Section 1-4
Teaching Outline
Book J
Earth Science
Exploring the Planets Software:
NASA News:
Come
up with three questions per team that you will ask the class.
Slide 1: Two main features of the
Moon
1. Highlands (Terra)
2. Lowlands (Maria)
Button: Compare to Earth
Highlighted: Highlands: older and heavily
cratered
Highlighted: Cratered: Cratered
Caldera: Caldera:no raised rims
Highlighted Maria: Basaltic Lava
Flows, (seas)
EX: Basalt samples from earth
Highlighted Basalt:
Highlighted: Mare: singular of
Maria
Highlighted: Basaltic Lava
Slide 2: Features found
on the moon. Craters, Volcanic Flows, Tectonic Features, No Atmosphere,
No water.
Highlighted: Tectonic:
The folding
and faulting of a planets crust.
Highlighted: Atmosphere:
the sphere
of gas surrounding a planet including water vapor
Slide 3: The Far side of the moon
Only photographed from space craft. Why?
Older and more cratered than the Earth side of the Moon.
Slide 4: The orbit, Rotation
and Revolution of the Moon.
Why are they the same?
Slide 5: There were six mission to the Moon. 3 Astronauts
per mission. 2 astronauts per mission went to
the surface. Discuss Lunar Command Module and Lunar
Lander
Highlighted:
Regolith:
the
broken pieces of rocks and minerals that make up a planets surface.
Slide 6: Since there is no air or atmosphere on the
moon there is no sounds. You couldn't hear someone
scream or an avalanche or a meteor impact. You might
feel the vibration through your feet.
Slide 7: There is also no weather on the Moon so footprints
or craters will remain for thousands or
millions of years. Nothing to wash or blow them away.
Slide 8: Button:
Replay:
Gravity on the moon is 1/6th the gravity of Earth.
Assignment:
calculate
your weight on the Moon. Divide your weight by 6.
How much would you weigh with
a 160 lbs space suite on?
Slide 9: Cratering before 3.8 billion years ago was
very intense.The solar system was full of rock and ice that the planets
smashed into as they traveled
around the sun. At first these impacts were very intense but over time
the impacts lessened as the asteroids and comets were swept up.
View video: Heaven
and Hell
Slide 10: This is an image of an average moon crater
85 km across, 3 km deep with 2 km mountains in
the center
Slide 11:Some extremely huge craters are also found
on the moon one example is Orientale a Multiringed
basin.
This basin is 2500 km in diameter
Button:
Compare
to Earth
(it's as large as Texas)
Highlighted:
Multi-Ringed
Basin
Slide 12:The surface of the moon is covered by shattered
rocks sometimes fused together by the heat of
the impacts. This type of rock is called Breccia.
Highlighted:
Breccia:
rock
made from the jagged broken pieces of other rocks andMinerals
EX: Show samples of Breccia
Slide 13: Typical highland rock is a type of plagioclase
feldspar.
EX: Feldspar
Slide 14: For the Moon to be made up of layers of different
types of rock it must have once been molten that allowed the rocks to seperate
by density.
Highlighted: Magma Ocean: 4.5 Billion
years ago it was molten 4.4 Billion years ago solid crust started forming
creating the early highlands
Magma
Lava
Slide 15:Layers seperate by density
Slide 16:After the crust cools magma flooded the low
lying areas forming maria.
Button: Compare to Earth
Slide 17: Formation of Maria starts with a meteor impact.
Slide 18: cracks in the crust allow Maria to flow to
the surface filling low areas.
Slide 19: Rilles:
rilles
are stream like valleys on the moon.
Does the moon have water to form valleys?
What could flow on the surface and cause valleys?
Highlighted: Rilles:
note the lunar
dune buggy
Highlighted: Lava Flows
Button: Compare to Earth
Slide 20:Rilles ended up
being about 3 billion years old. 1.4 billion years younger than the highlands.
Rilles formed at about the same time as the maria.
Button: Compare to Earth:
rilles
are formed from channels or rivers of lava or possible
collapsed lava channels
Slide 21: Basalt vesicles. Forms like bubbles in root
beer.
Slide 22: Pyroclastic : pyro=fire,
clastic=broken
Highlighted: pyroclastic
Button: compare to Earth
Slide 23: The soil is made of frozen droplets of lava
Slide 24: the orange droplets contain high amounts of
titanium
Slide 25: Highlighted:
Cinder
cones form from pyroclastic eruptions
Highlighted: Compare to Earth
Slide 26: Wrinkle Ridges: Tectonic
features caused by the cooling of the Moon's crust.
Highlighted: Wrinkle Ridges
Slide 27: Highlighted:
Landslides:
gravity
pulls material downward.
Highlighted: Falls:
occur at the
base of cliffs
Highlighted: Flows:
flow across
large flat areas on water or air.
Highlighted:Slides:
large
sections of slope move down hill and pile up at the base of the slope
Slide 28: Large flows occur on the
moon and travel over many kilometers
Highlighted: Compare to Earth. Giant flows kilometers long
Slide 29: The Structure of the Moon
Crust: made of Feldspar
Mare: Basalt
Mantle: Olivine and Pyroxene (Minerals in Basalt)
Core: Possibly Metallic
Slide 30: Moon Formation
Slide 31: Formation demonstration of a major impact forming
the moon.
