Minerals and Rocks Flashcards
- naturally occurring
- has a definite chemical composition
- a definite crystal structure
mineral
examples of graphite
carbon
pencil lead, batteries
examples of sulfur
nonmetalic, chemical
matches, fireworks
examples of talc
Powder, ceramics
examples of non minerals
cement, steel, man-made
not composed of organic matter/not from living things
inorganic
coal is from?
plants
amber is from?
tree sap
pearls are from?
oysters
have a definite volume and a definite shape
SOLIDS
Mercury is not a mineral because?
it is liquid at room temperature
combined with one or more metals
(largest group of minerals)
silicate minerals
extremely rare
(subdivided into several
other classes)
non-silicate minerals
elements found in nature in their mineral form
native elements
minerals that contain sulfur ions
sulfides
minerals which include the sulfate ion
sulfates
minerals that contain oxygen bonded with one or more metals
oxides
minerals containing (OH) are typically included in this class.
hydroxides
minerals with that contain Fluorine,
Chlorine, Bromine and Iodine ions.
Halides
minerals that contain a carbonate ion, CO2−3.
Carbonates
The internal structure or arrangement of atoms within a mineral
CRYSTAL STRUCTURE/Halite (NaCl)
Atoms/molecules are arranged in?
repeating geometric patterns
what are the six (6) BASIC CRYSTAL SYSTEMS?
- cubic
- tetragonal
- hexagonal
- orthorhombic
- monoclinic
- triclinic
minerals form when?
a) lava or magma cools to solidification
b) water evaporates and leaves minerals remain
c) water is supersaturated with a mineral; minerals will settle out of the water and deposit as a precipitate.
what are the six (6) Physical Properties?
- color
- streak
- luster
- hardness
- cleavage or fracture
- density
Specific and unique for each mineral
Chemical Properties
Determined by chemical composition and structure
IDENTIFYING MINERALS
Not a reliable property; some minerals can be many different colors
PHYSICAL PROPERTIES
Color may vary due to?
1) Natural coloring agents -impurities
2) Weathering; exposure to the environment
The color of the mineral in its powdered form
Streak
Determined by using a streak plate
PHYSICAL PROPERTIES
The way a mineral shines/reflects light from its surface.
Luster
reflects light like the surface of a
polished metal
Metallic
reflects light in more subtle ways
Non Metallic
A measure of how easily a mineral can be scratched.
a) Determined by a
minerals internal structure.
b) When a mineral is scratched by a substance; it is softer than the substance
c) When a mineral scratches a substance; it is harder than the
substance
Hardness
When a mineral splits/breaks along smooth flat surfaces
(is the way a mineral breaks)
Cleavage
One direction; sheet
Mica
Three; cubic shape
Galena
is the way crystal grows
crystal shape
When a mineral breaks unevenly
into curved or irregular pieces with a rough and jagged surfaces.
Fracture
examples of sulfur?
bauxite, hematite, quartz
Minerals have different densities, and vary in weight given the same sample size
(How heavy the mineral feels in your hand)
Density or Heft
what are the three (3) SPECIAL PROPERTIES?
Lodestone-Magnetite
Iceland Spar-Calcite
Pitchblend
what is a Pitchblend?
radioactive
what is a Iceland Spar-Calcite?
produces double refraction
what is a Lodestone-Magnetite?
naturally magnetic
A mineral that contains metals and
nonmetals that can be mined and removed in usable amounts; for a profit
Ore
elements that have a shiny surfaces, are able to conduct heat and electricity, and are malleable
Metals
Elements that have dull surfaces
and are poor conductors of heat and electricity and are brittle.
Nonmetals
A mixture of two or more metals or a mixture of metals and nonmetals
Alloy
Minerals that have desirable qualities; such as hardness, color, luster, clarity, durability, rarity…
Gems
what are the four (4) Precious Stones?
Diamond, Rubies, Sapphires, Emeralds
what are the three (3) Semi-Precious Stones?
Amethyst, Garnet, Topaz
Gems that are not minerals
Pearls, Amber
Many kinds of rocks are composed of minerals
Granite; mica, feldspar and quartz
rocks that are composed of ONLY ONE mineral
Monomineralic
rocks that are composed of TWO OR MORE minerals
Polymineralic
There are almost 4, XXX different minerals
4,700
Silicates make up to how many % of the crust?
90%
are classified based on their method of formation/origin.
Rocks
3 Rock Groups
- Sedimentary
- Igneous
- Metamorphic
Rocks that usually form in horizontal layers; from the accumulation of sediment, organic matter, or chemical precipitates
SEDIMENTARY ROCKS
form from mineral particles and
sediment that are compacted and cemented together
Clastic
pressed by weight of overlying rock
Compaction
glued by natural cements in water
Cementation
form from minerals dissolved in
water; which settle-out/precipitate.
Chemical
form from the accumulation of
plant/animal matter that undergoes a transformation into rock.
Organic
a) They are composed of rock, mineral or organic particles.
b) Some have a range of particle sizes.
c) Some have a uniform sediment size; due to sorting during deposition
SEDIMENTARY CHARACTERISTICS
0.2 - 0.006cm
Sandstone
0.006 –0.0004cm
Siltstone
less than 0.0004 cm
Slate
Some rocks are organic and may contain?
fossils
Usually form in horizontal layers called?
strata or beds
Form from the cooling and
crystallization/solidification of molten lava or magma
IGNEOUS ROCKS
TWO TYPES OF IGNEOUS ROCKS
Extrusive/Volcanic
Intrusive/Plutonic
Forms from the fast cooling of lava on or near Earth’s surface.
Extrusive/Volcanic
Form from the slow cooling of magma within the Earth
Intrusive/Plutonic
Rocks that form from pre-existing rocks (sedimentary, igneous, metamorphic);that have been changed.
(Often found in mountainous regions where the deeper bedrock
is exposed due to weathering and erosion)
METAMORPHIC ROCKS
can rearrange and form new rocks due to contact with extreme heat
(magma), or extreme pressure (orogeny)
Molecules
Conditions that cause rocks to undergo metamorphism
1) Heat
2) Pressure
3) Chemical Activity
Rocks around a magma/lava can be metamorphosed through direct contact with the magma/lava
Contact Metamorphism
Rocks buried deep within the crust can re-crystallize due to extreme pressure during mountain building events
Regional Metamorphism
Environments within the crust have high temperatures and high pressure; causing rocks to change by recrystallization.
METAMORPHIC CHANGES
TYPES OF METAMORPHIC ROCK
TEXTURE
Foliated
Non-Foliated/Unfoliated
Rock has mineral crystals arranged
in layers or parallel bands.
Foliated
Minerals join; but do not form visible layers.
Mineral Alignment
Mineral crystals join and arrange in
layers; Gneiss
Banding
Rock does not have mineral crystals arranged in layers; do not break in layers/sheets
Non-Foliated/Unfoliated
examples of famous rocks
- whitehouse; sandstone
- grand canyon; layers of sedimentary rocks
- mount rushmore; granite
- pyramids; limestone
- great wall of china; stone, brick, etc.
igneous rocks examples
obsidian, granite
sedimentary rocks examples
sandstone, limestone
metamorphic rocks examples
slate, marble
minerals examples
quartz, talc, halite, silver, copper, diamond
what is Au element?
gold
what is S element?
sulfur
what is Ag element?
silver
Tin+Copper
Bronze
Copper+Zinc
Brass
Iron+Chromium+Limestone
Steel
Tead+Tin
Pewten