what properties allow you to distinguish between the outer and inner core the upper and lower mantle and the asthenosphere and mesosphere
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The internal structure of the Earth is made up of concentric spherical layers: a solid outer silicate crust, an asthenosphere and a highly viscous mantle, a liquid outer core that is much less viscous than the mantle, and a solid inner core. Scientific understanding of the internal structure of the Earth is based on observations of topography and bathymetry, observations of rocks in outcrops, samples brought to the surface from greater depths by volcanoes or volcanic activity, analysis of seismic waves passing through the Earth, measurements of Earth's gravitational and magnetic fields; and experiments with crystalline solids at pressures and temperatures characteristic of the Earth's deep interior.
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