One of the identifying characteristics of a mineral is in
the density of the sample. Sixth graders
read earlier in the week that a mineral's density is determined by the kinds of
atoms that make up the mineral, as well as how closely the atoms are joined
together.
Geologists use special scales to determine the density of
minerals. The sixth graders estimated
the density by measuring the mass of a sample mineral on a set of balance
scales. They then measured the volume by displacing water. The density was then computed by dividing the
mass by volume.
Student teams tested five samples and then exchanged mineral
samples to verify the work of another team.
The samples were placed in greatest to least order according to the
number of grams per cubic centimeter.
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