Step 1: Concept of isostasy and gravity anomalies.
Large mountains are typically compensated by a less dense root extending into the mantle — like an iceberg floating in water.
Step 2: Explaining the smaller-than-expected gravitational effect.
If the observed gravitational deflection is less than what’s expected from the visible mass, it implies a mass deficiency beneath — i.e., a low-density root is counteracting the mountain’s gravitational pull.