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lithosphere
(redirected from Lithospheric)

   Also found in: Encyclopedia, Wikipedia, Hutchinson 0.03 sec.
lith·o·sphere  (lth-sfîr)
n.
The outer part of the earth, consisting of the crust and upper mantle, approximately 100 km (62 mi.) thick.

lithosphere [ˈlɪθəˌsfɪə]
n
(Earth Sciences / Geological Science) the rigid outer layer of the earth, having an average thickness of about 75 km and comprising the earth's crust and the solid part of the mantle above the asthenosphere

lithosphere  (lth-sfîr)
The outer part of the Earth, consisting of the crust and upper mantle. It is about 55 km (34 mi) thick beneath the oceans and up to about 200 km (124 mi) thick beneath the continents. The high velocity with which seismic waves propagate through the lithosphere suggests that it is completely solid. Compare asthenosphereatmospherehydrosphere
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lithosphere

lithosphere
the solid part of the earth, as contrasted with the atmosphere and hydrosphere.
See also: Earth
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.lithospherelithosphere - the solid part of the earth consisting of the crust and outer mantle
layer - a relatively thin sheetlike expanse or region lying over or under another
crust, Earth's crust - the outer layer of the Earth
earth, globe, world - the 3rd planet from the sun; the planet we live on; "the Earth moves around the sun"; "he sailed around the world"
mantle - the layer of the earth between the crust and the core
Earth's surface, surface - the outermost level of the land or sea; "earthquakes originate far below the surface"; "three quarters of the Earth's surface is covered by water"


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? Mentioned in ? References in periodicals archive
 
Anorogenic magmatism is linked to lithospheric extension, hotspots and intraplate rifting and various types of mineralization associated with this style of magmatism, including Sn, Nb, Ta, U, Th, F and Be in anorogenic granites (Sawkins 1984), and Olympic Data-type Cu-Au-U iron-oxide deposits.
As a lithospheric plate passes over a hot spot, like a conveyor belt passing over a lit candle, the heat raises a chain of volcanoes.
Both samples exhibit Cr-diopsides which had once been in equilibrium with garnet peridotites under cool geothermal conditions (of the order of 37mW/m2), with no evidence for lithospheric damage and most of the grains plot within the Diamond Stability Field.
 
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