Примери коришћења Lithosphere на Енглеском и њихови преводи на Српски
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The Ganymedian ice lithosphere.
The lithosphere beneath passive margins is known as transitional lithosphere.
The role of subduction dynamics on the regional movements of the lithosphere segments.
Continental lithosphere and oceanic lithosphere differ markedly in their thicknesses.
The nature of a convergent boundary depends on the type of lithosphere in the plates that are colliding.
Earth's lithosphere is divided into several rigid tectonic plates that migrate across the surface over many millions of years.
While a weld between oceanic and continental lithosphere is called a passive margin, it is not an inactive margin.
A region's climate is generated by the climate system, which has five components: atmosphere, hydrosphere,cryosphere, lithosphere, and biosphere.
It should be noted that the crust and lithosphere are defined by different properties and do not constitute the same layer.
Familiarization with the formation anddevelopment of the basic spheres of the Earth- lithosphere, atmosphere and hydrosphere;
The strength of the lithosphere is derived from its temperature;thick lithosphere exists because the outer part of the Earth is relatively cold.
The noosphere is therefore as much part of nature as the barysphere, lithosphere, hydrosphere, atmosphere, and biosphere.
Classification of lithosphere plates, causes and direction of their movement, possible relationships between plates(collision, subduction…) as the cause of endodynamic processes and creation of relief.
The Earth's climate system illustrates the whole planetary system of interaction between lithosphere, hydrosphere, biosphere and atmosphere.
Because it contains thick continental crust, this lithosphere is less dense than the underlying asthenospheric mantle and normal subduction is disrupted.
Here, exceedingly large convective cells bring very large quantities of hot asthenospheric material near the surface andthe kinetic energy is thought to be sufficient to break apart the lithosphere.
This refers to whether a crustal boundary between oceanic lithosphere and continental lithosphere is a plate boundary or not.
Cool oceanic lithosphere is significantly denser than the hot mantle material from which it is derived and so with increasing thickness it gradually subsides into the mantle to compensate the greater load.
The division of the outer parts of the Earth's interior into lithosphere and asthenosphere is based on mechanical differences and in the ways that heat is transferred.
Time line of events as following: the eruption of energy from the sun in the form of charged particles contained in the electrical IMF, that is SW,magnetization of environment(some parts of the lithosphere) and the occurrence of earthquake.
Continents are also defined due to its placement andthat they sit on continental lithosphere which is part of tectonic plates floating high on Earth's molten mantle.
Cold, thick, and therefore strong lithosphere can support higher mountain ranges than can thin lithosphere, just as thick ice on a lake or river is better able to support larger people than thin ice.
It mainly focuses researchers on tectonic deformation of rocks, rock stratum androck mass in the lithosphere, including geometry, kinematics, and dynamics of structural deformation.
Coal-seam fires have been slowly shaping the lithosphere and changing atmosphere, but this pace has become fast and extensive at modern times, triggered by enormous mining activities.[5].
The element occurs within a number of mineral deposits, principally rutile and ilmenite,which are widely distributed in the Earth's crust and lithosphere, and it is found in almost all living things, water bodies, rocks, and soils.
Cold, thick, and due to this fact strong lithosphere can support greater mountain ranges than can thin lithosphere, just as thick ice on a lake or river is better able to support bigger people than thin ice.
The concept was based on the presence of significant gravity anomalies over continental crust, from which he inferred that theremust exist a strong, solid upper layer(which he called the lithosphere) above a weaker layer which could flow(which he called the asthenosphere).
This was caused by a sudden shift of the earth's entire lithosphere, he theorized, simultaneously moving all of the continents into their present position, a much different view than the widely accepted explanation offered the plate tectonics theory.
Landscape may be viewed as a precondition for the type of influence of all the other natural components in space, and as such it influences the qualitative characteristic of surface andsurfacing part of lithosphere, climate conditions, soil, vegetation, the quotient of outflow etc.
Divergent boundaries are typified in oceanic lithosphere by the rifts of the oceanic ridge system, including the Mid-Atlantic Ridge and, in continentental lithosphere by rift valleys such as the famous East-African Rift.