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Sol de Mars seen by the Phoenix probe - Mars: Phoenix landing site - Image...

Sol de Mars seen by the Phoenix probe - Mars: Phoenix landing site - Image obtained by the Phoenix probe short
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Largest available format 1213 × 2933 px 1 MB
Dimension [pixels] Dimension in 300dpi [mm] File size [MB] Online Purchase
Large 1213 × 2933 px 103 × 248 mm 809 KB
Medium 424 × 1024 px 36 × 87 mm 553 KB

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PIX4616602
Image title
Sol de Mars seen by the Phoenix probe - Mars: Phoenix landing site - Image obtained by the Phoenix probe shortly after its successful landing on the Mars surface on May 25, 2008. The probe landed on a vast plain north of the planet in the Vastitas Borealis region. This image, one of the first captured by Nasa's Phoenix Mars Lander, shows the vast plains of the northern polar region of Mars. The flat landscape is strewn with tiny pebbles and shows polygonal cracking, a pattern seen widely in Martian high latitudes and also observed in permafrost terrains on Earth. The polygonal cracking is believed to have resulted from seasonal freezing and thawing of surface ice. Phoenix touched down on the Red Planet at 4:53 p.m. Pacific Time (7:53 p.m. Eastern Time), May 25, 2008, in an arctic region called Vastitas Borealis, at 68 degrees north latitude, 234 degrees east longitude. This is an approximate - color image taken shortly after landing by the spacecraft's Surface Stereo Imager, inferred from two color filters, a violet, 450 - nanometer filter and an infrared, 750 - nanometer filter
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Sol de Mars seen by the Phoenix probe - Mars: Phoenix landing site - Image obtained by the Phoenix probe shortly after its successful landing on the Mars surface on May 25, 2008. The probe landed on a vast plain north of the planet in the Vastitas Borealis region. This image, one of the first captured by Nasa's Phoenix Mars Lander, shows the vast plains of the northern polar region of Mars. The flat landscape is strewn with tiny pebbles and shows polygonal cracking, a pattern seen widely in Martian high latitudes and also observed in permafrost terrains on Earth. The polygonal cracking is believed to have resulted from seasonal freezing and thawing of surface ice. Phoenix touched down on the Red Planet at 4:53 p.m. Pacific Time (7:53 p.m. Eastern Time), May 25, 2008, in an arctic region called Vastitas Borealis, at 68 degrees north latitude, 234 degrees east longitude. This is an approximate - color image taken shortly after landing by the spacecraft's Surface Stereo Imager, inferred from two color filters, a violet, 450 - nanometer filter and an infrared, 750 - nanometer filter

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Photo © NASA/JPL-Caltech/University of Arizona/Novapix / Bridgeman Images
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Novapix

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