Slide 32: The combining of metallic cores on Earth.
Slide 33: Summary
-
Giant Impact
-
Ocean of Magma
-
Light feldspar crust forms
-
Period of impacts
-
Large multi-ringed basins
-
Maria forms
-
No wind or water erosion
-
Light tectonic features from cooling
-
Landslides form gravity
Slide 34: Quiz
Section 1-4 Teaching Outline
Book J
Earth Science
Earth’s Moon pp. 39-44
Activating Prior Knowledge
Hold up a rock.
Have them imagine that this rock was the size of a large
building moving through space
Have them imagine it coming through earths atmosphere
and hitting the earth.
What do you think would happen?
Anticipatory Set
Discover: Why do craters look diferent
from each other?
Items Used: Sand and 3 different size objects.
Procedure:
See steps on page 39J
Assign Reading
Guide for Reading
-
Reading Question "What features
of the moon can be seen with a telescope?
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" How did the Apollo landings help
scientists learn about the moon?
Reading Tip
-
As you read write down ways the moon’s surface is similar
to the earth’s.
Presentation
-
Would you want to vacation on the moon?
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Consider that temperatures range from 100
degrees Celsius, to –170 degrees Celsius
-
There is no air
-
Space suits weigh over 90 kilograms
or nearly 190 lbs
-
Gravity is only 1/6 that of earth (divide
your weight by 6)
-
So astronauts could leap higher than basketball players even
with space suits.
-
Would you still want to travel there?
The Structure and Origin of the Moon
-
When scientists measured the size of the moon they found
that it was about ¼ the size of the earth.
-
When they measure the gravity of the moon they find it is
1/6 that of earth.
-
Gravity depends on the density and mass of an object. If
two o\bjects are the same size and one has less gravity it is less dense.
-
This told scientists that the moon is made up of lighter
or less dense rock similar to the rock on the crust of the earth.
-
The moon didn’t have as much of an Iron core as the earth
did.
-
Could the Moon be made of the Earth’s
Crust?
-
Many people have wondered how the moon may have formed.
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Was it formed somewhere else and capture?
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Did it form the same time as the earth?
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Was it formed by a collision that blasted of earth which
formed the moon?
-
One clue that gives us a hint is that from testing lunar
racks we find that the moon is about 1 billion years younger that the earth.
-
See figure 19 to discuss the current theory.
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4.5 billion years ago a large object the size of Mars struck
the Earth with a Glancing Blow.
-
This ripped off a large portion of the Earth’s molten crust.
-
The Earth Being molten quickly reformed
-
The blasted part of the earth still molted collected into
a large droplet caught in earth’s gracity.
-
This later became the moon
-
This may explain why the earth does not have a full crust
but a series of small continetal plates that do not completely cover the
earth’s surface, which are made of basically the same material as the moon.
Looking at the Moon from Earth
-
For thousands of years people considered moon and could see
shapes on it’s surface but we didn’t know what they were.
-
Many people thought that the moon was a perfect heavenly
body made by God as a perfect sphere in the heavens.
-
About 400 years ago we finally developed technology that
let us veiw the moon more closely.
-
This device was called a telescope and Galileo Galilei and
italian astronomer in 1609 made one to veiw the moon.
-
With this telescope he could
see the moon wasn’t perfectly smooth but had craters mountains and ridges.
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The round pits were craters some
thousands of miles across.
-
What would these compare to on earth?
Volcanoes
so originally crates were thought to be volcanoes.
-
About 50 years ago scientists concluded that these round
pits may be caused by meteor impacts.
-
Galileo also saw large smooth areas that were darker than
the hills and the mountains. What would they compare
to on earth? Seas
-
Galileo thought the same thing so he called them Maria
a latin word for seas.
-
Mare singular Maria
Plural
(show the globe and name some of the seas. So Galileo
pictured the Moon like earth with seas and continents covered with mountains.)
-
Today we know that they are not seas but large oceans of
frozen lava that poured out on the surface billions of years ago, possibly
from meteor impacts. The
side facing earth has more maria than the side facing away. Why would that
be?
VIDEO. Show Cosmos
Heaven and hell which shows first the tunguska comet impact and
then the meteor impact on the moon.
Missions to the Moon p. 42
-
We have talked about the Space Race between the Russians
and the US in the late 50’s and early 60’s through the 70’s. To show the
Russians who was best we decided to go to the moon.
-
President Kennedy in 1961 gave his famous speech about going
to the moon by the end of the decade read section
to the class
-
Between 1964 and 1972 the US and Soviet Union sent menay
spaceships and probes to the moon to learn more about it.
-
No-one knew what it was like was it
so soft and dusty that spacecraft would be swallowed up by the dust and
sink?
-
The Surveyor spacecraft tested
the surface by landing on the moon and it didn’t sink
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Lunar Orbiter space craft orbited
the moon and photographed it trying to find safe places to land.
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