"On Earth, desert dunefields are periodically flooded by water in areas of fluctuating groundwater, and where lakes, rivers and coasts are found in proximity. These periodic floods leave tell-tale patterns behind them," said Mary Bourke from Trinity College Dublin in the UK.
"You can imagine our excitement when we scanned satellite images of an area on Mars and saw this same patterned calling card, suggesting that water had been present in the relatively recent past," said Bourke.
Fieldwork subsequently showed that these arcuate striations resulted from dune sediments that had been geochemically cemented by salts left behind by evaporating groundwater.
These dune sediments later become relatively immobile, which means they are left behind as the dunes continue to migrate downwind.
"Following our work in Namibia, we hypothesise that on Mars, similar arcuate striations exposed on the surface between dunes are also indications of fluctuating levels of salty groundwater, during a time when dunes were actively migrating down the valley," Bourke said.
"This location is now a potential geological target for detecting past life forms on the Red Planet, which is important to those involved in selecting sites for future missions," she added.
The research was published in the journal Geophysical Research Letters.
Disclaimer: No Business Standard Journalist was involved in creation of this content
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