{ "title": "Light-Toned and Possible Hydrated Materials in a Gullied Crater", "authors": "HiRISE", "metadata": { "thumbnailURL": "https://static.uahirise.org/anews/2020-09-21/ESP_025472_1405.jpg", "excerpt": "This observation shows a gullied crater in the southern mid-latitudes with light-toned deposits near the center of its floor." }, "version": "1.5", "identifier": "ESP_025472_1405", "language": "en", "layout": { "columns": 10, "width": 1024, "margin": 85, "gutter": 20 }, "documentStyle": { "backgroundColor": "#faf7f2" }, "components": [ { "role": "heading1", "layout": "heading1Layout", "text": "HiPOD: 21 September 2020" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#8c2028" } }, { "role": "title", "layout": "halfMarginBelowLayout", "text": "Light-Toned and Possible Hydrated Materials in a Gullied Crater" }, { "role": "photo", "layout": "fullBleedLayout", "caption": "An enhanced color cutout showing detail of the bedrock and dune crests. The blueish sand likely is basaltic in nature. Less than 1 km across. (NASA/JPL/UArizona)", "URL": "https://static.uahirise.org/anews/2020-09-21/ESP_025472_1405.jpg" }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "
This observation shows a gullied crater in the southern mid-latitudes with light-toned deposits near the center of its floor, and two areas of collapsed terrain at the northern and southern edges of the crater floor.
Data from the CRISM instrument—also onboard the Mars Reconnaissance Orbiter—tentatively show a minerals containing chemically-bound water in the “chaotic” areas.
ID: ESP_025472_1405
date: 02 January 2012
altitude: 253 km
NASA/JPL/UArizona