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Earth and Moon Statistics http://solarsystem.nasa.gov/multimedia/gallery/Earth_Mo By the Lunar and Planetary Institute For use in teacher workshops
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Earth and Moon Statistics By the Lunar and Planetary Institute For use in teacher workshops.

Dec 22, 2015

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Page 1: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Earth and Moon

Statistics

http://solarsystem.nasa.gov/multimedia/gallery/Earth_Moon.jpg

By the Lunar and Planetary Institute

For use in teacher workshops

Page 2: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Earth’s MoonWhat’s the Moon like?

What do people see when they look at the Moon?

http://photojournal.jpl.nasa.gov/catalog/PIA00094

Page 3: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

http://www.lpi.usra.edu/resources/mapcatalog/LandingSite/index.html

Page 4: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

http://solarsystem.nasa.gov/multimedia/display.cfm?IM_ID=1757

How Big is the Moon?

Page 5: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Moon Size

~ 1/4 width of Earth

Radius of 1080 miles

Gravity ~1/6 of Earth’s

http://grin.hq.nasa.gov/IMAGES/SMALL/GPN-2000-001444.jpg

Page 6: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Relative Size and Distance of Earth and Moon?

http://nix.ksc.nasa.gov/info;jsessionid=gfuzp418gewa?id=C-1979-00910&orgid=2

Page 7: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

http://visibleearth.nasa.gov/view_rec.php?id=1624

Earth and Moon to Scale

If Earth were a basketball, then the Moon would be a

tennis ball,

23.5 feet away

Page 8: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Moon Stats No light of its own!!

Page 9: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Moon Rotation

Spins on axis (rotates) once every 27.3 days

Tilted ~7 degrees (Earth = 23.5)

Page 10: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Moon’s Orbit Orbits (revolves around) Earth every 27.3 days

Elliptical orbit (not a perfect circle)

360,000 km 406,000 km 224,000 miles 252,000 miles

http://solarsystem.nasa.gov/multimedia/display.cfm?IM_ID=442

Page 11: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

The Near Side The Moon rotates in 27.3 days.

The Moon orbits Earth in 27.3 days.

Because the Moon rotates and revolves at the same rate, we only see one side The NEAR side

There is NO DARK SIDE

There is a FAR side….

Page 12: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

And the Backside!

The FAR side

http://photojournal.jpl.nasa.gov/catalog/PIA00304

Page 13: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Phases of the Moon

Page 14: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Solar Elcipse

Page 15: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.
Page 16: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Moon Stats Moon’s orbit around Earth is inclined about 5 degrees to Earth’s plane of orbit around the Sun

Ecliptic plane

Sun EarthMoon

Moon’s orbital plane

Image created by LPI staff

Page 17: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

The Five Major Theories of Formation of the Earth’s Moon

Page 18: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Evidence supporting the Co-accretion Theory

• States that the earth and the moon accreted at the same time out of the same nebular material

• In this theory, the proto-moon drew material out of the same nebular cloud as the earth in the same relative location as result, the two should be very similar in composition

• Why it doesn’t work: The co-formation theory explains why the moon is located in its current location, but cannot explain the evidence that the earth and moon are composed of different materials.

Page 19: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Co-accretion Image

Page 20: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Did the moon form by Fission?

•Theory proposed by Darwin•Based on fast-spinning primordial earth•Earth spun and flattened so quickly that it ejected a large piece of material, which eventually became the moon

•Strengths: Isotopic ratio and Iron content similarities between Earth and Moon are explained

•Flaws: Energy needed to cause loss of the material not supported by present day spinning of the earth

Page 21: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

The Capture Theory

• Ring of dust around the earth slows the moon, which has already formed, allowing it to be captured into the earth’s gravitational field.

Page 22: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Capture Theory Continued…

• The Capture theory postulates that the moon was formed at another place and time in the solar system and while passing by the earth, it was pulled into the earth’s gravitational field.

• Reasonable hypothesis because many moons surrounding other planets are actually captured asteroids and not objects that formed in place with the mother planet. A moon that is captured would most likely have a non-spherical shape. Ex. Phobos and Deimos, the moons of Mars

Page 23: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

The Moons of Mars (captured satellites)

Page 24: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Why the Capture theory does not work

• indicator that a moon has been captured would be if it orbited in a direction that differed from that of the mother planet, but our moon is rounded in shape and orbits the earth, the capture theory does not hold up.

• The only piece of evidence supported by the capture theory is the difference in composition between the earth and the moon.

Page 25: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

The Colliding Planetesimals Theory

• Hypothesizes that the moon condensed from the debris of planetesimaly sized objects that collided during the formation of the solar system

• Limited evidence to support this theory.

• Current lunar mission is studying this theory.

Page 26: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

The One that Works!

The Collision-Ejection Theory aka: The Giant Impactor Theory

Page 27: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

What this theory is all about

• hypothesizes that the moon was formed when a planetesimal the size of mars struck the earth, thereby ejected large volumes of matter from the earth.

• disk of orbiting material ejected from the collision eventually condensed to form our moon in its orbit around the Earth.

Page 28: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Origin of the Theory

• The theory was proposed in the mid-1970’s, but was rejected by many scientists until 1984 when a conference evaluating the validity of theories of the moon left no doubt that the collision theory was the most likely possibility

• New models of planet formation had suggested that giant impacts were not at all uncommon during the late stages of terrestrial planet formation.

Page 29: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Collision Theory Images

Page 30: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.
Page 31: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Why this theory works

Page 32: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Explains the Lack of volatiles on the Moon’s

surface• In order to explain the lack of volatiles on the moon, we would need an event which created a heat so high that all would have been vaporized. If an object the size of Mars were to collide with the forming Earth, the heat produced by this collision would provide a reasonable explanation as to why the moon’s surface characteristics imply that it has been ‘baked’ more than the earth.

Page 33: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

The Iron Core of the Moon explained

• moon is also thought to contain a small iron core

• The collision theory states that the moon would be able to retain the iron core even through the collision.

• The earth’s Iron core had already undergone gravitational differentiation at the time of the impact, therefore, the debris ejected from the earth consisted of material from the iron depleted rocky mantle.

Page 34: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Supports similarities in Oxygen isotopic ratios

• The earth and the moon have exactly the same oxygen isotope composition while rocks and meteorites from different areas of the solar system have differing ratios.

• The similarity in isotopic ratios supports the belief that the moon formed from material in the earth’s vicinity.

Page 35: Earth and Moon Statistics  By the Lunar and Planetary Institute For use in teacher workshops.

Ultimate Fate of the Moon

• The Moon is gradually receding from the Earth into a higher orbit

• Calculations suggest that this will continue for about fifty billion years.

• By that time, the Earth and Moon will become caught up in what is called a "spin–orbit resonance" in which the Moon will circle the Earth in about 47 days (currently 29 days),

• Both the Moon and Earth will rotate around their axes in the same time, always facing each other with the same side.

• Beyond this, it is hard to tell what will happen to the Earth–Moon system, considering that the Sun is expected to become a red giant approximately 5 billion years from now.