Transcript document

Notes: The Earth System
pg. 63
• A system is a group of parts that work together as
a whole.
• The constant flow, or cycling, of matter through
the Earth system is driven by energy.
• Energy is the ability to do work.
• Energy that drives the Earth system has two main
sources:
1.) heat from the sun
2.) heat flowing out of Earth as it cools
Earth’s System Has 4 Main
Spheres:
pg. 65
1.) Atmosphere- Earth’s outermost layer made
up of
a mixture of gases: mostly nitrogen and
oxygen. Contains dust, cloud droplets, water
vapor, rain, snow, earth’s weather
2.) Geosphere- the solid rocks and metals
that make up the Earth. Four parts: crust,
mantle, outer core, inner core
pg. 65
pg. 65
3.) Hydrosphere- Contains all of Earth’s water.
Water covers about ¾ of Earth’s surface.

97% is salt water

2% is frozen in the polar ice caps

1% is drinkable (fresh water)
pg. 65
4.) Biosphere- the parts of Earth that contain
living organisms
Notes: Constructive Vs. Destructive Forces
pg. 67
Lands are constantly being created and destroyed by
competing forces.
Constructive Forces
Destructive Forces
Forces that destroy and wear away
Forces that construct and shape
landmasses.
the land’s surface by building up
mountains and other land masses.
Examples:
Examples:
Notes: Earth’s Layers
pg. 69
How do Geologists Learn About Earth’s Layers?
A. They use two main types of evidence to learn about Earth’s
interior:
1.) direct evidence from rock samples
a. Geologists have drilled holes as deep as 12.3 km into
Earth.
b. The drills bring up samples of rock. These rocks give
geologists clues about Earth’s structure and conditions
deep inside Earth.
2.) indirect evidence from seismic waves.
a. When earthquakes occur, they produce seismic waves .
b. Geologists record the seismic waves and study how they
travel through Earth.
What Are the Features of Earth’s Layers?
B. The three main layers of Earth are the crust, mantle and core.
1.) The layers vary greatly in size, composition, temperature,
and pressure.
2.) The deeper down inside Earth, the greater the pressure.
3.) The temperature inside earth increases as depth increases.
C. The Layers of the Earth
1.) Crust – a layer of solid rock that includes both dry land and
the ocean floor (Earth’s outer skin)
a. Oceanic Crust – the crust that lies beneath the ocean;
mostly composed of basalt (a dark, fine-grained rock)
b. Continental Crust – the crust that forms the continents;
mostly composed of granite (a rock that is usually light in
color and has coarse grains)
2.) Mantle – a layer of rock that is solid, and very hot
a. Lithosphere – made up of the crust and upper mantle;
strong, hard and rigid rock
b. Asthenosphere – below the lithosphere; the material is
hotter and under more pressure; the material can bend
but is still considered a solid
3.) Core – below the mantle; made mostly of the metals iron a
nickel; consists of 2 parts
a. Outer Core – molten/liquid metals of iron and nickel
b. Inner Core – dense ball of solid metals iron and nickel
Pg. 68
Draw and Label the Layers of the Earth
Crust
Lithosphere
Asthenosphere
Mantle
Outer Core
Inner Core
I. Plate Tectonics
A. ___Continental Drift______
1. Many early scientists have noticed
that the Earth’s continents seemed
to fit together.
2. ___Alfred Wegener____- proposed
the theory of continental drift
a. _Permian Period_ - about 225
million years ago
1.) all the continents formed a
supercontinent called
Pangaea
2.) ____Panthalassa____ was
the major ocean
b. __Triassic Period____ - Pangaea
was split in two
1.) _____Laurasia_____ in the
north (North America, Eurasia)
and Gondwanaland in the
south ( India, Africa, and
South America)
2.) Panthalassa broken in two,
one part becomes the
____Tethys Sea______
pg. 71
c. Wegner theorized that continents
moved horizontally to their present
location.
