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Curiosity scooped the soil on Oct. 15, 2012, the 69th sol, or
Martian day, of operations. It was delivered to CheMin for X-ray diffraction analysis on October 17, 2012, the 71st sol. By directing an X-ray beam at a sample and recording how X-rays are scattered by the sample at an atomic level, the
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This graphic shows results of the first analysis of
Martian soil by the Chemistry and Mineralogy (CheMin) experiment on NASA's Curiosity rover. The image reveals the presence of crystalline feldspar, pyroxenes and olivine mixed with some amorphous (non-crystalline) material. The soil sample, taken
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instrument can definitively identify and quantify minerals on Mars for the first time. Each mineral has a unique pattern of rings, or "fingerprint," revealing its presence.
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joint project implies that all materials created by its probe are copyrighted and require permission for commercial non-educational use.
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from a wind-blown deposit within Gale Crater, where the rover landed, is similar to volcanic soils in Hawaii.
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The following pages on the
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states that all of the images in the photo gallery are in the public domain "Unless otherwise noted."
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The colors in the graphic represent the intensity of the X-rays, with red being the most intense.
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data may be copyrighted if they are not explicitly produced by the
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The NASA website hosts a large number of images from the
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in the United States because it was solely created by
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User:Marshallsumter/Radiation astronomy/Diffractions
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PIA16217-MarsCuriosityRover-1stXRayView-20121017.jpg
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Commons is a freely licensed media file repository.
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PIA16217-MarsCuriosityRover-1stXRayView-20121017.jpg
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121:10.30.2012
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147:Date
17:File
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998:石巢
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239:.)
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
