{"id":241248,"date":"2016-05-27T04:00:00","date_gmt":"2016-05-27T08:00:00","guid":{"rendered":"http:\/\/spaceweekly.com\/?guid=32e6989918acf5c8c6928531c0c73040"},"modified":"2016-05-27T04:00:00","modified_gmt":"2016-05-27T08:00:00","slug":"chiles-salt-flat","status":"publish","type":"post","link":"https:\/\/spaceweekly.com\/?p=241248","title":{"rendered":"Chile&#8217;s salt flat"},"content":{"rendered":"<p>\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.esa.int\/var\/esa\/storage\/images\/esa_multimedia\/images\/2016\/05\/chile_s_salt_flat\/16006012-1-eng-GB\/Chile_s_salt_flat_small.jpg\" width=\"170\" height=\"96\" align=\"left\" hspace=\"8\" \/><\/p>\n<p>\nThe Sentinel-2A satellite takes us to the diverse landscape of the eastern Atacama desert in South America. The region pictured lies around 200km east of the Chilean city of Antofagasta on the Pacific coast (not pictured), and is virtually devoid of vegetation.\n<\/p>\n<p>\nAt the top of the image we can see part of Chile\u2019s largest salt flat, the Salar de Atacama. With an average elevation of some 2300 m above sea level, it is formed by waters flowing down from the Andes, which, having no drainage outlets, are forced to evaporate, leaving salt deposits.\n<\/p>\n<p>\nIt is the world\u2019s largest and purest active source of lithium, containing some 30% of the world&#8217;s lithium reserve base, and providing almost 30% of the world\u2019s lithium carbonate supply.\n<\/p>\n<p>\nThe bright turquoise rectangles and squares visible along the top part of the image are evaporation ponds. Subsurface salt brines are pumped from beneath the saline crust in two different areas. In one of them, extracted salt brines have unrivalled concentration levels of potassium and lithium. In the other, the brines obtained contain high concentrations of sulphate and boron.\n<\/p>\n<p>\nIn the lower right part of the image we can see the Socompa stratovolcano, known for its \u2018debris avalanche deposit\u2019 where the land collapsed on its western rim some 7000 years ago. The area has since been partially filled by lava, and we can see dark lava flows around the volcano.\n<\/p>\n<p>\nThe multispectral instrument on Sentinel-2 uses parts of the infrared spectrum to analyse mineral composition where vegetation is sporadic. In this false-colour image, the intense shades of brown and orange come from the use of an infrared part of the spectrum leading to an exaggeration of colour intensity.\n<\/p>\n<p>\nThis image \u2013 also featured on the <a href=\"http:\/\/www.esa.int\/spaceinvideos\/Videos\/2016\/05\/Earth_from_Space_Chile_s_salt_flat\">Earth from Space video programme<\/a> \u2013 was captured by Sentinel-2A on 8 March. The satellite is the first in the twin satellite Sentinel-2 mission for Europe\u2019s Copernicus programme, and carries a wide-swath high-resolution multispectral imager with 13 spectral bands, for a new angle on our land and vegetation.<\/p>\n","protected":false},"excerpt":{"rendered":"<p><img loading=\"lazy\" decoding=\"async\" src=\"http:\/\/www.esa.int\/var\/esa\/storage\/images\/esa_multimedia\/images\/2016\/05\/chile_s_salt_flat\/16006012-1-eng-GB\/Chile_s_salt_flat_small.jpg\" width=\"170\" height=\"96\" align=\"left\" hspace=\"8\"><\/p>\n<p>\nThe Sentinel-2A satellite takes us to the diverse landscape of the eastern Atacama desert in South America. The region pictured lies around 200km east of the Chilean city of Antofagasta on the Pacific coast (not pictured), and is virtually devoid of vegetation.\n<\/p>\n<p>\nAt the top of the image we can see part of Chile&rsquo;s largest salt flat, the Salar de Atacama. With an average elevation of some 2300 m above sea level, it is formed by waters flowing down from the Andes, which, having no drainage outlets, are forced to evaporate, leaving salt deposits.\n<\/p>\n<p>\nIt is the world&rsquo;s largest and purest active source of lithium, containing some 30% of the world&#8217;s lithium reserve base, and providing almost 30% of the world&rsquo;s lithium carbonate supply.\n<\/p>\n<p>\nThe bright turquoise rectangles and squares visible along the top part of the image are evaporation ponds. Subsurface salt brines are pumped from beneath the saline crust in two different areas. In one of them, extracted salt brines have unrivalled concentration levels of potassium and lithium. In the other, the brines obtained contain high concentrations of sulphate and boron.\n<\/p>\n<p>\nIn the lower right part of the image we can see the Socompa stratovolcano, known for its &lsquo;debris avalanche deposit&rsquo; where the land collapsed on its western rim some 7000 years ago. The area has since been partially filled by lava, and we can see dark lava flows around the volcano.\n<\/p>\n<p>\nThe multispectral instrument on Sentinel-2 uses parts of the infrared spectrum to analyse mineral composition where vegetation is sporadic. In this false-colour image, the intense shades of brown and orange come from the use of an infrared part of the spectrum leading to an exaggeration of colour intensity.\n<\/p>\n<p>\nThis image &ndash; also featured on the <a href=\"http:\/\/www.esa.int\/spaceinvideos\/Videos\/2016\/05\/Earth_from_Space_Chile_s_salt_flat\">Earth from Space video programme<\/a> &ndash; was captured by Sentinel-2A on 8 March. The satellite is the first in the twin satellite Sentinel-2 mission for Europe&rsquo;s Copernicus programme, and carries a wide-swath high-resolution multispectral imager with 13 spectral bands, for a new angle on our land and vegetation.<\/p>\n","protected":false},"author":5,"featured_media":615444,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[27],"tags":[],"class_list":["post-241248","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-multimedia"],"_links":{"self":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/241248","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\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=241248"}],"version-history":[{"count":1,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/241248\/revisions"}],"predecessor-version":[{"id":241249,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/posts\/241248\/revisions\/241249"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=\/wp\/v2\/media\/615444"}],"wp:attachment":[{"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=241248"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=241248"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/spaceweekly.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=241248"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}