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earth science 2 chemical
minerals
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Resource
Stock or supply of anything
that can be drawn on by anyone to function effectively
Mineral
A solid, inorganic substance
of natural occurrence, building blocks of rocks
Rock
A
conglomerate
of various minerals formed on
Earth's
surface
Characteristics of a Mineral
Naturally
Occurring
Inorganic
/
Abiogenic
Stable
/
Solid
Definite Chemical Composition
Ordered Internal Structure
Naturally Occurring
Means that a substance is not
man-made
, exists by nature without
artificial
aid
Inorganic
/
Abiogenic
Synthesized
through
geological
systems and processes, not made from living organisms
Stable/Solid
Must stay solid at room temperature (
20-25°C
), not in liquid or
gas
forms
Definite Chemical Composition
Must be defined by their
chemical composition
, expressed by their chemical formula in specific
ratios
Ordered Internal Structure
Must have regular,
repetitive
geometric patterns or
crystal
structures
Physical Properties of Minerals
Color
Streak
Luster
Penetrability
/
Diaphaneity
Tenacity
Hardness
Color
Physical color of mineral, considered unreliable as some exhibit many hues and many share similar colors
Streak
A mineral's color in powdered form, achieved by rubbing the mineral across an unweathered surface
Types of Luster
Adamantine
Earthy
/
Dull
Greasy
Metallic
Pearly
Resinous
Silky
Submetallic
Vitreous
Waxy
Penetrability
/
Diaphaneity
Property of minerals to allow light to pass through, can be
transparent
,
translucent
or opaque
Tenacity
Mineral's resistance to
breaking
or
deforming
Hardness
Measure of a mineral's resistance to
abrasions
or
scratches
Mineral
Splitting
Cleavage
Fracture
Cleavage
Tendency of minerals to
break
along planes of
weakness
(smooth, flat surfaces)
Cleavage Habits
Basal
/
Pinacoidal
Prismatic
Cubic
Rhombohedral
Octahedral
Dodecahedral
Basal
/
Pinacoidal
Cleavage
Cleaves at the base,
one
direction
Prismatic
Cleavage
Cleaves to form
prisms
,
two
directions
Cubic Cleavage
Cleaves as
cubes
,
three
directions at right angles
Rhombohedral
Cleavage
Cleaves into
rhombohedrons
,
three
directions not at right angles
Octahedral
Cleavage
Cleaves as
octahedrons
,
four
directions
Dodecahedral Cleavage
Cleaves as
dodecahedrons
,
six
directions
Fracture Habits
Conchoidal
Uneven
Hackly
Splintery
Earthy
Smooth
Subconchoidal
Conchoidal Fracture
Fracture resembles a semicircular shell with a smooth, curved surface
Uneven Fracture
Fracture
leaves a rough or
irregular
surface
Hackly Fracture
Fracture
resembles a broken
metal
, with rough, jagged points
Splintery Fracture
Fracture forms elongated splinters, exhibited by fibrous minerals
Earthy Fracture
Crumbly fracture, mineral crumbles upon fracture, reminiscent of dry earth
Smooth Fracture
Even fractures with a smooth surface reminiscent of a
perfect
cleavage
Subconchoidal Fracture
Cross between a
conchoidal
and
smooth
fractures, with a smooth, yet irregular rounded corners
Parting
Type of breaking that is often quite similar to
cleavage
, breakage along planes of weakness but in
twinning
planes
Specific Gravity
Ratio of the density of the mineral and density of
water
, < 1 means lighter than
water
and will float, > 1 means heavier than water and will sink
Crystal Habits
Acicular
Banded
Bladed
Botryoidal
Columnar
Cubic
Dendritic
Dodecahedral
Drusy
Fibrous
Foliated
Geodic
Granular
Massive
Nodular
Octahedral
Oolitic
Pisolitic
Prismatic
Radiating
Rosette
Stalactitic
Striated
Tabular
Acicular
Crystals
Have a
needle-like
shape
Banded
Crystals
Have
narrow
layers (bands) of different color and/or
texture
Bladed Crystals
Elongated crystals whose length exceeds mineral's thickness
Botryoidal
Crystals
"A bunch of
grapes
" aggregates that are
round
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