scientist have know for a while that Mars ’ contestation vary wildly over ten of thousands of geezerhood , going from being perfectly perpendicular to having ice buildups at the equator . New inquiry has identify that these occasional change have left a tincture . They found that ancient   ice cap have not disappeared completely but are still there , buried in layers beneath the North Pole .

The new findings are reported in the journalGeophysical Research Lettersand detail the so - called cavi unit , a deposit of ice and sand forecast to be one C of millions of years old . The ice was engineer in slab with sand , although in certain surface area it was 90 percent water by volume . If meld , it would be like having a 1.5 - time ( 5 - substructure ) layer of water around the Red Planet .

“ We did n’t expect to observe this much weewee ice here , ” lead author Stefano Nerozzi , a postgraduate research assistant at the University of Texas Institute for Geophysics , articulate in astatement . “ That in all likelihood makes it the third largest weewee reservoir on Mars after the polar Methedrine caps . ”

The breakthrough was possible thanks to the purpose of the Shallow Radar instrument onboard NASA ’s Mars Reconnaissance Orbiter . It was also independently verified bygravity dataof the region , which supports the presence of a immense secret deposition of ice-skating rink .

The observance might provide a more elaborate timeline of Martian glaciation . There are suggestions that despite abundant liquid water , Mars was never a “ tropic ” Eden and life-time might have found it hard to evolve in aperennially frigidplanet .

“ Understanding how much urine was available globally versus what ’s trammel in the perch is authoritative if you ’re going to have liquid water on Mars , ” Nerozzi said . “ you’re able to have all the right conditions for life , but if most of the water is put away up at the poles , then it becomes difficult to have sufficient amount of fluid water near the equator . ”

The North Pole hugger-mugger sediment is clearly an crucial reservoir of water for Mars . Based on the assessment , its mass is tantamount to the combined underground ice rink deposit retrieve in all the other small latitudes on the Red Planet .