Image Credit: NASA/JPL/ASU
|
Context image credit: NASA/JPL/MOLA
View on map Detailed information on this image is available at the
THEMIS Data Releases website.
Please see the THEMIS Data Citation Note for details on crediting THEMIS images.
Dust avalanches, also called slope streaks, occur on many
Martian terrains. The deposition of airborne dust on surfaces
causes a bright tone in the THEMIS VIS images. Any movement
of the dust downhill, a dust avalanche, will leave behind
a streak where the darker, dust-free surface is exposed.
These dust avalanches occur on the slopes of Lycus Sulci near Olympus Mons.
|
|||||||||||