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45 Cards in this Set

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Minerals

Natural, inorganic, solid, that possesses an orderly internal structure of atoms and have a definite chemical composition

Rock

Any natural occurring sold mass of mineral or mineral like matter

Elements

Basic building blocks of minerals

Atoms

Smallest particles of matter that have all the characteristics of an element

The order from biggest to smallest

Rock


Mineral


Elements


Atom

Atomic mass

# of protons + # of neutrons

Nucleus

Central part of an atom that contains protons and neutrons

Proton

Positive electrical charge

Nuetron

Neutral electrical charges (no charge)

Energy levels or shells

Surround the nucleus and contain electrons

Electron

Negative electrical charges

Atomic #

# of protons in the atoms nucleus


Ex: Carbon has six protons so it’s atomic number is 6

Where does atomic mass come from

Protons and neutrons only

Bonding of atoms

Forms a compound with 2 or more elements

Ions

Atoms that gain or lose electrons

Types of atomic bonds

Ionic , covalent , and metallic

Ionic bonds

electrons are transferred between atoms (strongest bond)

Covalent

A pair of electrons are shared between atoms

Metallic bond

Electrons move freely between atoms

Isotopes

When a change in the # of neutrons causing a change the atomic mass

Ex: Carbon with 7 neutrons instead of 6

Physical properties of minerals (Most important)

Habit, Luster, Color , Streak , Hardness, and Cleavage

Physical properties of minerals (2nd best)

Fracture and specific gravity

Physical properties of minerals (3)

Taste, smell, malleability, reaction to acid, magnetism, touch, and double reaction

Habit

Common crystal shape

Luster

Appearance in light

Streak

Color of mineral in powder form

Ex Using porcelain plate to see what color comes out

Subdivisions of Luster

Metallic Luster and Nonmetallic

Metallic luster

Looks like a metal in reflected light

Nonmetallic luster

Does not look like a metal

Hardness

Resistance to scratching or abrasion of the mineral

Ex scratching glass or using fingernail to scrach

Mohs hardness scale

1- talc


2- gypsum


3-Calcite


4- Fluorite


5- apatite


6- orthoclase


7- quartz


8- topaz


9-corundum


10- diamond

Cleavage

Tendency to break along planes of weak bonding. All parallel surfaces are part of the same cleavage

Fracture

Random pattern of breakage

Specific gravity

Mineral density as a ration relative to water whose specific gravity is one

Minerals with high SG will feel heavy with low SG will feel lighter

Rock forming minerals

Made of the following: Oxygen, silicon, aluminum, iron, calcium, potassium, and magnesium

Which elements are most abundant in the crust

Oxygen (46.6%) and Silicon (27.7%)

Mineral Groups

Rock forming silicates

Mineral Groups

Rock forming silicates and nonsilicate minerals

Rock forming silicates

Most common,


Contain the silicon-oxygen tetrahedron molecule

Groups based upon tetrahedral arrangement

Olivine- independent tetrahedra


Pyroxene- tetrahedra arranged in chains


Amphibole- tetrahedra arranged in double chains


Micas- tetrahedra are arranged in sheets


Feldspars and Quartz- 3D network of tetrahedra

Micas

2 types are biotite(dark) and muscovite(light)

Feldspar

Most abundant group of minerals in earths crust

Nonsilicate minerals

Major groups are oxides, sulfides, carbonates, halides, and native elements (gold, copper, silver)

Carbonates

A major rock-forming group


Found in limestone and marble rocks

Mineral resources

Occurrences of useful minerals that will eventually be extracted. Economic factors may change and influence a resource