{"id":777991,"date":"2024-02-28T06:03:51","date_gmt":"2024-02-28T11:03:51","guid":{"rendered":"http:\/\/spaceweekly.com\/?p=777991"},"modified":"2024-02-28T06:03:51","modified_gmt":"2024-02-28T11:03:51","slug":"sand-dunes-meet-stacked-ice-at-marss-north-pole-2","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=777991","title":{"rendered":"Sand dunes meet stacked ice at Mars\u2019s north pole"},"content":{"rendered":"<p> <br \/>\n<\/p>\n<div id=\"\">\n<header class=\"entry article__block\">\n\t<span class=\"pillar article__item\">Science &amp; Exploration<\/span><\/p>\n<p>\t\t\t\t\t\t<span>28\/02\/2024<\/span><br \/>\n\t\t\t\t<span><span id=\"viewcount\">124<\/span><small> views<\/small><\/span><br \/>\n\t\t\t\t\t\t\t\t\t\t<span><span id=\"ezsr_total_25959986\">3<\/span><small> likes<\/small><\/span><\/p>\n<\/header>\n<div class=\"abstract article__block article__item\">\n<p>ESA\u2019s Mars Express has captured an intriguing view near Mars\u2019s north pole, imaging where vast sand dunes meet the many layers of dusty ice covering the planet\u2019s pole.<\/p>\n<\/div>\n<div class=\"article__block\">\n<p>The terrain surrounding Mars\u2019s north pole, known as Planum Boreum, is fascinating. The pole itself is covered in layers and layers of fine dust and water ice; these stack several kilometres thick and stretch out for around 1000 km (approximately the width of France).<\/p>\n<p>While most of this material is not visible here, you can see the beginnings of Planum Boreum to the right of the frame, with some subtle wrinkling showing where layers of material are starting to build up. Ground has also built up more starkly in steps, as is most clearly visible in the topographic view of this region below. The lowest altitude regions are blue\/green and the highest are red\/white\/brown.<\/p>\n<\/p><\/div>\n<p>\t\t\t\t\t\t<!-- Topography_of_Mars_s_north_polar_region_article.tif  discarded 578452 --><\/p>\n<div class=\"article__block\">\n<figure class=\"article__image article__image--large\"><figcaption class=\"image__caption\">\n\t\t\t\t\t\t\tTopography of Mars\u2019s north polar region<br \/>\n\t\t\t\t\t\t\t\t<\/figcaption><\/figure>\n<p>These layers formed as a mix of dust, water ice and frost settled on the martian ground over time. Each layer holds valuable information about Mars\u2019s history, telling the story of how the planet\u2019s climate has changed over the past few million years.<\/p>\n<p>In martian winter, the layers are topped by a thin cap of dry ice (carbon dioxide ice) a couple of metres thick. This cap completely disappears to the atmosphere each martian summer.<\/p>\n<p>This image comes from the Mars Express High Resolution Stereo Camera (HRSC). Two steep banks, or escarpments, cut vertically through the frame. These mark the boundary between the aforementioned layered deposits (which stretch out of frame towards the pole, right) and the vast, sweeping dune fields covering the lower terrain of Olympia Planum (to the left).<\/p>\n<p>Click on the image below to explore the region and discover more about the different features you can see.<\/p>\n<\/p><\/div>\n<div class=\"article__block\">\n<figure class=\"article__image article__image--large\"><figcaption class=\"image__caption\">\n\t\t\t\t\t\t\tSand dunes meet stacked ice at Mars\u2019s north pole<br \/>\n\t\t\t\t\t\t\t\t<\/figcaption><\/figure>\n<\/p><\/div>\n<p><h2 class=\"heading\">Walls of ice<\/h2>\n<\/p>\n<div class=\"article__block\">\n<figure class=\"article__image article__image--left\"><figcaption class=\"image__caption\">\n\t\t\t\t\t\t\tPerspective view of Mars\u2019s north polar region<br \/>\n\t\t\t\t\t\t\t\t<\/figcaption><\/figure>\n<p>The left part of this image is dominated by a vast, elongated swathe of rippled sand dunes, stretching out for more than 150 km within this frame alone. This wrinkled, turbulent appearance is highly at odds with the smooth and more pristine terrain visible to the right.