B. Evidence of Continental Drift
1. Fossil and Climate Clues
a. The reptile ___Mesosaurus____
1.) fossils found in South America
and Africa
2.) lived on land and water but
would have been impossible for
this animal to have swam across
an entire ocean
b. A fern _____Glossopteris________
1.) fossils found in Africa, Australia,
India, South America, and
Antarctica
2.) found in areas that vary greatly
in climate, scientists believe
these regions once were
connected and had similar
climates
c. Fossils of warm weather plants were
found in Arctic Ocean Islands
d. Glacial deposits have been found
where no glaciers exist today
2. Sea-floor Spreading
a. ___Mid-Ocean Ridge____1. using sound waves, scientists discovered a
system of underwater mountain ranges in
many oceans
2. The peaks of some of these mountains can
form an island
b. 1960’s scientist, _Harry Hess_, suggested a
theory of ___sea-floor spreading___
1. Magma gets forced upward through
cracks in the ocean floor
2. As new material comes up it pushes
sections of the sea floor away from the
ridge.
3. The magma solidifies and creates new sea
floor
c. Evidence for Sea-floor Spreading
1. Youngest rocks are located at the midocean ridge
2. Reversals of Earth’s magnetic field are
recorded by rocks in strips parallel to
ridges
Harry Hess
C. Plate Tectonics
1. Earth’s crust and upper mantle are broken
into sections called __plates_____
a. The crust and upper mantle are called
the ______lithosphere_________
b. Middle layer of the mantle is the
_asthenosphere__ - semi-molten rock,
very plastic-like
c. __Convection Currents__ inside Earth
cause plate tectonics – the cycle of
heating, rising, cooling, and sinking of
material inside Earth
2. Plate Boundaries
a. Divergent Boundary - two plates move
away from one another; ex. Sea-floor
spreading
b. Convergent Boundary -two plates move
toward each other, there are three types:
1.) subduction zone- dense ocean plate sinks
under light continental plate
ex: deep sea trench, volcanic mountain
chains
2.) two ocean plates collide
ex: deep sea trench, volcanic island chain
3.) two continental plates collide
ex: mountains, earthquakes common
c. Transform Fault Boundary two plates slide past each other; they can
move in opposite directions or in the same
direction
Types of Heat Transfer
pg. 73
RADIATION
CONDUCTION CONVECTION
The transfer of
energy that is
carried in rays
like light
Heat transfer
between
materials that
are touching
Heat transfer by
the movement
of a fluid
Examples:
Examples:
Examples:
•
•
•
•
•
•
Roasting a marshmallow
Heat from a fire
Getting a sunburn
•
Frying an egg in a pan
Burning your feet on hot
sand
Using a heating pad on sore
muscles
•
•
Heating a pot of soup on the
stove
Warm air from a heater
rising to the ceiling
Cold air from freezer sinking
to the floor
How does stress change Earth’s crust?
pg. 77
• As Earth’s plates move, they can bend or fold rock.
• Forces created by movement of the earth’s plates are
examples of stress.
• Stress adds energy to rock until the rock changes shape or
breaks.
• Three kinds of stress occur in the Earth’s crust:
1. Tension – the stress force that pulls on the crust and
thins the rock in the middle; two plate pull apart
2. Compression – the stress force that squeezes rock until
it folds or breaks; two plate come together and push
against each other.
3. Shearing – the stress force that pushes rock in two
opposite directions; two plates slip past each other
BEFORE STRESS
TENSION
COMPRESSION
SHEARING
How do faults form?
• When enough stress builds up in the rock, the rock breaks
and makes a fault.
• There are three main types of faults:
1. Normal Faults – rock is pulled apart by tension in
Earth’s crust
2. Reverse Faults – compression pushes the rock of the
crust together
3. Strike-Slip Fault – rocks on either side slip past each
other and have little up or down motion; produced by
shearing
•
•
•
•
•
•
How does plate movement create new landforms?
Over millions of years, the forces of plate movement can
change a flat plain into features such as anticlines and
synclines, folded mountains, fault-block mountains, and
plateaus.
Folds – bends in rock that form when Earth’s crust is
compressed and gets shorter and thicker
Anticline – a fold that bends upward into an arch
Syncline – a fold that bends downward in a V shape
Fault-block mountain – when hanging walls of two normal
faults drop down on either side of the footwall
Plateau – large area of flat land that was lifted up high
above sea level
How does stress change Earth’s crust?
pg. 77
• As Earth’s plates move, _____________________________
• Forces created by ______________________________are
examples of __________________.
