Seasonal dunes on Mars nicknamed ‘Buzzel’.
Ridges cross the Nepenthes Mensae region, which is often referred to as a river delta for its striking pattern.
The edges of a debris apron, where cliff material eroded away.
Alluvial fans are some of the evidence that scientists used to confirm there was once water on Mars.
A small but recent impact crater.
Scientists use HiRISE to monitor how gullies change over time, which could help them figure out what created them.
Exposed bedrock on the Capri Chasma, which may once have been filled with flood waters.
‘Spiders’ are eruptions of dust caused by the way the Martian surface warms and cools.
Eos Chasma is part of Valles Marineris, the largest canyon on Mars.
Another gully scientists are having HiRISE monitor.
A pedestal crater, where a crater has eroded away at different rates based on different rock types.
Watching Mars defrost
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