{ "title": "Protonilus Mensae Glaciation", "authors": "HiRISE", "metadata": { "thumbnailURL": "https://static.uahirise.org/anews/2021-04-15/ESP_068044_2240.jpg", "excerpt": "During periods in Mars’ history when the planet had greater axial tilt, shifts in atmospheric circulation may have favored the extensive accumulation of snow in some locations." }, "version": "1.5", "identifier": "ESP_068044_2240", "language": "en", "layout": { "columns": 10, "width": 1024, "margin": 85, "gutter": 20 }, "documentStyle": { "backgroundColor": "#faf7f2" }, "components": [ { "role": "heading1", "layout": "heading1Layout", "text": "HiPOD: 15 April 2021" }, { "role": "divider", "layout": "bigDividerLayout", "stroke": { "width": 3, "color": "#8c2028" } }, { "role": "title", "layout": "halfMarginBelowLayout", "text": "Protonilus Mensae Glaciation" }, { "role": "embedwebvideo", "aspectRatio": 1.777, "URL": "https://youtu.be/yCa9WYCzJcc", "caption": "HiClip: Protonilus Mensae Glaciation", "accessibilityCaption": "Narration by Tre Gibbs." }, { "role": "body", "format": "html", "layout": "hipodMarginLayout", "text": "


During periods in Mars’ history when the planet had greater axial tilt, shifts in atmospheric circulation may have favored the extensive accumulation of snow in some locations. Protonilus Mensae is just such a site of extensive glaciation. (Narration: Tre Gibbs)

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ID: ESP_068044_2240
date: 4 December 2020
altitude: 251 km (156 mi)

NASA/JPL/UArizona

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