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The lithosphere (λίθος lithos for "rocky", and grc | σφαῖρα sphaira for "sphere") is the rigid outermost shell of a rocky planet .
Kaynak: Lithosphere
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins. Oceanic crust is primarily composed of mafic rocks
Kaynak: Oceanic crust
"pertaining to building")Little | Fowler | Coulson | 1990 is a scientific theory that describes the large-scale motions of Earth 's lithosphere .
Kaynak: Plate tectonics
plastic flowing rock about 200 km thick and the lowermost part of the lithosphere composed of rigid rock about 50 to 120 km thick A thin
Kaynak: Mantle (geology)
It lies below the lithosphere , at depths between 100 and 200 km (~ 62 and 124 miles) below the surface, but perhaps extending as deep as
Kaynak: Asthenosphere
Earth's lithosphere is divided into several rigid segments, or tectonic plate s, that migrate across the surface over periods of many
Kaynak: Earth
A craton (κράτος kratos "strength") is an old and stable part of the continental lithosphere . Having often survived cycles of merging and
Kaynak: Craton
all living beings and their relationships, including their interaction with the elements of the lithosphere , hydrosphere , and atmosphere .
Kaynak: Biosphere
In geophysics , delamination refers to the loss and sinking of the portion of the lowermost lithosphere from the tectonic plate to which
Kaynak: Delamination (geology)
In geology , a rift is a linear zone where the Earth's crust and lithosphere are being pulled apart and is an example of extensional
Kaynak: Rift
It exists at the interface of the lithosphere , atmosphere , hydrosphere and biosphere The sum total of all the organisms, soils, water
Kaynak: Pedosphere
Orogeny refers to forces and events leading to a large structural deformation of the Earth's lithosphere (crust and uppermost mantle )
Kaynak: Orogeny
nor destroy lithosphere , is a type of fault whose relative motion is predominantly horizontal in either sinistral or dextral direction.
Kaynak: Transform fault
The Philippine Sea Plate or Philippine Plate is a tectonic plate comprising oceanic lithosphere that lies beneath the Philippine Sea , to
Kaynak: Philippine Sea Plate
The lithospheric flexure (also called regional isostasy) is the process by which the lithosphere (rigid outer layer of the Earth) bends
Kaynak: Lithospheric flexure
The Pilbara craton is an old and stable part of the continental lithosphere located in Pilbara , Western Australia . It is one of only
Kaynak: Pilbara craton
In geology , a forebulge is a flexural bulge in front of a load on the lithosphere . This load causes the lithosphere to flex by
Kaynak: Forebulge
interdisciplinary field of scientific research that explores interactions between the biosphere and the lithosphere and/or the atmosphere
Kaynak: Geobiology
The phosphorus cycle is the biogeochemical cycle that describes the movement of phosphorus through the lithosphere , hydrosphere , and
Kaynak: Phosphorus cycle

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