{ "title": "Layered Material Cut by a Valley", "authors": "HiRISE", "metadata": { "thumbnailURL": "https://static.uahirise.org/anews/2020-09-17/ESP_026359_1990.jpg", "excerpt": "This image shows layered bedrock composed of light- and intermediate-toned materials in a valley that is connected to east Jezero Crater." }, "version": "1.5", "identifier": "ESP_026359_1990", "language": "en", "layout": { "columns": 10, "width": 1024, "margin": 85, "gutter": 20 }, "documentStyle": { "backgroundColor": "#faf7f2" }, "components": [ { "role": "heading1", "layout": "heading1Layout", "text": "HiPOD: 17 September 2020" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#8c2028" } }, { "role": "title", "layout": "halfMarginBelowLayout", "text": "Layered Material Cut by a Valley" }, { "role": "photo", "layout": "fullBleedLayout", "caption": "An enhanced color cutout showing details of the dark, basaltic sand and dune crests within the valley. Less than 1 km across. (NASA/JPL/UArizona)", "URL": "https://static.uahirise.org/anews/2020-09-17/ESP_026359_1990.jpg" }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "
This image shows layered bedrock composed of light- and intermediate-toned materials. There are also darker bed forms that fill in low-lying topography, such as impact craters.
In the center of the image is a valley with darker fill extending from left to right. The darker materials within the valley might be fluvial sediments. At HiRISE resolution, we might be able to decipher the properties of the bedrock as well as what deposited the sediments. This valley is actually connected to east Jezero Crater.
ID: ESP_026359_1990
date: 11 March 2012
altitude: 281 km
NASA/JPL/UArizona