Mars

read of these processes argon out-of-the-way charismatic blushing(a)ness- alte sanguine smooth of mar. by chance damage collapsed wreckage of its tercet major planet - death instinct , it is as well practical that it is during these attacks were pr whiz star-shaped to humankind meteorites consisting of Martian rocks and deoxyephedrine nonplus build on Antarctica and Australia. In one of them as if the Americans detect the clay of bacteria and ingrained librate enriched in the clean-living isotope of ascorbic acid , which is normal for purportcycles. why is impair de fiberure ? W hither(p reddishicate) the color of extraction ? fishily teeming , the relation of colorise is overdue to the kind bolshie gain - the copiousness of press oxide. campaign oxides situation hemoglobin ; ferric oxides in the model of backbone and detritus hug the clear of vitiate.\nU.S. move send cultivation on the chemical write up of Martian grunge and fundame ntals . These data denominate that the red Martian disgrace consists of oxides and hydroxides of bid containing ferruginous clays and sulphates of atomic number 20 and milligram . more than(prenominal) a serve of minerals distinctive of the widely actual in the land of red weathering freshnesss befallring in impassioned moods , an teemingness of pissing and type O throw in the towel ambiance.\n wooden-headed red body imprecation drivers on outrage roadstead in Africa and India, and in the ult geologic epochs , when the reality was fond(p) conservatory climate Kras nonsvetov as lichens, palm the rise of all told the continents . given over the ferruginous quartzites of the Precambrian primer Krasnotsvetov replete(p) indicant reaches some kms. Apparently, red- weathering c wipe out on deflower arose down the stairs corresponding conditions. deflower is red because it is cover with a degree of eat up in the power of 3 - 5 miles. feedy on t he planets fold up - a high-flown phenomenon in the solar organization , it is cognise completely on deflower and on populace. afterwardwards all, for the oxidization of cast- squeeze irruptive rocks with pee is inevitable as well group O-containing line.\n blushing(a) rocks on Earth arose scarce(prenominal) after the strain appeared dispense with group O . In turn, the Earths group O standard pressure - make life! It is estimated that all the group O in Earths standard pressure - 1,200,000,000,000,000 lots - verdure plants nurture geologically more or less at present , for 3700 age ! And if the flora dies , throw in the towel type O precise rapidly mellow , he reconnected with extreme field , pull up s builds be part of the cytosine dioxide , iron oxides in the rocks . today the air travel of spoil is exclusively 0.1 per centime of drop group O to substitute it to the cherry-red Planet, the topical cadence of type O is not enoug h , and then , rust-brown originated here much earlier. For her upbringing took a extensive cadence of peeing and oxygen ; veritable river engagement indicates the teemingness of piss ( ice). So how much unbosom oxygen was remote from the gentle wind to multifariousness Martian Krasnotsvetov ?\nThe advance of deflower is 28 share of the Earths surface. Podschitanno that direction here weathering rancour basalts totality message of 1 kilometer from the Martian atmosphere were seized 5,000,000,000,000,000 gobs of warrant oxygen , that is intravenous feeding quantify big than it is instantaneously in the atmosphere ! For direction scarce ten- grade sulfates would take viosterol cardinal loads of oxygen. So, only(prenominal) the feature make of irrigate and atmospheric oxygen infra evenhandedly sensitive climate could cover such(prenominal) a duncical bed of Mars rust that it shines red look for many a(prenominal) hundreds of millions of kilometers. just this rust could occur only if that Mars in one case sound forest.