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“Motions” in the Heavens Fixed Stars, Moving Planets • Stars remain in fixed positions with each other – Constellations (groups of stars) • Planets “wander” with respect to stars – Retrograde Motion Aristotelian Geocentrism • Earth is center of Universe – Concentric celestial spheres in which the Sun, Moon, and stars are imbedded like jewels – Unblemished, symmetrical Universe – People don’t fall of the Earth as it moves… – Parallax • Not observed in stars – Did not explain retrograde motion Copernicus, 1530 • Heliocentric – Sun, center of Solar System • Explained retrograde motion Tycho Brahe, Johannes Kepler • Brahe: Mapped positions of known bodies – Could predict where any planet would be seen in near future – Drank himself to death • Kepler: Planets move in elliptical orbits – Brahe’s student – Mathematical formulae to describe motion Galileo vs. Aristotle • “Law of Inertia” and falling off the Earth • The Milky Way as a collection of stars (not a cloud of light) • Jupiter’s Moons vs. Geocentrism Ganymede Io Galileo vs. Aristotle • Sunspots and Lunar Maria – Not “homogenous unblemished bodies” Isaac Newton • Popular myth: Isaac Newton invented gravity • A moving body travels in a straight path unless acted on by an outside force – Gravity between Sun and planets makes for elliptical orbits The Earth-Moon System The Lunar Orbit Phases of the Moon Eclipses VS Red Shift • Works for sound or light – If the object is moving toward you, it will have a higher frequency (waves/s) • Louder (sound) • Bluer (light) – If moving away (lower frequency): • Softer (sound) • Redder (light) The Big Bang Theory • All matter and energy compressed into single inconceivably dense point • Universe expands and thins to form the galaxies and stars • 13.7 billion years old “explosion” Nebular Hypothesis • Origin of solar system traced to rotating clouds of gas + fine dust – 1755, Immanuel Kant – Nebulae (“fog” or “cloud”) – Mostly hydrogen and helium – These two elements make up all but small fraction of Sun Gas and very fine dust particles Temperature rises to millions of degrees Nuclear fusion begins H atoms combine to form Helium sunlight! Some Rocky Bits Are Left • Most rocky bits have been swept away (accreted onto forming planets) • Now, rocky bits that are left are basically trapped due to gravity Asteroid Belt trapped between Mars (4) and Jupiter (5) Asteroid Belt The SS at a glance… • 4.6 billion yrs old • All planets, at first, were composed of gas • Protoplanets closest to sun were hot—gasses moving fast enough to escape gravitational pull of Pplanet • Solar wind—a stream of particles originating from the sun—pushed gasses from inner SS to outer • Terrestrial planets vs. Jovian planets Terrestrial planets Jovian Planets Dwarf Planets The Terrestrial Planets… Mercury • Closest planet to the sun • Smallest planet – radius = 2,400 km • 1 mercury year = 88 earth days • Spins slowly on its axis – One day on mercury = 59 earth days – Insane temp. differences • Side facing sun = 427°C • Far side = - 175°C – Thin He atmosphere – Magnetic field—possibly created by liquid core 1. Solid crust (100-300 km thick) 2. Silicate Mantle (600 km thick) 3. Molten Iron Core (1800 km radius) Mercury Geology • Mariner 10 • Impact craters • Caloris baisn-1550 km wide—impact so powerful, planetary scale effects— weird terrane – Intercrater plains—heavily cratered plains between large impact craters – Smooth plains—similar to lunar mare—lava filled depressions – Compression folds—long, linear folds caused by partial cooling of interior Terrestrial Planets: Venus • 108 million km from sun • Very similar in size to Earth—radius 6052 km • Dense atmosphere of CO2—sulfuric acid clouds • Atmospheric pressure at surface = 92 times that of Earth • One year on Venus = 224 earth days • Spins slowly on axis – One Venusian day = 244 earth days • Mean surface temp = 460°C Radar image of Venus Venus: UV True color photo of Venus Studying Venus • Spacecraft – Russian Venera project • V1 and 2—flyby • V3—crashed into surface • V4—probe—accurate atm temp, pressure, and comp—ran out of power • V5 and V6—crushed by atm pressure • V7—crashed • V8—landed and took temp, atm comp and pressure readings for 50 min • V9 and V10—sent first images of surface—survived only 93 minutes • V11-12—detected electrical storms • V13-14—first color pictures • V15-16--orbiters Studying Venus Cont… • Magellan—1989 – Radar mapped 99% of Venusian surface • Strange observations – Only 1000 pristine impact craters—absence of small (<2km) craters – 167 >Mt. Everest sized shield volcanoes • Pancake domes—caused by mantle plumes – 60% of surface is flat – No evidence of plate tectonics—can explain lack of magnetic field Why is Venus so hot? • Venus and earth probably had similar atmospheres • Closer proximity to sun = higher mean temperatures • Too hot for water to condense • No oceans = no way to remove CO2 from atmosphere • CO2 + water vapor = runaway greenhouse effect • Water vapor boiled off into space Terrestrial Planets: Earth Everyone should now know more about Earth Than any other planet in the Solar system… Terrestrial Planets: Mars • 150 million km from sun • About half the size of earth (3400 km radius) • Cold – Average temp = -56°C – Temps at poles can drop below -120°C • Dry – If you were to condense all water vapor in atmosphere—global layer only 1 mm thick (Earth 3 km) • Thin, CO2 atmosphere • 2 moons – Phobos and Deimos Phobos Deimos Studying Mars • Originally, mars was believed to have oceans – Poor resolution of early telescopes – Human eye predisposed to discerning lines • Viking project—mapped surface – Viking I and II—landers— returned first color photos of surface • Mars Global Surveyor—very successful orbiter— photographed most of the Martian surface • Spirit and Opportunity landers—still operational Geology of Mars • Old heavily cratered plains and young, flat, crater poor volcanic plains • Tharsis bulge--four huge shield volcanoes – Olympus mons—largest volcano in SS (25 km tall, 500 km wide) • Tectonic scheme similar to Venus—dominated by volcanism and mantle plumes – Valles Marineris—a large tectonic crack in the martian crust—caused by cooling of planet and by uplift in Tharsis region-- Wind and Water on Mars? • Liquid water is unstable on the martian surface • Ice caps – Water ice covered by dry ice (CO2) • Permafrost from poles to 60°Latitude • Evidence of large floods – Eastern portion of Valles Marineris • Dust devils • Dust storms Martian dust devils