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The Moon & Mercury – Dead Worlds
Outline ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Bulk Physical Properties ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
 
Magnetic Field - Moon ,[object Object],[object Object],[object Object],[object Object]
 
Magnetic Field - Mercury ,[object Object],[object Object],[object Object]
 
Inferences ,[object Object],[object Object]
Orbit – the Moon ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
[object Object],What does this imply about the structure of the moon’s interior? Both orbital and rotational periods are 27.3 days.
Orbit - Mercury ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Resonance ,[object Object],[object Object]
Orbital Period 88 days. Rotational Period: 59 days
Interior - Moon ,[object Object],[object Object],[object Object],[object Object],[object Object]
 
 
Moon’s Interior (2) ,[object Object],[object Object]
Mercury’s Interior ,[object Object],[object Object],[object Object]
 
Surface Conditions - Moon ,[object Object],[object Object],[object Object],[object Object],[object Object]
Moon’s Surface Conditions (2) ,[object Object],[object Object],[object Object]
 
Surface Conditions - Mercury ,[object Object],[object Object],[object Object]
Mercury Surface Conditions (2) ,[object Object],[object Object],[object Object]
Lunar surface features ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Craters – how do they form?
Meteorite begins to vaporize on impact
It’s the  expanding vapor , not the impact,  that forms the crater.  That’s why craters are round, even if the meteorite impacts from a low angle.
Crater rims are raised above the surroundings. Rebound of the rock under the impact can form a central peak.  Over time, the crater walls can slump, creating terraces.
 
Some craters have rays, or a blanket of material thrown out by the impact.
What do the rays indicate about the age of the crater and the energy of the impact?
Sometimes craters are formed in long chains
 
Lunar Highlands ,[object Object],[object Object],That the highlands are older than the lower, smoother regions.  They were formed 4.6 – 3.8 billion years ago.
What rock are the highlands made of? Anorthosite, a close  relative  of granite.
When did the cratering happen? ,[object Object],[object Object]
 
Lunar Maria – just big craters? ,[object Object],[object Object],[object Object]
 
 
 
 
 
Mare – singular Maria - plural No plate tectonics, but mountains form at edges of maria.
Features on the maria ,[object Object],[object Object],[object Object]
Chocolate pudding will do the same thing, if left on the countertop too long.
Rilles ,[object Object],[object Object],Rilles  were  formed by a flowing material, but it wasn’t water – it was lava. How do we know?
 
[object Object],[object Object],[object Object]
An active rille on earth.
The Apollo 15 landing was made near the famous Hadley rille.
Apollo 15 rover in front of Hadley rille.
Erosion on the moon ,[object Object],Two things contribute to erosion on the moon: the drastic changes in temperature, and meteorite impacts.
[object Object],[object Object]
Recent craters have sharp walls with little slumping Inside.
Older craters have poorly defined walls with lots of slumping.
Lunar soil is very powdery, even slippery. Why would it be slippery?
Lunar soil is composed of tiny glass spheres and broken fragments.
[object Object],[object Object]
Lunar rock fragments melted into a breccia.
Impacts are still continuing today, but they’re mostly micro-meteorites, like this one.
Mercury’s Surface Features ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
 
 
antipode
 
But then again… ,[object Object],[object Object],[object Object],[object Object]
Missions to the Moon ,[object Object],[object Object],[object Object],[object Object],[object Object]
Missions to the Moon (2) ,[object Object],[object Object],[object Object]
 
Missions to the Moon (3) ,[object Object],[object Object]
Mission to Mercury ,[object Object],[object Object]
 
http://nssdc.gsfc.nasa.gov/image/planetary/mercury/mercuryglobe2.jpg http://www.pa.msu.edu/people/frenchj/moon/moon-16day-2723.jpg http://nssdc.gsfc.nasa.gov/planetary/factsheet/moonfact.html http://nssdc.gsfc.nasa.gov/planetary/factsheet/mercuryfact.html http://www.freemars.org/jeff/planets/Luna/Luna.htm http://www.adlerplanetarium.org/cyberspace/planets/mercury/images/scale1.jpg http://www.astronomy.org/programs/moon/earth-moon-mass.gif http://www.psrd.hawaii.edu/Sept99/MoonCore.html http://ase.tufts.edu/cosmos/view_picture.asp?id=393 http://ccmc.gsfc.nasa.gov/educational/MagnetosphereWebPage.htm http://ase.tufts.edu/cosmos/view_picture.asp?id=385 http://www.sckans.edu/~gangwere/LAS170a2/_27.html http://www.windows.ucar.edu/tour/link=/mercury/News_and_Discovery/Merc_orbit_reson.html
http://www.astro.psu.edu/users/niel/astro1/slideshows/class41/slides-41.html http://www.mhhe.com/physsci/astronomy/fix/student/chapter9/09f27.html http://zebu.uoregon.edu/~imamura/121/nov10/nov10.html http://btc.montana.edu/messenger/instruments/MercuryCore.gif http://www.pennastroimaging.com/Lunar+Planetary%20Images.htm http://starchild.gsfc.nasa.gov/docs/StarChild/space_level2/apollo11_lem.html

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moon and mercury