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Chapter 19 Formation of the Solar System 19-1 A Solar System is Born  Solar Nebula  Dust and gas clump together in a huge interstellar cloud  Many light years across  Forms beginnings of a new planetary system 19-1 A Solar System is Born  Solar Nebula  Gravity pulls matter together  All mass has gravity  Clumps get larger and larger and gravity will increase  Pressure pushes apart  As cloud warms up particles move faster  Pressure will push away from gravity 19-1 A Solar System is Born  Solar Nebula  Gravity will overcome pressure and cloud will compress  Beginning stage of a star  Out region will become planets 19-1 A Solar System is Born  Planetesimals to Planets  Planetesimal  When dust collides and sticks together  Building blocks of planets  Grow from microscopic to boulders to planets 19-1 A Solar System is Born  Planetesimals to Planets  Planets  Giant gas planets attract nebula gases in outer regions  Rocky planets don’t grow large and are usually inner planets  Are created by collisions by smaller planetesimals 19-1 A Solar System is Born  Birth of a Star  Pressure becomes so great that hydrogen fusion begins  Point where the sun is born 19-1 A Solar System is Born  Planetary Motion  Rotation  Planets spin on their axis  Causes one part of the planet to face the sun all of the time  Causes day and night 19-1 A Solar System is Born  Planetary Motion  Orbit  Path a planet takes around the sun  Also called revolution  Period of Revolution  Time it takes a planet to go around the sun once 19-1 A Solar System is Born  Planetary Orbits  First introduced by Johannes Kepler in 1601  Kepler’s 1st Law of Motion  Planets do not orbit in circles but orbit in a ellipse  Astronomical unit  AU  150 million km 19-1 A Solar System is Born  Planetary Orbit  Kepler’s 2nd Law  Planets move faster when they are closer to the sun  The planet must move farther around its orbit in the same amount of time 19-1 A Solar System is Born  Kepler’s 3rd Law  Compares the period of a planet’s revolution with its semimajor axis  Proves that knowing the planet’s period of revolution you can calculate the planet’s distance from the sun 19-1 A Solar System is Born  Newton’s Law of Universal Gravitation  States that the force of gravity depends on the product of the masses of the objects divided by the square of the distance between them  The farther you are from something the less gravity will pull on you 19-2 The Sun  Structure  Core  At center of the sun  Where energy is produced  Radius of 200,000 km  Temperature of 15,000,000˚C 19-2 The Sun  Structure  Radiative Zone  Very dense region  About 300,000 km thick  Atoms are so dense it takes millions of years for light to pass through 19-2 The Sun  Structure  Convective Zone  Region about 200,000 km thick  Gases circulate in convection currents  Hot gas rises and cold gas sinks 19-2 The Sun  Structure  Photosphere  Gases get thick enough to see  What we know as the visible surface  Only about 600 km thick 19-2 The Sun  Structure  Chromosphere  Thin region below the corona  Only 3,000 km  Deep, red color that is to faint to see unless there is a total solar eclipse 19-2 The Sun  Structure  Corona  Forms the sun’s outer atmosphere  Can extend outward 10-12 times the diameter  Gases in corona are so thin that it is only visible during total solar eclipse 19-2 The Sun  Energy of the Sun  Nuclear Fusion  The process by which 2 or more nuclei with small masses join together to form a larger nucleus  Produces a lot of energy  Normal nuclei repel each other  Gravity and temp in core overcome the repelling force 19-2 The Sun  Energy of the Sun  Nuclear Fusion  3 Steps  2 H nuclei collide to produce deuterium  Deuterium combines with a H nuclei to produce He-3  2 He-3 atoms combine to form He-4  Energy is released at each step 19-2 The Sun  Sun’s Surface  Sunspots  Cooler, dark spots on the sun  Caused by magnetic fields that slow down the convection zone  Solar Flare  Giant storms on the surface of the sun  Cause the auroras on Earth Chapter 20 A Family of Planets 