Earth lithosphere

E21755

The Earth lithosphere is the planet’s rigid outer shell, comprising the crust and uppermost mantle broken into tectonic plates that move and interact to shape Earth’s surface.


Statements (47)
Predicate Object
instanceOf geological layer
tectonic shell
averageAgeContinental up to several billion years in cratons
averageAgeOceanic less than about 200 million years
boundaryType convergent plate boundary
divergent plate boundary
transform plate boundary
composedOf solid rock
contains major mineral and energy resources
defines tectonic plate boundaries
densityComparison oceanic lithosphere is denser than continental lithosphere
dividedInto tectonic plates
hasProperty brittle
rigid
hasType continental lithosphere
oceanic lithosphere
includes Earth crust
uppermost mantle
influences distribution of continents and oceans
global carbon cycle via subduction and volcanism
long-term climate through tectonics
involvedIn earthquake generation
mountain building
plate tectonics
volcanic activity
mechanicallyDistinctFrom asthenosphere
motionDriver mantle convection
ridge push
slab pull
movesOver asthenosphere
olderComponent continental lithosphere
overlies asthenosphere
partOf Earth
separatedFrom asthenosphere by the lithosphere-asthenosphere boundary
studiedIn geology
geophysics
plate tectonics theory
supports Earth topography
isostatic equilibrium of continents and oceans
thermalControl cooling thickens lithosphere over time
thicknessRange about 50–100 km under typical ocean basins
about 5–10 km at mid-ocean ridges
up to about 200–250 km under stable continental cratons
undergoes continental collision
seafloor spreading
subduction
youngerComponent oceanic lithosphere


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