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In the EDM of today's APOD, countless bright, zig-zagging and whitish lanes of Carbon Dioxide (CO2) Frost (or, simply, Dry Ice) highlight an extremely intricated Network of Channels carved into the Surface of the South Polar Region of Mars. These Channels, however, are eroded a little bit more at every Martian Spring, when the Seasonal Polar Ice Cap, which at the South Pole of Mars is mostly composed of Dry Ice, sublimates (meaning that it goes directly from a solid state to a gaseus state) at the Ice-Surface Interface. The erosion occurs under the seasonal Ice Layer and, when a trapped (and pressurized) Gas Pocket finds an escape route, then it carries along some loose Surface Material. Once the Gas makes it to the open and gets dispersed, the loose Surface Material is then blown away in a downwind direction and, finally, falls down in Dark Fans on top of the Seasonal Ice Layer (see the CTX Frame and the EDM). Mars Local Time: 17:27 (Middle Afternoon) These pictures (which are a NASA - Original Mars Reconnaissance Orbiter CTX b/w frame identified by the serial n. ESP_029545_0950-RED_NOMAP_browse and a NASA - Original Mars Reconnaissance Orbiter EDM false-color frame identified by the serial n. ESP_029545_0950) have been additionally processed and then colorized (and re-colorized, respectively) in Absolute Natural Colors (such as the colors that a human eye would actually perceive if someone were onboard the NASA - Mars Reconnaissance Orbiter and then looked down, towards the Surface of Mars), by using an original technique created - and, in time, dramatically improved - by the Lunar Explorer Italia Team. |