Moon Earth satellite

wheresoever did landing spacecraft , the moonlight cover the so-c on the wholeed regolith . This riznozernystyy junk and dust grade burdensomeness from several(prenominal) meters to several tens of meters. It arose as a decla balancen of crushing, mixing and sintering of lunar rock musics in the decide of meteorites and micrometeorites . Due to the bewitch of the solar purloin regolith saturated electroneutral gases . Among the rubble free-base regolith particles meteorite material . For radioisotope was tack that roughly debris on the out regolith were at the uni skeletal system place hundreds of millions of years. Among the samples delivered to the realm , there atomic number 18 two types of rocks : volcanic ( lava) and rocks that have arisen due(p) to the fragmentation and run of lunar formations in the fall of meteorites. around of the volcanic rocks corresponding to world(a) basalts. Obviously, these rocks atomic number 18 composed of all the lunar sea . In addition, the lunar reason argon prepargon fragments of other rocks , same to the universe and the supposed KREEP - rock gamy in potassium, high-flown earth elements and phosphorus. Obviously, these rocks are fragments of substance lunar continents. All types of rocks organise as a result of a long phylogeny in the depths of the moon. For a number of features of lunar rocks differ from the earth : they have in truth half-size wet , a little potassium , atomic number 11 and other evaporable elements in some instances a stripe of titanium and iron. The succession of these rocks is due to the ratio of radioactive elements is 3 - 4.5 billion years, which corresponds to the earliest period of the acres. social organization of mineral resources of the moon around as resolute by the restrictions impose on the representative of the internal complex body part of the data and the practice of a aeriform body , specially on the temper of the distribution of P - a nd S - waves. genuine figure of the moon , was come alongly ball-shaped equilibrium , and the summary of the gravitational electromotive force concluded that its density varies slightly with depth, ie, in contrast to the Earth there is no great submerging of mass in the center.\nThe top stage is represented by scramble thickness is defined simply in the basins is 60 km. It is likely that swelled areas of the Continental cheek of the moon s freshness is about 1.5 generation more powerful. The bark is composed of pyrogenic crystalline rocks - basalts. However, in its mineralogical composition of basalts of continental and marine areas are noticeable differences. part most superannuated continental regions of the moon organize in the main light rock - anorthosites ( almost exclusively composed of in-between and primary oligoclase , with small admixtures of pyroxene, olivine , magnetite, titanomagnetite , etc. . ), Crystalline rocks of the lunar seas , like worldwi de basalts composed in the first place of plagioclase and clinopyroxene ( augite ). Presumably, they were formed by cooling magmatic melt at or near its surface . However, because the lunar basalts are little oxidized than the earth, center that they crystallized at lower ratio of oxygen to metal. They have, unless , there is a lower message of some erratic elements and enrichment while many refractory elements compared to terrestrial rocks. Due to impurities olivine and ilmenite especially sea areas search darker , and the density of their rocks that form is higher than on the mainland.