{ "title": "Ridges in West Candor Chasma", "authors": "HiRISE", "metadata": { "thumbnailURL": "https://static.uahirise.org/anews/2020-04-08/ESP_063406_1750.jpg", "excerpt": "There are possible landslide-related faults within the layered rocks on the floor of west Candor Chasma." }, "version": "1.5", "identifier": "ESP_063406_1750", "language": "en", "layout": { "columns": 10, "width": 1024, "margin": 85, "gutter": 20 }, "documentStyle": { "backgroundColor": "#faf7f2" }, "components": [ { "role": "heading1", "layout": "heading1Layout", "text": "HiPOD: 8 APRIL 2020" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#8c2028" } }, { "role": "title", "layout": "halfMarginBelowLayout", "text": "Wonderfully Strange" }, { "role": "photo", "layout": "fullBleedLayout", "caption": "An enhanced color coutout using the red-green-blue filter. The blue represents basaltic (volcanic) material. Less than 1 km across. (NASA/JPL/UArizona)", "URL": "https://static.uahirise.org/anews/2020-04-08/ESP_063406_1750.jpg" }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "


There are possible landslide-related faults within the layered rocks on the floor of west Candor Chasma (part of the Valles Marineris canyon system). These may explain the pervasive deformation of the layered strata along the north wall of the chasma..

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A future digital terrain model can also help to analyze the fault structure.

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Below is a non-narrated HiClip mini, with added sound effect. (Less than 1 km across.)

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

ID: ESP_063406_1750
date: 5 February 2020
altitude: 263 km

NASA/JPL/UArizona

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