• Stress adds energy to rock until the rock _______________
______________________________
• Three kinds of stress occur in the Earth’s crust:
1. Tension – the stress force that _________________and
_________________in the middle; two plate pull apart
2. Compression – the stress force that ____________until
it ___________________; two plate come together and
push against each other.
3. Shearing – the stress force that ___________________
___________________; two plates slip past each other
How do faults form?
• When enough stress builds up in the rock, the rock breaks
and makes a fault.
• There are three main types of faults:
1. Normal Faults – rock is ________________by
____________in Earth’s crust
2. Reverse Faults – ______________pushes the rock of
the crust ________________
3. Strike-Slip Fault – rocks on either side ______________
___________and have little up or down motion;
produced by ___________________
•
•
•
•
•
•
How does plate movement create new landforms?
Over millions of years, the forces of plate movement can
change a flat plain into features such as anticlines and
synclines, folded mountains, fault-block mountains, and
plateaus.
Folds – __________________that form when Earth’s crust
is __________________and gets shorter and thicker
Anticline – a fold that bends ________________________
Syncline – a fold that bends _________________________
Fault-block mountain – when hanging walls of two normal
faults ___________________________________________
Plateau – large area of ________________that was ______
_______________________________________
I. Plate Tectonics
A. _________________________
1. Many early scientists have noticed
that the Earth’s continents seemed
to fit together.
2. _____________________ - proposed
the theory of continental drift
a. __________________- about 225
million years ago
1.) all the continents formed a
supercontinent called
__________________
2.) _____________________ was
the major ocean
b. ___________________ - Pangaea
was split in two
1.) ____________________ in the
north (North America, Eurasia)
and ______________ in the
south ( India, Africa, and
South America)
2.) Panthalassa broken in two,
one part becomes the
_________________________
pg. 59
c. Wegner theorized that continents
moved horizontally to their present
location.
B. Evidence of Continental Drift
1. Fossil and Climate Clues
a. The reptile ____________________
1.) fossils found in South America
and Africa
2.) lived on land and water but
would have been impossible for
this animal to have swam across
an entire ocean
b. A fern ________________________
1.) fossils found in Africa, Australia,
India, South America, and
Antarctica
2.) found in areas that vary greatly
in climate, scientists believe
these regions once were
connected and had similar
climates
c. Fossils of warm weather plants were
found in Arctic Ocean Islands
d. Glacial deposits have been found
where no glaciers exist today
2. Sea-floor Spreading
a. _________________________1. using sound waves, scientists discovered a
system of underwater mountain ranges in
many oceans
2. The peaks of some of these mountains can
form an island
b. 1960’s scientist, ______________suggested a
theory of _________________________
1. Magma gets forced upward through
cracks in the ocean floor
2. As new material comes up it pushes
sections of the sea floor away from the
ridge.
3. The magma solidifies and creates new sea
floor
c. Evidence for Sea-floor Spreading
1. Youngest rocks are located at the midocean ridge
2. Reversals of Earth’s magnetic field are
recorded by rocks in strips parallel to
ridges
Harry Hess
C. Plate Tectonics
1. Earth’s crust and upper mantle are broken
into sections called ___________________
a. The crust and upper mantle are called
the ____________________________
b. Middle layer of the mantle is the
_________________- semi-molten rock,
very plastic-like
c. ______________________ inside Earth
cause plate tectonics – the cycle of
heating, rising, cooling, and sinking of
material inside Earth
2. Plate Boundaries
a. __________________- two plates move
away from one another; ex. Sea-floor
spreading
b. __________________-two plates move
toward each other, there are three types:
1.) subduction zone- dense ocean plate sinks
under light continental plate
ex: deep sea trench, volcanic mountain
chains
2.) two ocean plates collide
ex: deep sea trench, volcanic island chain
3.) two continental plates collide
ex: mountains, earthquakes common
c. _________________________two plates slide past each other; they can
move in opposite directions or in the same
direction