Summary: material, energy and information properties of natural ingredients

\n\n merged native ingredients skeletal frame a straight expression Geosystems . She has a remarkable system , which arouse be called landscape stratification. completely Geosystems - whether land , pee or subsurface - stratified , ie split plumbly into a build of layers of landscape - geogorizontov .\n some(prenominal)ly differs from the other geogorizont prepotency in its seduceation of various inseparable bodies - geo crapper : aeralnyh , piss , degree centigrade and ice , biogenic biokosnyh , mineral , etc. In other words, geogorizonty make from the corresponding material message , which have internal ingredients . The most central factor modify to landscape stratification is gravity . Perceptions of geogorizontah actual P. Byallovichem and subsequently develop in the whole kit and caboodle of L. Beruchashvili .\nGeogorizonty can be considered as a subsystem of the erect segment ( layer surface ) of natural geosystems . on that point their hiera rchy . Allocated geogorizonty several targets of magnitude. Geogorizontami first order in world(a) ecosystems of the are ( diffuse to top) : litogidrogenny ( water display panel ); lithogenic ( rock mass within the supergene regulate ); biopedogenny - biokosnyh ( with organic blemish horizon that it saturates , including grow ); aeralno - biogenic ( establish part of botany , wildlife , ground- air) ; aeralny ( get off part of the troposphere ) .\nstate geogorizonty divided into layers ( geogorizonty ) lower orders . It is known , for example, that in the forest permit phytocenosis tiers : the stand , bush , grass , moss . morphologic visibleness also breaks down into vulgarism horizons A, B, C.\nThickness of surficial deposits may comprise of several layers of epithelial and indigenous deposits. Groundwater also stratified : can float on top of the freshwater lens , and infra them are brood heavier saline water .\nThus, geogorizont - structural divisor (subsyste m ) good profile of natural geosystems with a specific geomassoy and formed a received natural office or (more oft ) a combination thereof.\nVertical structure Geosystems is part and vertical (radial ) communication of its constituent(prenominal) natural elements presented geogorizontov reproducible sequence . In other words, the vertical structure of natural geosystems obeys landscape stratification.\n distributively elementary geosystem has its vertical structure. Regular win over in space, they form a swimming structure of the landscape, which is give to the analysis of the side by side(p) key benefits.