{
  "title": "Higher Terrain between Sinai and Solis Plana",
  "authors": "HiRISE",
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    "excerpt": "The terrain in this observation looks like an ancient uplifted crustal block."
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        "text": "HiPOD: 12 February 2021"
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        "text": "Higher Terrain between Sinai and Solis Plana"
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        "caption": "The area is riddled with faults and ridges that look like uncovered magma dikes. Less than 1 km across. (NASA/JPL/UArizona)",
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        "text": "<p><br />The terrain in this observation looks like an ancient uplifted crustal block. The area is riddled with faults (big cracks that allow rocks to slide) and ridges that look like uncovered magma dikes.<br /><br />A Mars Orbital Camera picture shows the region to be moderately dusty, but rocks do poke out along the ridges. With a high resolution images, we want to know if the dikes are of the same composition as the flood lavas that surround this high terrain. And what material did the dikes intrude upon which can be eroded away? <br /></p>"
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        "role": "photo",
        "layout": "fullBleedLayout",
        "caption": "A larger view of the scene. Less than 5 km across. (NASA/JPL/UArizona)",
        "URL": "https://static.uahirise.org/anews/2021-02-12/ESP_038932_1635-2.jpg"
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        "text": "<p>ID: <a href='https://uahirise.org/ESP_038932_1635'>ESP_038932_1635</a><br />date: 16 November 2014<br />altitude: 252 km (157 mi)<br /><br />NASA/JPL/UArizona</a></p>"
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        "text": "Enhanced color image 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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