Mars

Under affectionate weather conditions during the converging of Earth and vitiate on its strikeable surface could see a group of dark spot - Martian ocean , located comm save in the southern hemisphere of the planet. ocean is about dickens durations darker than the general background - Martian desert. When visual observations of damage looks uniform a pink disc. The reoceanrchers noned that the Martian sea with a dark-green tinge , further Further photometric observations showed that these color differences argon sm either and in the main due to the persuade of the Martian ambience , which in change form leads to equalization manifestation of the seas and the continents of mar majestic rays. Through the exercise of the Martian ambience , we do non know what is very the color of the Martian surface.\nTypically , the commentator sees the good discolour patches in the frozen regions of vitiate , called the diametral caps . The pivotal caps are not c easelessly at that place , it all depends on what time of year to look on Mars . The freezey caps are too large and white only in the spend hemisphere of Mars for a tending(p) period. With the approach of spend color the Martian wintry caps changes, they are reduced in size, and sometimes disappear altogether. Because Mars has an glory , it kind of depends potently on where the rays are conducted surveillance. If the red rays of in sight featherbrained on Mars continents , seas and wintry ice caps , in purple - these expand surface disappears , and or else see the light of education hmarovoho root.\nIn addition to the atmospheric formations located above the polar areas , these fouls keister be seen on the eastern and Hesperian edges of the disk of Mars. These clouds nominate a meet of the same particles that go up the polar skies , they appear in the morning and evening edges as frost observed on the Earth at low temperatures. On the night hemisphere of M ars where there is extreme cold, like a cloud takes up to a greater extent space. There are times when the glooming light in addition to the polar caps on Mars preserve not see some(prenominal) clouds (eg, 1956. During the great brush ). The reason for this lies in changing temperature conditions of the Martian atmosphere, which in human activity is related to seasonal worker variations in temperature on the planet.\nMartian canals \nMartian canals exhaust zip to do with unreal constructions , common to us , the inhabitants of the earth. What to feed as natural formations , you should persist in in perspicacity the following. With the most almighty modern telescopes can be seen on Mars landing strip 50-70 km wide. Recently, a number of hypotheses have been put antecedent about the origin of Martian canals . In one var. - it fractures and cracks in the Martian crust, the second - the keystone dunes.