{ "title": "HiPOD", "metadata": { "thumbnailURL": "bundle://header.jpg", "excerpt": "Tartarus Colles are a group of knobby hills in the northern plains of Mars." }, "version": "1.5", "identifier": "testArticle", "language": "en", "layout": { "columns": 10, "width": 1024, "margin": 85, "gutter": 20 }, "documentStyle": { "backgroundColor": "#F5F9FB" }, "components": [ { "role": "heading1", "layout": "heading1Layout", "text": "HiPOD: THURSDAY, 10 OCTOBER 2019" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#8c2028" } }, { "role": "title", "layout": "halfMarginBelowLayout", "text": "A Mesa in the Tartarus Colles Region" }, { "role": "photo", "layout": "fullBleedLayout", "caption": "A mesa in the Tartarus Colles region of Mars. (NASA/JPL/University of Arizona)", "URL": "bundle://ESP_055234_1910-main.jpg" }, { "role": "caption", "layout": "halfMarginBothLayout", "text": "Less than 5 km across, 278 km above the surface. (NASA/JPL/University of Arizona)" }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "

The objective of this observation is to examine layers around a mesa. Some layers are thin; others much thicker.

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Tartarus Colles are a group of knobby hills in the northern plains of Mars. Their formation might be the result of interactions between lava and water to form what are often called “rootless cones.”

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NASA/JPL/University of Arizona
ID: ESP_055234_1910

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