1. Rocks are naturally formed, consolidated material composed of grains
of one or more minerals. Minerals are crystalline (orderly three-dimensional arrangements
of atoms).
2. Elements are substances that cannot be broken down by ordinary chemical
methods. Atoms are the smallest particles of elements. They are constructed of
protons, neutrons (forming the nucleus) and electrons. Atomic mass number,
atomic number and atomic weight control the"character" of an element,
particularly its isotopes.
3. Chemical activity is related to ions and their bonding.
4. Eight elements comprise 98% of the weight of the crust. Oxygen accounts
for half the weight of the crust. Silicon is the second most abundant element
in the crust and silicate minerals, combinations of oxygen and silicon, are
the most common in the crust.
5. Crystalline substances have a three-dimensional, regularly repeating,
orderly pattern of their anions. The silica tetrahedron is the basic "building
block" of most common (silicate) minerals. Silicate structure reflects
the arrangement of silica tetrahedra and the numbers of shared oxygens. These
structures include: isolated silicate structure (no shared oxygens), chain-silicates
(two shared oxygens), sheet silicates (three shared oxygens), and framework
silicates (four shared oxygens).
6. Minerals are naturally occurring solids that are crystalline (which is
to say that they have a periodically repeating arrangement of atoms) and have
a specific chemical composition. Specific chemical composition reflects the
orderly internal arrangement of atoms. Zoning further reflects the orderly
arrangement.
7. A small number of rock-forming minerals comprise most of the crust. Five
mineral groups (feldspar, quartz, pyroxene, amphibole, and mica) account for
greater than 90% of the earth's crust. Feldspars are the most common crustal mineral,
while olivine is the most abundant mineral in the earth as a whole. Nonsilicates
are either native elements or are classified by their negative ion. These
include ore minerals of commercial value.
8. Physical properties are used to identify minerals. These include color,
streak, luster, hardness, external crystal form, cleavage, fracture, specific
gravity, special properties (smell, taste, striations, magnetism), and other
properties (double refraction, effects of polarized light, x-ray defraction).
Chemical tests can be used to identify minerals.
