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Perovskite
A
silicate rock
Mesosphere
Much stronger than the
asthenosphere
Flows with more
resistance
Strength
increases
with
depth
due to
immense pressure
from overlying
layers
Outer core
The only mechanical layer made of
liquid
- melted
Fe-Ni alloy
The
liquid
nature of the
outer
core is due to extremely
high
temperatures (more than
3000°C
) that melt
Fe
,
Ni
, and all other elements
The flow of
liquid metals
in the
outer core
is responsible for the Earth's magnetic field
Lehmann discontinuity
The
outer-inner
core boundary
Inner core
A solid ball of mostly
Fe
despite the
extreme temperature,
due to the
overwhelming pressure
Temperatures
in the
inner core
are similar to the temperatures of the surface of the Sun - around more than
5400°C
Mineral
Naturally-occurring
Inorganic
Homogeneous solid
Has definite chemical composition
Has ordered crystalline structure
Properties of minerals
Color
Luster
Crystal habit
or
shape
Streak
Hardness
Cleavage
or
fracture
Density
or
specific gravity
Tenacity
Diaphaneity
Magnetism
Effervescence
Odor
and
taste
Thousands of different
minerals
have been identified and named, but only a few are abundant on the
Earth's crust
(
rock-forming minerals)
Out of all the elements, only
8
make up most
rock-forming minerals
Silicates
The most common mineral group, using
oxygen
and
silicon
as their "
building blocks
"
Non-silicate mineral groups
Native elements
Carbonates
Oxides
Sulfates
Phosphates
Igneous rocks
Formed when
molten material cools
and
solidifies
Intrusive igneous rocks
Form
below
the
Earth's surface
Extrusive igneous rocks
Form
on
the
Earth's
surface
Intrusive vs extrusive igneous rocks
Intrusive have
bigger/coarser
mineral grains, extrusive have
smaller/finer
grains
Komatiite
A very rare type of
extrusive igneous rock
that forms when
extremely hot
lava cools rapidly, common during the
Archean eon
Other extrusive igneous rocks
Obsidian
Bombs
Blocks
Volcanic ash
Sedimentary
rocks
Formed from loose
sediments
that have been
eroded
,
buried
and
compacted
Types of sedimentary rocks
Clastic sedimentary
rocks
Chemical sedimentary
rocks
Biochemical
or
organic sedimentary
rocks
Metamorphic rocks
Formed when a rock is subjected to
chemical
or
physical
processes that alter its
composition
,
mineralogy
, and/or
texture
Foliated
metamorphic rocks
Have a
planar
arrangement of mineral grains, result of
deformation
Non-foliated metamorphic rocks
Develop in environments with
minimal deformation,
other factors like
chemically-active fluids
play a
larger
role
Rocks continually undergo changes that alter their characteristics, ultimately changing them into different rocks
(
rock cycle)
Erosion
A
geological
process where earth
materials
are
weathered
and
transported
Deposition
The process of adding
eroded
earth
materials
to an
environment
or
landform
Types of depositional environments
Terrestrial
environments
Transitional
environments
Marine
environments
Terrestrial depositional environments
Fluvial
Eolian
Alluvial
Glacial
Lacustrine
Terrestrial landforms and waterforms
Mountains
Hills
Plains
Valleys
Plateaus
Deserts
Glacial environments
Rivers
Transitional depositional environments
Beach
Deltaic
Tidal flat
Lagoonal
Transitional landforms and waterforms
Deltas
Wetlands
Swamps
Marshes
Marine depositional environments
Shallow
marine/reefal
Continental
shelf
Continental
slope
Deep
marine
Tidal flat
Low-lying
areas affected by
tides
Lagoonal
A
small
body of
water
closed off from a
larger
body of
water
(the
ocean
)
Associated landforms and waterforms
Deltas
Wetlands
Swamps
Marshes
Deltas
Areas at the end of the
mouth
of a
river
where
freshwater
mixes with
seawater
Wetlands
Areas near
rivers
or
coastlines
where
soils
are
saturated
or
submerged
in
water
Swamps
Wetlands
where trees
dominate plant life
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