{ "title": "Inverted Channels", "authors": "HiRISE", "metadata": { "thumbnailURL": "https://static.uahirise.org/anews/2020-03-11/ESP_055573_1440.jpg", "excerpt": "There is a system of curving, inverted features located on the eastern floor of this crater spanning from the north to the south." }, "version": "1.5", "identifier": "ESP_055568_2050", "language": "en", "layout": { "columns": 10, "width": 1024, "margin": 85, "gutter": 20 }, "documentStyle": { "backgroundColor": "#faf7f2" }, "components": [ { "role": "heading1", "layout": "heading1Layout", "text": "HiPOD: 11 MARCH 2020" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#8c2028" } }, { "role": "title", "layout": "halfMarginBelowLayout", "text": "Inverted Channels" }, { "role": "photo", "layout": "fullBleedLayout", "caption": "Less than 5 km across, 249 km above the surface. (NASA/JPL/UArizona)", "URL": "https://static.uahirise.org/anews/2020-03-11/ESP_055573_1440.jpg" }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "


There is a system of curving, inverted features located on the eastern floor of this crater spanning from the north to the south. These features might be fluvial in origin. If that is the case, high resolution investigation of these features, including the height at which they stand above the preserved surface around them, will help in determining the hydraulic history of the host crater.

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Below is a non-narrated HiClip mini of the observation (less than 5 km across).

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" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#528cb9" } }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "

ID: ESP_055568_2050
date: 4 June 2018
altitude: 249 km

NASA/JPL/UArizona

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