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Isostasy, the Condition of Equilibrium Between Floating Landmasses and the Denser

Question 5

Multiple Choice

Isostasy, the condition of equilibrium between floating landmasses and the denser rock beneath them, can best be explained by:


A) greater crustal thickness extending below sea level
B) a high density root system caused less dense landmass to float
C) a low density root system caused parts of the crust to stand much higher
D) both (a) and (c)

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