Our
Moon
Printable
version
March
2, 2000
Announcements
-
HOMEWORK
#3
due next lecture!
-
Midterm
next thursday!
-
Looking
for:
Preview:
Our Moon
-
Surface
features
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Exploration
-
Internal
Structure
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Tides
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Formation
Theories
-
Moon
History
Surface
Features
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Light areas
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heavily cratered
-
highlands
-
more
than 4 billion years old
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Dark areas
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Maria (seas)
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fewer craters
-
about
3.5 billion years old
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water cannot exist on the
surface of the moon
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Cooperative learning experiment:
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150 visible meteor craters
on the earth
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1000s on the moon
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assume constant bombardment
by meteors
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List the surfaces in order
of age
Exploration
of the Moon
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Soviet
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1959--1976 unmanned probes
(Luna series)
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took picures, orbited, landed
and returned
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US
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Early 1960s--1972
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Rangers crashed into
moon
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Lunar obiters mapped
surface
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Surveyors landed
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Apollo manned visits
and return (1969-1972)
Ranger 9 end of mission
Movie
Surveyor 3 receives a
visitor
Apollo 15
Internal
Structure of Moon
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Measured using seismometers
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Possible iron core
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Plastic asthenosphere (analog
outer mantle)
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Solid lithosphere (analog
continental plates)
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crust
Lunar seismometer
Tides
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For of gravity depends on
distance
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One side of the earth feels
moon's pull more than other side
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Loose things move
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Sun helps too
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Cooperative Learning Experiment:
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What phase(s) of the moon
cause the biggest tides?
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Moon feels tides too
-
more moonquakes when earth
tides are biggest (what phase(s)?)
Formation
Theories
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Fission
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moon spun off of protoearth
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moon popped out of pacific
ocean
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Capture
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moon formed separately, wandered
near
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Co-creation
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planetessimal blobs started
rotating around each other, each got bigger
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Collision Ejection
Movie
Moon
History
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Regardless of formation theory
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Measured cratering rate
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Look at craters, craters
in craters, craters in craters in craters....
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Maria formed when lava leaked
into BIG craters
Mare Basalt (lava rock)
Highland rock (4.1 billion
years old)
Summary
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Surface
features
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Moon's
surface is very old compared to Earth's
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Cratered
highlands older than Maria
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Exploration
-
Internal
Structure
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Moonquakes
but no plate tectonics
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Tides
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Formation
Theories
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Moon
History
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Maria
are lava-filled craters
Biosphere
-
Home of all living creatures
on Earth
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3 km deep in crust
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10 km high in troposphere
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Living creature's outputs
have impact on atmosphere
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Plants create oxygen :-)
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CFCs deplete ozone :-(
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Industrial processes create
Carbon dioxide (CO2)
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The greenhouse effect: Carbon
dioxide (CO2) helps trap heat by transmitting UV, reflecting
IR
-
CO2 content increasing
since 1958. What did it do before then?
-
Global warming?
-
These effects may not be
"real." Do you want to take the chance?
Atmospheric CO2
content measured in Hawaii
Average global temperature
temperature change
Biosphere
-
Home of all living creatures
on Earth
-
3 km deep in crust
-
10 km high in troposphere
-
Living creature's outputs
have impact on atmosphere
-
Plants create oxygen :-)
-
CFCs deplete ozone :-(
-
Industrial processes create
Carbon dioxide (CO2)
-
The greenhouse effect: Carbon
dioxide (CO2) helps trap heat by transmitting UV, reflecting
IR
-
CO2 content increasing
since 1958. What did it do before then?
-
Global warming?
-
These effects may not be
"real." Do you want to take the chance?
Atmospheric CO2
content measured in Hawaii
Average global temperature
temperature change