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Lines of Pits in Protonilus Mensae
This observation shows a lobe-shaped debris apron emanating from a massif (shown in the upper left of the image) in the Protonilus Mensae region in the Northern Hemisphere of Mars.
Icy Cliffs and Impact Craters
We’ve come to understand in recent years that about a third of Mars has ice just below the surface.
A Tale of Collapse Terrain
North of Ganges Chasma lies Orson Welles Crater, whose floor contains broken up blocks we call chaotic terrain and which is the source for the major outflow channel Shalbatana Vallis.
Ancient Rivers
Billions of years ago, a river flowed across this scene in Mawrth Vallis. Like on Earth, these river beds can get filled up with rocks that are cemented together.
On the Edge of the South Pole Layered Deposit
This image shows the edge of the Martian South Polar layered deposit. The stack of fine layering is highlighted by the rays of the polar sun.
A Transition from Depressed to Inverted Channels in Gorgonum Basin
This image shows a transition from depressed to inverted channels in the Gorgonum Basin.
An Impact Crater within Nanedi Valles
With this image, we can cross-dating the relative age of the impact with that of the valley system, as well as learning more about the fluvial and morphology characteristics of area.
Distinct Terrain in the Southern Hemisphere
The objective of this observation is to study this patch of variable terrain.
Do Not Adjust Your Television Set
There are parts of Mars that are covered in a fluffy powder that is carved by the wind into odd patterns.
Fed by Channels
This image shows a channel-fed lava flow in Daedalia Planum.