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Image Credit: Giphy.com/nasa |
Scientists from the USGS, the University of Arizona, Durham University (England) and the Planetary Science Institute identified the dark, narrow surface features as Recurring Slope Lineae (RSL). These RSL features grew and faded incrementally, recurring annually during the warmest time of the year on Mars.
It was found with further analysis that the terminal ends of these RS slopes were identical to the slopes of sand dunes where movement was caused by dry granular flows. For water to cause these RSLs, the volume of water present would have to correspond to the length of slope available (needing more liquid on longer slopes). However, the similar slopes had very different lengths. Furthermore it was found that water was unlikely to be found near just the tops of the slopes with such defining angles.
Read the full press release at: https://www.usgs.gov/news/previous-evidence-water-mars-now-identified-grainflow
Or read the full study at: https://www.nature.com/articles/s41561-017-0012-5
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