|
A South-facing Escarpment located in the North/Western part of the Martian Region known as Hellas Planitia (a target that was chosen for the research of Phyllosilicates) showed us the presence, inside the Rocks (---> mostly in their horizontal cracks) forming it, of a pale bluish Material, barely visible in this Absolute Natural Color image (in the EDM, to be precise). The CRISM Spectra of such Material showed that it consists of a combination of Chlorite and Water Ice. This image was captured by the NASA - Mars Reconnaissance Orbiter during the Southern Martian Winter, such as in the time period when the Southern Hemisphere's South-facing Escarpments (just like this one) of the Red Planet retain Water Ice Deposits that formed during that dark, long and extremely cold Season. Mars Local Time: 15:36 (Middle Afternoon) These picturees (which are a NASA - Original Mars Reconnaissance Orbiter NON-Map Projected b/w frame and a false color EDM, identified by the serial n. ESP_027758_1530 and ESP_027758_1530-1) have been additionally processed, magnified to aid the visibility of the details, contrast enhanced 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. |