intriguing-rock-types
The Curiosity rover is about to finally begin its mission on Mars, after years – decades, depending on who’s telling the story – of instrument development and mission planning. One key aspect of that planning was the selection of the mission’s landing site. The target is Gale Crater, a 154-kilometer diameter impact crater that formed between about 3.5 and 3.8 billion years ago.
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Ashwin Vasaveda, the mission’s Deputy Project Scientist, explained the benefits in a presentation at the Mars Society’s annual convention in Pasadena on Saturday. “We’re landing more accurately than any previous mission, which allows us to put our ellipse next to something that is far too dangerous to actually land on,” he said, referring to Mt. Sharp.
The mound’s layers are best seen with the Mars Reconnaissance Orbiter’s HiRISE camera – the highest resolution camera ever flown around the Red Planet. In the vernacular of sedimentary geology, different layers result from different environmental conditions, so the mineralogically distinct deposits mean that Curiosity should see clues of many past martian environments.
The images that follow show some of HiRISE’s greatest hits from Gale Crater, a preview of geological features that Curiosity may soon get to know in intimate detail.
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In the image above, several geological processes have been at work, from wind-formed dunes to impact craters to potential river erosion. Many of the rock units shown here displayed spectroscopic signatures of sulfates and clays – the types of rocks that drew scientists to Gale in the first place due to their association with water.
*Image: NASA/JPL/University of Arizona*
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