The density of any object is given by its mass divided by its volume.

Mathematically, density equals mass divided by volume.

The density at all points of a homogeneous object equals its total mass divided by its total volume.

The beauty is that we can directly determine the density of the planet, which is its mass divided by its volume.

It is equal to the molar mass (M) divided by the mass density (ρ).

To the right the glacier descended in shattered masses, divided by yawning crevasses.

Then they calculated the density (mass divided by volume) and went to the density tables in their textbooks to identify the liquid.

Mathematically, density is defined as mass divided by volume.

The density of the sample is simply its mass divided by its volume.

It's really pretty easy: density of an object is the object's mass divided by the object's volume.