{
  "title": "Colorful Bedrock on the Floor of an Impact Crater",
  "authors": "HiRISE",
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    "excerpt": "HiRISE acquires many images of bedrock exposures inside impact craters, because deep bedrock may be exposed in the central uplift."
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        "text": "HiPOD: 2 November 2020"
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        "text": "Colorful Bedrock on the Floor of an Impact Crater"
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        "caption": "There are layers of rock with different colors (from different minerals) exposed in places where the dark reddish wind-blown drifts have been removed. Less than 1 km across. (NASA/JPL/UArizona)",
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        "text": "<p><br />HiRISE acquires many images of bedrock exposures inside impact craters, because deep bedrock may be exposed in the central uplift, or new deposits may form on the floor.<br /><br />The cutout shows an enhanced-color section of the floor of one crater. There are layers of rock with different colors (from different minerals) exposed in places where the dark reddish wind-blown drifts have been removed.<br /></p>"
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        "role": "photo",
        "layout": "fullBleedLayout",
        "caption": "A fuller view of the scene. Less than 5 km across. (NASA/JPL/UArizona)",
        "URL": "https://static.uahirise.org/anews/2020-11-02/ESP_031099_1355-2.jpg"
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        "text": "<p><br />ID: <a href='https://uahirise.org/ESP_031099_1355'>ESP_031099_1355</a><br />date: 15 March 2013<br />altitude: 248 km (154 mi)<br /><br />NASA/JPL/UArizona</a></p>"
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        "text": "Enhanced color is less than 1 km across; black and white is less than 5 km. For full images with scalebars, see the above ID link to our website.<br /><br />"
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