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Different arrangements of tetrahedra in the silicate group of minerals result in differences in the minerals'
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
The relative hardness of a mineral can best be tested by
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
The mineral mica breaks evenly along flat sheets mainly because of its
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
Which mineral property is illustrated by the peeling of muscovite mica into thin, flat sheets?
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
Differences in hardness between minerals are most likely caused by the
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
Scratching a mineral against a glass plate is a method used for determining the mineral's
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
The physical properties of minerals result from their
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
Minerals are identified on the basis of
internal arrangement of atoms
cleavage
hardness
hardness, cleavage, and crystal shape
atomic arrangement
scratching the mineral across a glass plate
internal arrangement of atoms
their physical and chemical properties
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