This type of air/water/magma sinks because it's more dense

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Multiple Choice

This type of air/water/magma sinks because it's more dense

Explanation:
Density differences determine whether a parcel sinks or rises. When a substance cools, its molecules pack more closely, making it denser than the surrounding fluid. Heavier, denser material tends to sink under gravity while less dense, warmer material rises. In air, cooler air is denser than warmer air, so it sinks; in water, colder water is denser than warmer water, so it sinks; in magma, cooler magma becomes denser than hotter surrounding material and can descend. Among the options, cold is the one that becomes denser as temperature drops, so it sinks. Warm or hot are less dense and rise, and “liquefied” isn’t a density descriptor.

Density differences determine whether a parcel sinks or rises. When a substance cools, its molecules pack more closely, making it denser than the surrounding fluid. Heavier, denser material tends to sink under gravity while less dense, warmer material rises. In air, cooler air is denser than warmer air, so it sinks; in water, colder water is denser than warmer water, so it sinks; in magma, cooler magma becomes denser than hotter surrounding material and can descend. Among the options, cold is the one that becomes denser as temperature drops, so it sinks. Warm or hot are less dense and rise, and “liquefied” isn’t a density descriptor.

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