Evolution of geographic shell

As a result of thermochemical responses that line in the field of view of ​​the outer core out of the ground form metals, their oxides, volatile affair and water. Light diffuse change reaction products under touch on scar jam - perysfery. Because of the lower thermal conductivity of the last mentioned are non immediately introduce through the rise up of the artificial satellite, but accumulated under the mend perysfery form the second base warm-up muster area of ​​the upper cape - astheno region. Periodic pink slip of excess asthenosphere magma square volatile and heat as a result of volcanic activity commence with by the validation therein rozuschilnenoho space. jewel cladding perysfery pursuit the declining volume, passively subsiding on these areas, fashioning negative landforms on Earth. The area where this subsidence does not, stored as rest period hills. This is confirmed by restriction trappovyh provinces continents to syneklyzam platforms, Manuals huge outpourings of plateau basalts shaping of ocean basins in the Cenozoic. The decrease in the Earth by sealing protoveschestva, dyssypatsiyi heat content and other gases and products of the disassociation of water is go with by a decrease in the rung of the planet and its surface area. In other words, the reduction of surface compressive sphere is not achieved spherical compression plykatyvnym its stone shell as expected Elie de Beaumont and E. Suess come out of the prototypic models of fiery bland earth, and sinking at different levels of its someone units. And this is the main dispute between chilly contraction from the unmixed contraction Suess but its assumptions. \nReducing the Earths surface due to the reduction of the volume and the progressive tense reduction of the radius leads to increased stemma and depth of primitiveness solid perysfery. Thus, the order of magnitude of the amplitude of the fireman of the planet is st raight proportionate to its grow and internal activity and inversely proportional to the exogenous factors characterizing the specialty of the destruction of the relief, which ultimately determined by the presence or absence of exhaust water on the surface of the planet. naval basins and continental blocks - the highest kindly contraction form during compression of the global sphere, which the stone cladding - perysfera, subsidence oer rozuschilnenymy spaces asthenosphere passively adapts to the volume, which reduces the balls. Depressions and hills in spite of appearance these major heotekstur concordant compression of high order in the later stages of the Earth during its contraction.