
History of the Earth
Presentation
•
Science
•
9th Grade
•
Medium
+15
Standards-aligned
Hope Moyo
Used 2+ times
FREE Resource
13 Slides • 32 Questions
1
UNIT 2: Earth As A
System
2
The structure of Earth
After the planet formed about 4.6 billion years ago, several processes released heat that kept the surface a molten pool of metals.
1.
Bombardment: The young planet was bombarded by
material from space which collided with the planet causing
the planet to heat up. This kept the surface of planet earth
molten.
2.
Accretion: the process by which material from space is
added to the planet. This added mass to the planet. The
increase in the mass of earth causes an increase in the
gravitational force of earth.
3
The structure of Earth
3. Differentiation: describes how
molten material changed position in the planet based on density.
Molten metals like nickel and iron sank towards the center of the earth while the less dense
materials like aluminum and
silicon rose to the planet’s surface.
4
Chemical composition of Earth
Earth consists primarily of six elements:
● Iron (Fe)
● Oxygen (O)
● Silicon (Si)
● Magnesium (Mg)
● Nickel (Ni)
● Sulfur (S)
5
Chemical composition of Earth
Early earth is made primarily of
dense liquid metals.
The liquid iron and nickel were
more dense and sank to the center while the less dense materials like silicon and aluminum rose to the
surface.
Over time, the molten materials separated into 3 layers:
6
Multiple Select
Which of the processes contribute to the heating up of the young planet earth? Pick 3!
Bombardment
Accretion
Creation
Differentiation
7
Multiple Choice
____ is the process by which material from space is added to the planet.
Bombardment
Accretion
Differentiation
8
Multiple Choice
____describes how molten material changed position in the planet based on density.
Bombardment
Accretion
Differentiation
9
Multiple Select
Choose the elements that earth is made up of
Iron
Fluorine
Magnesium
Zinc
Nickel
10
Multiple Select
The core is made from which 2 elements?
iron
aluminum
silicon
nickel
11
Multiple Select
The outer parts of earth are made from which 2 elements?
iron
aluminum
silicon
nickel
12
Layer
Divisions
Composition
Thickness
Temperature
Distance from
surface of
earth
More info
1.Core
Inner
core
Solid mixture
of iron and
nickel.
6,400 km
5,000 to
7,000 oC
5,150 to
6,370 km
below Earth
Has a density of
13.5 g/cm3
Outer
core
Liquid mixture
of iron and
nickel
5,100 km
4,400 to
6,100 oC
2,891 to
5,150 km
below Earth
Remains liquid
due to lower
pressure than
inner core
2. Mantle
Mantle
Aluminum,
iron,
magnesium
and silica
2,900 km
870 oC
Lies 2,891 to
40 km below
Earth’s
surface
Accounts for 70%
of the volume of
Earth
Asthenosphere: upper mantle which comes in direct contact with the lithosphere.
3. Crust
-
Rock
50 km
–
Relatively thin and adds very
little to the volume of the planet.
Earth’s Composition
13
Draw
Draw an arrow and point to the inner core and label it A.
14
Draw
Draw an arrow and point to the mantle and label it B.
15
Draw
Draw an arrow and point to the crust and label it .
16
Multiple Choice
Which layer makes up 70% of the earth's volume?
core
crust
mantle
17
Multiple Choice
Which layer of earth is LIQUID?
Outer core
Inner core
Crust
mantle
18
Multiple Choice
Name the layer that has a temperature of 5,000 to 7,000 degrees Celcius.
Inner core
Outer core
Mantle
core
19
Multiple Choice
Name the layer that is thin and adds very little to the volume of the planet
Mantle
crust
20
Earth’s Early Atmosphere
The atmosphere is made up of gasses that
surround the surface of Earth.
The earliest atmosphere was made up of primarily two gasses: hydrogen and helium.
These gasses were too light and were swept away by solar wind to outer space.
Solar wind is made up of charged particles from the surface of the sun.
21
Earth’s Early Atmosphere
Gasses from early atmosphere came from volcanoes and consisted mostly of gasses such as hydrogen, water vapor, carbon dioxide and hydrogen sulfide.
Early atmosphere also contained small
amounts of nitrogen, carbon monoxide
and methane.
22
Earth’s Second Atmosphere
About 4 billion years later, earth began to cool.
Volcanic eruptions produced gasses
such as water vapor, carbon dioxide, hydrogen sulfide and trace amounts of nitrogen, carbon monoxide, methane and ammonia.
Many of these gasses reacted with
minerals on land or dissolved in the
ocean.
23
Earth’s Second Atmosphere
The gasses that did not react began to accumulate and form Earth’s second atmosphere.
The ammonia released from volcanoes was broken down by the
sun.
The breakdown of ammonia increased
the amount of nitrogen in the
atmosphere.
24
Earth’s Third Atmosphere
Around 2.5 billion years ago, oxygen in the atmosphere increased as a result of the byproducts of photosynthesis.
25
Formation of Earth’s Oceans
Early earth was inhospitable due to the high temperatures.
The surface of earth was a pool of molten materials.
When Earth’s surface cooled, a thin brittle layer called the crust was formed.
Over time, early crust was melted and
reformed many times.
26
The Lack of Oxygen
Oxygen in the atmosphere was
released by ancient blue green
bacteria.
These organisms conducted photosynthesis which is a reaction that changes carbon dioxide and water to glucose, a simple sugar.
A byproduct of photosynthesis is oxygen gas.
27
Multiple Choice
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Multiple Choice
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Multiple Choice
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Multiple Choice
31
Multiple Choice
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Multiple Choice
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Multiple Choice
34
Multiple Choice
35
Multiple Choice
36
Multiple Choice
37
Multiple Choice
38
Multiple Choice
39
Multiple Choice
40
Multiple Choice
41
Multiple Choice
42
Multiple Choice
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Multiple Choice
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Multiple Choice
45
Multiple Choice
UNIT 2: Earth As A
System
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