karl, Alex, Jason and I watch as Vernon
prepares dinner in the field.
Photo by Jani.
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The 2.5km crater is some 4 million years old, but reasonably
well-preserved for its age because there is little rainfall. It is,
however, substantially filled-in with aeolian sand, and some dunes skirt
the rim and cross the crater in a couple of places, an arrangement we
also see on Titan. Comparing spaceborne radar images with conditions in
the field, we determined that the vegetation (even relatively sparse as
it is) dominates the radar return - in particular, the succulent
Euphorbia bushes may have a branch spacing that acts as a resonant
reflector. Here I fly the kitecam to get a perspective intermediate
between that from orbit and that on the ground.
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In fact, the crater is large enough that it wasnt possible to fit it all
in from the rim. Even with all 1000 feet of line out, I had to come a
bit downwind of the rim to get the camera far enough away to catch the
whole structure, but perseverance (and a stiff breeze) eventually gave
me the shot I wanted. The shallow depth of the crater is evident here.
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The giant dunes, which take on a pyramidal form here where the ephemeral
Tsauchab river occasionally truncates the linear dunes, are among the
highest in the world (although benefit from being built on an earlier
generation of the sand sea, apparently).
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Me on the dune next to dead vlei, the clay pan where the lifeless tree
skeletons show that past conditions have sometimes allowed trees to
grow. The close juxtaposition of dunes with very flat pan surface (Afrikaans:
'vlei') is something that radar data on Titan has been hinting at, but
here is very evident. Photo: Jason.
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Group shot at Sossusvlei, from Alex' camera. Jani, me, Alex, Clay,
Jason and Karl.
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