Title: Chapter 7: Forces Shaping Earth
1Chapter 7Forces Shaping Earth
- Note-taking worksheets 1 2
2NTW 1 Earths Layers
- Geologists study earthquakes and surface rocks to
indirectly observe Earths interior.
3When an earthquake occurs, energy is carried
through objects by seismic waves. These seismic
waves change speed and direction depending on the
density and material they travel through.
4With evidence from earthquake waves and exposed
rocks, scientists have developed a model of
Earths interior. This model shows Earth as
having four distinct layers.
5Quiz
- What do Geologists study so that they can
indirectly observe Earths interior? - How is energy carried through objects in an
earthquake? - What determines if a seismic wave will change
speed and direction? - How many layers does the Earths interior have?
6The Inner Core is the innermost layer of Earths
interior.
- This part of the Earths interior is very dense
and composed mostly of solid iron.
7The Inner Core
- It is believed that the temperature is 5000
degrees Celsius.
This layer experiences the greatest amount of
pressure.
8The Outer Core lies above the inner core.
- It is thought that this layer is composed mostly
of molten metal, such as iron and nickel, making
it a liquid.
9The Outer Core
- Seismic studies indicate that this layer is
uneven in nature.
10Quiz
- What is the innermost layer of Earths interior
called? - What is the layer that lies above the inner core
called? - Which layer of Earths interior is very dense and
composed mostly of solid iron? - Which layer of the Earths interior experiences
the greatest amount of pressure? - Which layer of the Earths interior is composed
mostly of molten metal making it a liquid? - Which layer of the Earths interior has the
greatest amount of pressure?
11The mantle is the largest layer of Earths
interior.
- Even though the mantle is a solid, the mantle
flows slowly similar to putty. Most of the
mantle is made of iron and magnesium.
12The Mantle
- The mantle is composed of two parts, the
lithosphere which is closest to Earths crust and
the asthenosphere.
13The crust is Earths outermost layer.
- Earths crust is thin when compared to the other
layers, although the thickness varies. It is
thinnest under the oceans and thickest through
the continents. It is composed mostly of oxygen
and silicon.
14Quiz
- What is the Earths outermost layer called?
- What is the largest layer of Earths interior
called? - List in order the four layers of the Earth
starting from the center one. - Which layer is a solid but flows slowly?
- Which layer of the Earth is the thinnest?
- What are the two parts of the mantle called?
- Where is the Earths crust the thinnest and where
is it the thickest?
15Density, temperature and pressure are properties
of Earth that are lowest in the crust and
greatest in the inner core.
16Quiz
- Are density, temperature and pressure the same no
matter where you are inside the Earth? - Where are density, temperature and pressure the
greatest? - Where are density, temperature and pressure the
lowest? - Why do you think this happens?
17NTW 2 Earths Plates
- The rigid, upper part of Earths mantle is called
the lithosphere.
18It is broken into about 30 sections or pieces
called plates that move around on the plastic
like asthenosphere which is also part of the
mantle.
- The major tectonic plates include Eurasian,
African, Australian-Indian (Indo-Australian),
Pacific, North American and South American.
19The movement of the plates is fairly slow, yet
over millions of years, plates and land masses
have moved great distances.
20The historical evidence that plates are moving
includes continents fit together like jig-saw
puzzle, same fossils found on different
continents and large amount of volcanic and
earthquake activity.
21Quiz
- The ________ is the rigid upper part of the
Earths mantle and the ________ is the plastic
like lower part. - The lithosphere is broken into about 30 sections
or pieces called ________. - State one reason scientists believe plate
techtonics occurred. - How many major techtonic plates did we list?
22THREE WAYS PLATES MOVE
- 1) Plates Move Apart The pulling force called
tension pulls two plates apart resulting in the
formation of new lithosphere. This process of
plate separation and lithosphere formation that
takes place under the oceans is called mid-ocean
ridges. High ridges often form.
23Quiz
- When plates move apart, the pulling force is
called ______. - When plates pull apart, they form new __________.
24THREE WAYS PLATES MOVE
- Plates That Collide
- A) When two plates of similar density collide
the crusts pile up. This force is called
compression. As rock layers are compressed, they
fold and fault and pile up to form mountains.
25THREE WAYS PLATES MOVE
- Plates That Collide
- B) When two plates of different densities
collide, the more dense plate plunges underneath
the other, forming a deep trench. When one plate
sinks underneath another plate, it is called
subduction. Volcanoes many times form in these
areas.
26Quiz
- When plates of similar density collide, what
happens to the crusts? - When plates of different densities collide, what
happens to the crusts? - When the plates collide, the force is called
___________. - When one plate sinks underneath another plate, it
is called _________.
27THREE WAYS PLATES MOVE
- 3) Sliding Plates - Plates can also slide past
one another and the boundary where these plates
meet is called a transform boundary. When a
force pushes something in different directions it
is called shearing. Where shearing occurs faults
form and the area experiences many earthquakes.
28Quiz
- When plates slide past one another, the boundary
where these plates meet is called a ____________
boundary. - What is shearing?
- What happens to the area where shearing occurs?
- What are the three ways a plate can move?
29Why Plates Move
- Scientists have come up with theories to explain
the plate movements but do not know for sure why
the large plates move. One theory is convection
of the mantle when uneven heating causes cycling
of material in the mantle to move.
30Why Plates Move
- Another theory is called Ridge-push where
mid-ocean ridges cause plates to slide down a
slope. Slab-pull happens as plates move away
from mid-ocean ridges and become denser.
31Other Forces Shaping Earth
- Weathering is breaking down rock into sediment.
Erosion moves the sediment. Deposition then
leaves the sediment in a new place, creating new
landforms.
32Two Types of Weathering
- a. Physical (Mechanical) weathering breaks down
the rocks physically. Examples plant roots
grow into rock, water freezes inside of cracks in
the rock.
33Two Types of Weathering
- b. Chemical weathering occurs when a minerals in
a rock are changed chemically. Examples oxygen
reacts with iron in rocks to produce rust.
34Quiz
- What is the theory called where mid-ocean ridges
cause plates to slide down a slope? - What are the three other things shaping Earth?
- What are the two types of weathering?
35Write the following of the back sides of the
foldable for each of Earths layers.
- Inner Core
- Solid
- Made of iron
- Temperature of 5000 degrees Celsius
- Experiences the greatest pressure
- Outer Core
- Molten metal making it a liquid
- Mostly made of iron and nickel
- Uneven in structure
- Mantle
- Largest/thickest layer
- Solid yet flows slowly like putty
- Made mostly of iron and magnesium
- Two parts Asthenosphere and Lithosphere
- Lithosphere is on the top part of the mantle,
right under the crust - Crust
- Outermost layer
- Mostly made of oxygen and silicon
- Thinnest of all layers
36(No Transcript)
37(No Transcript)
38(No Transcript)
39(No Transcript)
40(No Transcript)
41(No Transcript)
42(No Transcript)