Save
...
G11 SEM1 Q1
EARTH SCIE 1Q
L3-L4 | ROCK
Save
Share
Learn
Content
Leaderboard
Share
Learn
Created by
sandra
Visit profile
Cards (46)
IGNEOUS
ROCKS
Forms from
solidification
and
cooling
of lava or magma
2 TYPES OF IGNEOUS ROCKS:
intrusive
/
plutonic
igneous rock
extrusive
/
volcanic
igneous rock
INTRUSIVE
/
PLUTONIC
IGNEOUS ROCK
Magma
solidifies
Cools down
slowly
because they are formed
under
the earth’s surface, when the magma chamber’s force is not enough to force them (magma) up.
EXTRUSIVE
/
VOLCANIC
IGNEOUS ROCKS
Lava
solidifies
Cools down
quickly
because they are formed
on
the surface (lava)
May be
vesicular
→ contains air bubble
These exposed igneous rock will be
sediments
→ due to the weathering or explosion, or erosion on the surface
WEATHERING
Disintegration
or
breaking
down
of rocks (sedimentary)
PHYSICAL
WEATHERING - Changing of the big rocks to smaller pieces.
CHEMICAL
WEATHERING - Acid rain (weakening of the rocks)
EROSION
Displacement
or
transportation
to another, usually at the bodies of
water.
AGENTS OF EROSION
Those who carries these rocks to the bodies of water
Wind
Water
Human
factors
Animal
factor
Waves
Glacier
Gravity
(big factor)
If these rocks are brought to the bodies of water, they would be
buried
(
deposition
)
These rocks will be
compacted
and
cemented
, along with other rocks becoming a sedimentary rock
SEDIMENTARY
ROCKS
Formed from
pre-existing
rocks or pieces of living organism
Forms from the
compaction
and
cementation
of sediments
COMPACTION
Due to the weight above the rocks
CEMENTATION
Chemicals underwater segments the sediments
2 TYPES OF SEDIMENTARY ROCKS
clastic
sedimentary rocks
non-clastic
sedimentary rocks
CLASTIC
SR
Coming from the sediments made of
rocks
(gathered)
Form from fragments of
pre-existing
rocks
NON-CLASTIC
SR
minerals that have
precipitated
from water or have been formed through
biological
process
METAMORPHIC
ROCKS
Rocks that are subjected to high heat, high pressure, hot mineral-rich factors, or combination of these factors.
ROCK
CYCLE
transformations of one type of rock to another
TYPES OF METAMORPHIC ROCKS:
regional
METAMORPHIC ROCKS
contact
METAMORPHIC ROCKS
REGIONAL MR
Undergoes metamorphism due to the pressure
Occurs in a
regional
/
large
scale
Creates
foliated
metamorphic rock
CONTACT MR
Undergoes metamorphism due to the heat
Occurs on relatively
small
scale
Creates
non-foliated
metamorphic rock
ROCKS
Aggregate of
minerals
Can be composed of single mineral or commonly, as an aggregate of two or more minerals
TYPE OF IGNEOUS ROCKS BASED ON COMPOSITION
felsic
intermediate
mafic
ultramafic
FELSIC
>
65
% silica content
light
colored
INTERMEDIATE
55-65
% silica content
MAFIC
45-55%
silica content
ULTRAMAFIC
<
45
% silica content
dark
colored
low
silica content,
high
metal content,
high
temperature
INCREASING METAMORPHISM
shale
->
slate
->
phyllite
->
schist
->
gneiss
MINERAL
OCCURRENCE
Concentration of the mineral that is of scientific or technical interest.
MINERAL
DEPOSIT
Mineral occurrence of sufficient size and grade with concentration to enable extraction under the most favorable conditions.
ORE
DEPOSITS
Mineral deposits that have been tested and known to be economically profitable to mine.
AGGREGATE
Rock or mineral used as a filler in cement, asphalt, plaster, etc.
Generally used to describe nonmetallic deposits.
ORE
Naturally-occurring material from which a minerals of economic value can be extracted
TYPES OF MINERAL RESOURCES
magmatic
ore deposits
hydrothermal
ore deposits
sedimentary
ore deposits
placer
ore deposits
residual
ore deposits
MAGMATIC
ORE DEPOSITS
concentrated within a body of igneous rock
MAGMATIC PROCESSES:
crystal
fractionation
partial
melting
crustal
settling
2 TYPES
crystal
settling
fractional
crystallization
SEDIMENTARY
ORE DEPOSITS
concentrated by
chemical
precipitation
from lakes or sea water.
2 TYPES OF SEDIMENTARY:
evaporite
deposits
iron
formation
HYDROTHERMAL
ORE DEPOSITS
concentration of valuable substance by hot
aqueous
(water rich)
fluids
flowing through fractures and pore spaces in rocks.
See all 46 cards