{
  "title": "Gullies on the Northwest Rim of Hale Crater",
  "authors": "HiRISE",
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    "excerpt": "Hale is an elliptical-shaped crater, approximately 150 by 125 kilometers, just north of the Argyre Basin."
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        "text": "HiPOD: 16 July 2020"
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        "text": "Gullies on the Northwest Rim of Hale Crater"
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        "caption": "An enhanced color cutout showing bedrock and gullies in detail. Less than 1 km across. (NASA/JPL/UArizona)",
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        "text": "<p><br />While the origin of these gullies is not clear, some have attributes similar to their counterparts on the Earth that result from flowing water. These include upper regions where gully tributaries have eroded into the source rocks, sinuous or “snake-like” channel middle reaches, and down slope regions where gullies distribute and terminate in deposits of sediment and debris.</p>"
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        "text": "<p><br />Bright material deposits are evident along the walls of some gullies. These deposits might be the result of transport or exposure of finer-grained sediments, variations in the brightness of dust or materials, or the presence of ice or fresh deposits within the gullies.<br /></p>"
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        "caption": "A fuller of view of the scene where you can see some of the sedimentary fans at the ends of the gullies. Hale is an elliptical-shaped crater, approximately 150 by 125 kilometers, just north of the Argyre Basin. (NASA/JPL/UArizona)",
        "URL": "https://static.uahirise.org/anews/2020-07-16/ESP_014074_1445-2.jpg"
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        "text": "<p><br />ID: <a href='https://uahirise.org/ESP_014074_1445'>ESP_014074_1445</a><br />date: 28 July 2009<br />altitude: 255 km<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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