Scroll right and journey [ http://pdsmaps.wr.u ] for 300 kilometers over Terra Sirenum [ http://www-pdsimage mapmkr.htm ] in the cratered [ http://clasdean.la. ] highlands of southern Mars [ http://www.uapress. contents.htm ]. The infrared view [ http://photojournal PIAGenCatalogPage.pl ?PIA03483 ], 32 kilometers wide, was recently recorded by the THEMIS [ http://themis.asu.e ] camera on board the orbiting Mars Odyssey [ http://mars.jpl.nas odyssey.html ] spacecraft. Beginning [ http://themis.asu.e ] at the north (left) edge, the scene sweeps across the floor and over the rim of Koval'sky Crater. Continuing [ http://themis.asu.e ] southward [ http://themis.asu.e ] (right) of the crater's rim are lava flows [ http://volcano.und. Overview.html ] exhibiting fractures and numerous smaller impact craters. The infrared [ http://sirtf.caltec gallery.html ] image was made in daylight hours, so sun-facing slopes are still warm and bright while shadowed areas are cool and dark. But rocky [ http://antwrp.gsfc. ] regions also tend to remain cooler [ http://sirtf.caltec zoo.html ] and darker than their surroundings, likely corresponding to the dark blotchy terrain along the Koval'sky Crater floor and dark rings of rocky ejecta surrounding some of the smaller craters [ http://wwwflag.wr.u marscrat.html ].
Explanation
Scroll right and journey [ http://pdsmaps.wr.u ] for 300 kilometers over Terra Sirenum [ http://www-pdsimage mapmkr.htm ] in the cratered [ http://clasdean.la. ] highlands of southern Mars [ http://www.uapress. contents.htm ]. The infrared view [ http://photojournal PIAGenCatalogPage.pl ?PIA03483 ], 32 kilometers wide, was recently recorded by the THEMIS [ http://themis.asu.e ] camera on board the orbiting Mars Odyssey [ http://mars.jpl.nas odyssey.html ] spacecraft. Beginning [ http://themis.asu.e ] at the north (left) edge, the scene sweeps across the floor and over the rim of Koval'sky Crater. Continuing [ http://themis.asu.e ] southward [ http://themis.asu.e ] (right) of the crater's rim are lava flows [ http://volcano.und. Overview.html ] exhibiting fractures and numerous smaller impact craters. The infrared [ http://sirtf.caltec gallery.html ] image was made in daylight hours, so sun-facing slopes are still warm and bright while shadowed areas are cool and dark. But rocky [ http://antwrp.gsfc. ] regions also tend to remain cooler [ http://sirtf.caltec zoo.html ] and darker than their surroundings, likely corresponding to the dark blotchy terrain along the Koval'sky Crater floor and dark rings of rocky ejecta surrounding some of the smaller craters [ http://wwwflag.wr.u marscrat.html ].