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Earth Physical Strat
• Lithosphere (Brittle)
o Crust, Upper Mantle
• Athenosphere (ductile)
• Mantle (Solid, but convecting)
• Outer Core (liquid)
• Inner Core (Core)
Exosphere
Thermosphere
Mesosphere
Stratosphere
Troposphere
Earth Compositional Strat
• Crust (Silicate rock)
o Oceanic - mafic
o Continental - felsic
• Mantle (Silicate rock)
o Ultramafic
• Core (metal)
o Fe - 96%
o Ni - some nickel something else (O, S)
Moon
Diameter ~1/4Earth’s
Mass ~ 1% Earth’s
Orbits ~ 30Earth Diameters
Mean Surface Temperature
No global Magnetic Field
Not Atmosphere
Impact Craters
From Asteroids and Comets
Highlands
Older and Brighter
Lots of craters
Mountains (rupes)
Magma ocean
Supported physically- heavy silicate minerals sink, light minerals float
Supported compositionally - europium anomaly, substituted for CA
Mare (Maria)
Younger and Darker
Fewer crater
Maria has fewer craters than the lunar highlands, so it is not so exposed to impacts.
Suggests that impacts are related
Regolith
Impact debris
House-size boulders down to dust
Footprints left in regolith (very fine)
Capture Theory
random flew too close and got trapped by gravitational dynamics ( not good, the moon is too similar to Earth for it to be random and get trapped)
Fission Theory
Earth spins so fast that it spins off a blob to be a moon (composition it could be, volatile don't match, dynamically it doesn't match)
Giant Impact
Nearly fully formed proto-earth hit by a Mars-sized impactor (Thea), iron core of Thea merges with earth, rocky mantle of earth and Thea form the moon ~40- 60million years into SS
Best theory because very consistent throughout the solar system, satisfies dynamical observation, and provides heat for the magma ocean.
New Moon
moon and sun are on the same side of Earth (Conjunction). Best time to observe objects in the night sky
Full Moon
moon and sun are on opposite sides of Earth, rise at sunset, set at sunrise, highest at midnight
First Quarter Moon
moon and sun are 90 degrees apart (after new moon), rise at noon, set at midnight, highest at sunset
Gibbous and crescent moon
between the 1st and 3rd quarter phases
Third Quarter Moon
Moon and sun are 90 apart (after full moon), highest at sunrise • Waxing (increasing) - after New Moon and before Full Moon, more illuminated side
Waning (decreasing)
after full moon and before New Moon, less illuminated side
Restoring force
force acting to bring a body to its equilibrium, acts until synchronous rotation is achieved
Off-axis
tidal bulge allows for transfer of momentum from Earth's rotation to the Moon's orbital motion, confirming that the Moon is spiraling away from Earth about 4 cm per year
Umra
Full Shadow region, the entire sun is blocked
Penumra
Partial shadow region, part of the sun is blocked
Lunar Eclipse
Moon is in Earth’s shadow
Occurs when Earth shades the moon, only during a full moon, total (moon entirely within umra), partial (moon particular within umra)
Solar Eclipse
Earth is in the Moon’s shadow
Occurs when the moon passes in front of the sun, only during a new moon, total (Earth passes through the umbra), Partial (Earth passes through the penumbra), Annular (Earth passes beyond the umbra)
Reddening of the moon
caused by sunlight refracting through the Earth’s atmosphere
Catastrophism
the theory that the earth has largely been shaped by sudden, short-lived, violent events, possibly worldwide in catastrophe
Uniformitarianism
holds that slow, incremental changes, such as tectonic uplift and erosion, created all the Earth’s geological features.
Impactor
(bolide) - Mass, Velocity
Target Body
Size (mass) ‘gravity well”
Compositional
Atmosphere
Total Mechanical Energy
Kinetic Energy = Potential Energy
Kinetic Energy: ½ Mass Velocity^2
Impact Crater
Release of large amounts of energy
Initial Explosion
lots of energy is used to break, melt, vaporize materials,
Very fast (a few seconds to a few minutes)
Very high temperature
Crater Excavation
initial “hole” collapse and forms the final crater we see
Collapse: relatively fast (a few seconds to minutes)
Crater degradation: very long (millions of years)
Simple Crater
Energy Release vs. gravity vs. cohesion
Slopes are much steeper
Depth-to-width ratios and melt components are quite different
Complex Crater
Internal structures present ( peaks and rings)
Geologic Evidence of Impact
breccia and mega breccia
Pseudotachylite
Shatter cones and shocked materials
Melt sheets
Tektites
K/T Geologic boundary
K/T Geologic boundary
End-Cretaceous extinction
1st major stratigraphic boundary identified
Iridium anomaly discovered
Earth’s crust is depleted in Ir & asteroids are enriched in Ir
Heat pulse and global fires
Saturation
Densities reach maximum when each new crater destroys one old crater
Equilibrium
New crater wipes out an equal number of old ones
Production population
theorized size-frequency distribution of all primary
Geometric saturation
hexagonal close packing
Lunar crater densities
can be compared with measured surface ages from samples.
Crater size-frequency plots
can be used to infer the geological history of the surfaces
geological processes(erosion, sedimentation)
will remove smaller craters more rapidly than larger ones, so the surface tends to look younger at small scales rather than at large scales
Secondary craters
can seriously complicate the cratering record; the surface may be buried and then exhumed, giving misleading dates
Obliquity
Tilt of a planet's spin axis relative to the plane of its orbit around the sun, Causes seasons - March 21 (Spring equinox), Dec 21 (Winter Solstice), June 21 (Summer Solstice), Sept 23 (Fall Equinox) , 23.4°
Lunar Orbital Inclination
5.14°
Lunar Obliquity to ecliptic
1.54°
Lunar Obliquity
6.68°
As the moon orbits Earth
different fractions of the illuminated side show day and night
Day and Month on Earth
The moon is 1:1 synchronous rotation/revolution, meaning it spins once it makes one revolution around the Earth
Day and Night on the moon
daylight for 2 weeks, and then nights for about 2 weeks
Sidereal Month
One orbit around Earth with respect to stars, 27.3 days
Synodic Month
One orbits around Earth with respect to the sun in 29.5 days
energies associated with planetary heat engines
Accretion, Differentiation, Radioactive Decay
energies associated with planetary cooling mechanisms.
Conduction, convection, advection, radiation
Simple vs Complex Crater
depend on the composition of both the target and the impact, location closeness to the sun, the fewer components of the body, the less it's gonna decrease