JDługosz
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Maybe this will help: Imagine only a dense iron core, with the mantle and crust missing. You are on a tower 4000 miles from the center. As you descend, you get heavier because you get closer to the dense core.
Add a fluffy crust a few feet thick. When you move from the "outside" to the "inside" of this outer sphere, you decrease your weight by the gravity contributed by this light fluffy shell. Are there conditions such that the latter effect is smaller than the former? sure; if the crust is light enough and/or the core dense enough.
Continental rocks literally float on the mantle. So I would in fact expect that effect to occur, but can't tell without further information which change dominates.
Add a fluffy crust a few feet thick. When you move from the "outside" to the "inside" of this outer sphere, you decrease your weight by the gravity contributed by this light fluffy shell. Are there conditions such that the latter effect is smaller than the former? sure; if the crust is light enough and/or the core dense enough.
Continental rocks literally float on the mantle. So I would in fact expect that effect to occur, but can't tell without further information which change dominates.