Welcome to 6th Grade! » Science » Minerals
Minerals are naturally-occurring solids that have a crystal structure, are inorganic, and have a definite chemical composition.
•Naturally-occurring- not man-made
•Solid- keeps its shape
•Crystal-repeating pattern of shapes in the particles
•Inorganic- not made of living things
•Definite chemical composition- contains elements in definite proportions
uHave a repeating pattern of particles
uHave flat sides (faces)
uHave sharp edges and corners
Quartz Often Exhibits Good Crystal Form.
Substance composed of one kind of atom. Atoms are
the smallest particles of an element. Elements are the basic building blocks of minerals.
Two or more elements combined.
What are minerals and what are their characteristics?
Properties of Minerals
u Hardness is a measure of the resistance of a mineral to being scratched.
u Mohs scale consists of 10 minerals arranged from 10 (hardest) to 1 (softest).
Mohs Scale of Hardness
Mohs Hardness Scale
Number - Description - Example Mineral
1 -rubs off on fingers - talc
2 -can be scratched by fingernail - gypsum
3 -can be scratched by a copper penny - calcite
4 -can be scratched by a steel nail - fluorite
5 -can be scratched by a steel nail - apatite
6 -scratches glass - feldspar
7 -scratches steel or glass - quartz
8 -scratches quartz - topaz
9 -scratches topaz - corundum
10 - scratches all materials - diamond
u Small amounts of different elements can give the same mineral different colors.
u Streak is the color of a mineral in its powdered form.
u Luster is used to describe how light is reflected from the surface of a mineral.
Pyrite (Fool’s Gold) Displays
u Density is mass per volume.
uu The pattern of how the crystals are arranged.
uu There are six different crystal systems
u Cleavage is the tendency of a mineral to cleave, or break, along flat, even surfaces.
Mica Has Cleavage in One Direction
How Minerals Form
1. Crystallization from magma
Minerals Formed as a Result of Crystallization of Magma
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