Answer:
C. Their physical properties
Step-by-step explanation:
layers:
(inside the earth)
Inner Core solid iron nickel hot 5,200°C.
Outer Core liquid layer iron nickel hot 5,000°C.
D''' Layer 2 layers, inside mantle, weird seismic waves.
Lower Mantle silicon, oxygen, magnesium iron 3700°C.
Upper Mantle silicon, oxygen, magnesium, and iron 2,200°C.
Mohorovičić Discontinuity (Moho) crust & mantle meet, and it has a sudden change in how seismic waves travel due to the difference in the density and composition of the crust and the mantle.
Crust outside layer thinnest &coolest lighter elements oxygen, silicon, and aluminum 400°C.
(outside the earth)