{ "title": "HiPOD", "metadata": { "thumbnailURL": "bundle://header.jpg", "excerpt": "Not all craters are bowl-shaped. In fact, many impact craters have rebounding material creating a central uplift or peak." }, "version": "1.5", "identifier": "PSP_010745_1465", "language": "en", "layout": { "columns": 10, "width": 1024, "margin": 85, "gutter": 20 }, "documentStyle": { "backgroundColor": "#faf7f2" }, "components": [ { "role": "heading1", "layout": "heading1Layout", "text": "HiPOD: TUESDAY, 29 OCTOBER 2019" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#8c2028" } }, { "role": "title", "layout": "halfMarginBelowLayout", "text": "Scenes of an Uplift" }, { "role": "photo", "layout": "fullBleedLayout", "caption": "A black and white image of the central uplift of an impact crater. Less than 5 km across. (NASA/JPL/University of Arizona)", "URL": "bundle://PSP_010745_1465-main.jpg" }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "


Not all impact craters are of the classic bowl-shape variety. Often times, material from the center will rebound and create a peak that can show us some of the rock, possible minerals, and other material that was buried prior to impact.

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The enhanced color images show greater detail of the uplift, including exposed bedrock and delicate sand sheets. The teal-bluish sand likely represents basaltic (volcanic) material that might have been blown-in from elsewhere.

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NASA/JPL/University of Arizona

ID: PSP_010745_1465
date: 10 November 2008
altitude: 253 km

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