Examples of using Lithosphere in English and their translations into Italian
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Colloquial
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Ecclesiastic
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Ecclesiastic
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Computer
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Official/political
F are as follows: R- structures that produce lithosphere symmetrically and perpendicular to the relative velocity of the plates on either side this does not always apply, for example in the Gulf of Aden.
A mass of unusually hot rock rose from the lower mantle to the base of the lithosphere, fueling a dramatic increase in seafloor spreading rates;
especially in oceanic areas, the lithosphere is pushed upwards
solid lithosphere made up of the uppermost part of the mantle and the crust.
downward warping of the lithosphere due to the weight of the volcano.
over 100 km(62 mi) in a few decades beneath both oceanic and continental lithosphere.
lead-lead isotope geochemistry have revealed that the source of lamproites may be transition zone melts of subducted lithosphere which has become trapped at the base of the lithospheric mantle.
exchange of energy with the hydrosphere, the lithosphere and the biosphere.
As a result, oceanic lithosphere is much younger than continental lithosphere:
is an old and stable part of the lithosphere, the term"metacraton" is used to describe a craton that has been remobilized during an orogenic event,
accrete to adjacent lithosphere, eventually welding to it
than 6 months and attain minimum depths of well over in a few decades beneath both oceanic and continental lithosphere.
is denser than continental lithosphere, for which the mantle is associated with crust made of felsic rocks.
thinning of the crust and lithosphere by plate movement.
The resulting highland eroded over time, and when North American plate motion moved the valley away from the hotspot the resulting thinned lithosphere subsided forming a trough.
Foreland basins form because the immense mass created by crustal thickening associated with the evolution of a mountain belt causes the lithosphere to bend, by a process known as lithospheric flexure.
includes the outer portion of the lithosphere(soil and part of the subsoil),
Oceanic lithosphere is typically about 50-140 km thick(but beneath the mid-ocean ridges is no thicker than the crust),
D.G.& Stephenson, R.A.(eds.): European Lithosphere Dynamics, Geological Society of London Memoirs 32, pp. 83-95.
The flow of heat is greater where the thickness of the lithosphere is less,