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Minerals: Building Blocks of Rocks begins with an explanation of the difference between rocks and minerals. The brief comparison is followed by a formal definition of a mineral. Elements, atoms, compounds, ions, and atomic bonding are discussed. Also investigated are isotopes and radioactivity. Following descriptions of the properties used in mineral identification, the silicate and nonsilicate mineral groups are examined. The chapter concludes with a presentation of mineral resources, reserves, and ores.
Learning Objectives
After reading, studying,
and discussing the chapter, students should be able to:
·
The difference between a mineral
and a rock.
·
What atoms are, their structure,
and how they combine.
·
Isotopes and radioactivity.
·
Compare and contrast the different
types of chemical bonding.
·
The physical properties of
minerals and how they can be used for mineral identification.
·
The basic composition and
structures of the silicate minerals.
·
The importance and uses of some
nonsilicate minerals.
·
Mineral resources, reserves, and
ores.
I. Minerals: The
building blocks of rocks
A. Mineral:
definition
1. Naturally
occurring
2. Inorganic
3. Solid
4. Orderly
internal structure
5. Definite
chemical structure
II. Composition and
structure of minerals
A. Elements
B. Atom–the smallest
particle of matter
III. How atoms are
constructed
A. Nucleus
1. Protons
2. Neutrons
B. Electrons in
energy levels, or shells
C. Atomic
number–number of protons
D. Bonding of atoms
1.
Compound–two or more elements
2.
Ions–atoms that gain or lose electrons
E. Isotopes–varying number of neutrons
1. Mass number–sum of neutrons
and protons
2. Radioactive decay–emission of
energy and particles
IV. Minerals
A. Properties of
minerals
1. Crystal
form
2. Luster
3. Color
4. Streak
5. Hardness
6. Cleavage
7. Fracture
8. Specific gravity
9. Other
a. Taste
b. Smell
c.
Elasticity
d.
Malleability
e. Feel
f.
Magnetism
g.
Double refraction
h.
Reaction to hydrochloric acid
B. Mineral groups
1. Silicate
minerals
a. Most
common mineral group
b.
Silicon-oxygen tetrahedron
1.
Independent
2.
Arranged in chains
3.
Arranged in sheets
4.
Three-dimensional arrangement
c.
Feldspars most plentiful group
d.
Crystallize from molten material
2.
Nonsilicate minerals
a. Major
groups
1.
Oxides
2.
Sulfides
3.
Sulfates
4.
Halides
5.
Carbonates
6.
"Native" elements
b.
Carbonates
1.
Major rock-forming group
2.
Found in limestone and marble
c. Halite and gypsum–found in
sedimentary rocks
d. Many
have economic value
C. Mineral
resources
1.
Reserves–profitable, identified deposits
2. Ores–metallic minerals that can
be mined at a profit
3. Economic factors may change