Match each Earth layer or structural boundary listed in Column A with its defining physical or compositional characteristic in Column B.
- Conrad DiscontinuitySeismic boundary separating the sialic upper continental crust from the underlying simatic oceanic crust.
- AsthenosphereDuctile, partially molten zone of the upper mantle that accommodates lithospheric plate movement.
- StratosphereExternal atmospheric layer featuring temperature inversion due to solar ultraviolet absorption by ozone.
- BarysphereInnermost structural zone of the Earth characterized by extreme density and rich iron-nickel composition.
Cevap
Conrad Discontinuity matches the boundary between sial and sima crustal layers; Asthenosphere matches the ductile upper mantle zone; Stratosphere matches the atmospheric ozone heating zone; Barysphere matches the dense iron-nickel core.
Each feature correctly pairs its structural location with its chemical or physical attribute: the Conrad Discontinuity divides sialic and simatic crust, the Asthenosphere acts as the ductile upper mantle layer, the Stratosphere contains the protective ozone layer, and the Barysphere forms the dense central core region.
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Anahtar Kavram
Internal and External Structure of the Earth
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