<\/p>\n<p>This smooth region lacks clear signs of erosion and has avoided being hit by incoming rocks from space \u2013 an indicator that the surface is very young, likely rejuvenating every year.<\/p>\n<p>Between these two extremes sit two semicircular cliffs, the larger of which is around 20 km wide. Within the curves of these cliffs sit frost-covered sand dunes. The grand scale of the cliffs is clear from the dark shadows they cast on the surface below \u2013 their steep, icy walls tower up to a kilometre high.<\/p>\n<\/p><\/div>\n<div class=\"article__block\">\n<figure class=\"article__image article__image--right\"><figcaption class=\"image__caption\">\n\t\t\t\t\t\t\tA broader view: Olympia Planum and Planum Boreum<br \/>\n\t\t\t\t\t\t\t\t<\/figcaption><\/figure>\n<p>These two cliffs are located at a so-called polar trough, a feature created as wind pushes into and wears away the surface. These show up as rippled ridges in the terrain and are common in this region, creating the distinctive spiral-like pattern of the polar plateau (seen most clearly in the wider context view of this region below, and in\u00a0other images of Planum Boreum from Mars Express).<\/p>\n<\/p><\/div>\n<div class=\"article__block\">\n<h2 class=\"heading\">Exploring Mars<\/h2>\n<p>Mars Express has been orbiting the Red Planet since 2003. It is imaging Mars\u2019s surface, mapping its minerals, identifying the composition and circulation of its tenuous atmosphere, probing beneath its crust, and exploring how various phenomena interact in the martian environment.<\/p>\n<p>The spacecraft\u2019s HRSC, responsible for these images, has revealed much about Mars\u2019s diverse surface in the past 20 years. Its images show everything from\u00a0wind-sculpted ridges and grooves\u00a0to\u00a0sinkholes on the flanks of colossal volcanoes\u00a0to\u00a0impact craters, tectonic faults, river channels and ancient lava pools. The mission has been immensely productive over its lifetime, creating a far fuller and more accurate understanding of our planetary neighbour than ever before.<\/p>\n<\/p><\/div>\n<div class=\"article__block\">\n<figure class=\"article__image article__image--large\"><figcaption class=\"image__caption\">\n\t\t\t\t\t\t\tMars\u2019s north polar region in 3D<br \/>\n\t\t\t\t\t\t\t\t<\/figcaption><\/figure>\n<p><i>The Mars Express High Resolution Stereo Camera\u00a0(HRSC) was developed and is operated by the German Aerospace Center (Deutsches Zentrum f\u00fc<\/i><i>r Luft- und Raumfahrt; DLR).<\/i><\/p>\n<\/p><\/div>\n<div class=\"share button-group article__block article__item\">\n<p><button id=\"ezsr_25959986_2_5\" class=\"btn ezsr-star-rating-enabled\" title=\"Like\">Like<\/button><\/p>\n<p id=\"ezsr_just_rated_25959986\" class=\"ezsr-just-rated hide\">Thank you for liking<\/p>\n<p id=\"ezsr_has_rated_25959986\" class=\"ezsr-has-rated hide\">You have already liked this page, you can only like it once!<\/p>\n<\/div>\n<\/div>\n<p><br \/>\n<br \/><a href=\"https:\/\/www.esa.int\/Science_Exploration\/Space_Science\/Mars_Express\/Sand_dunes_meet_stacked_ice_at_Mars_s_north_pole?rand=771654\">Source link <\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Science &amp; Exploration 28\/02\/2024 124 views 3 likes ESA\u2019s Mars Express has captured an intriguing view near Mars\u2019s north pole, imaging where vast sand dunes meet the many layers of&hellip; <\/p>\n","protected":false},"author":1,"featured_media":777990,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[5],"tags":[],"class_list":["post-777991","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-ESA"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/777991","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=777991"}],"version-history":[{"count":0,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/777991\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/777990"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=777991"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=777991"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=777991"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}