20-1 The Nine Planets  Inner Planets  Mercury, Venus, Earth, and Mars  Terrestrial Planets  Small, dense, and rocky  Closely spaced 20-1 The Nine Planets  Mercury  Closest to the sun  Distance from sun  3.2 light minutes  Period of Rotation  58 Days and 16 Hours  Period of Revolution  88 Days  Diameter  4,879 km  Density  5.43 g/cm3  Surface Temp  -173˚ – 427˚ C  Surface Gravity  38% of Earth’s 20-1 The Nine Planets  Venus  2nd from the sun  Distance from Sun  6.0 light minutes  Period of Rotation  243 days  Period of Revolution  224 days, 17 hours  Diameter  12,104 km  Density  5.24 g/cm3  Surface Temp  464˚C  Surface Gravity  91% of Earth’s 20-1 The Nine Planets  Venus  Retrograde Rotation  Spins in a clockwise rotation when viewed from the poles  Atmosphere  90 times the pressure of Earth’s  Mostly Carbon Dioxide  Creates a massive greenhouse effect 20-1 The Nine Planets  Earth  Distance from Sun  8.3 light minutes  Period of Rotation  23 hours 56 minutes  Period of Revolution  365 Days 6 hours  Diameter  12,756 km  Density  5.52 g/cm3  Surface Temp  -13˚ C – 37˚ C  Surface Gravity  100% 20-1 The Nine Planets  Mars  4th Planet from Sun  Distance from Sun  12.7 light-minutes  Period of Rotation  24 hours 37 minutes  Period of Revolution  1 year 322 days  Diameter  6,794 km  Density  3.94 g/cm3  Surface Temp  -123 - 37˚C  Surface Gravity  38% of Earth’s 20-1 The Nine Planets  Mars  Atmosphere  Very Thin  Liquid water would boil away  Makes a cold planet 20-1 The Nine Planets  Mars  Water  Only in the form of ice  Evidance shows a past history of liquid water  Dry river beds  Polar ice caps 20-1 The Nine Planets  Mars  Volcanoes  2 large volcanic systems  Olympus Mons  Largest mountain in the solar system  Extinct shield volcano like Hawaii 20-1 The Nine Planets  Jupiter  5th from the Sun  Distance from Sun  43.3 light minutes  Period of Rotation  9 hours 56 minutes  Period of Revolution  11 years 313 days  Diameter  142,984 km  Density  1.33 g/cm3  Temperature  -153˚C  Gravity  236% of Earth’s 20-1 The Nine Planets  Jupiter  Largest Planet  Gas Giant  Very large planets that don’t have any known solid surfaces  Made primarily of H and He  Also has water, methane, and ammonia  Giant Red Spot  Long-lasting storm system  Has a faint ring system 20-1 The Nine Planets  Saturn  6th from the Sun  Distance from Sun  1.3 light hours  Period of Rotation  10 hours 39 minutes  Period of Revolution  29 years 155 days  Diameter  120,536 km  Density  0.69 g/cm3  Temperature  -185˚C  Gravity  92% of Earth’s 20-1 The Nine Planets  Saturn  2nd largest planet  Is believed to be still forming  Made of mostly H and He with traces of methane, ammonia, and ethane  Large ring system  Consist of icy particles ranging from a few cm to several meters 20-1 The Nine Planets  Uranus  7th Planet from the Sun  Distance from the Sun  2.7 light hours  Period of Rotation  17 hours 14 minutes  Period of Revolution  83 years 274 days  Diameter  51,118 km  Density  1.27 g/cm3  Temp  -214˚C  Gravity  89% of Earth’s 20-1 The Nine Planets  Uranus  Atmosphere is mainly H and methane  Is tipped on it’s side  Has a 90 degree tilt  Causes one side of the planet to be exposed to sun light and the other in darkness 20-1 The Nine Planets  Neptune  8th from the sun  Distance from Sun  4.2 light hours  Period of Rotation  16 hours 7 minutes  Period of Revolution  163 years 265 days  Diameter  49,528 km  Density  1.64 g/cm3  Temp  -225˚C  Gravity  112% of Earths 20-1 The Nine Planets  Neptune  Atmosphere is the same as Uranus  Has a very narrow set of rings  Has a Great Dark Spot  Is a major storm just like on Jupitor 20-1 The Nine Planets  Pluto  9th Planet  Distance from Sun  5.5 light hours  Period of Rotation  6 days 9 hours  Period of Revolution  248 years  Diameter  2,390 km  Density  2.05 g/cm3  Surface Temp  -236˚C  Surface Gravity  6% of Earth’s 20-1 The Nine Planets  Pluto  Made of rock and ice with a thin atmosphere of methane  It’s moon (Charon) is over half the planet’s size 20-2 Moons  Satellites  Natural or artificial bodies that revolve around larger bodies like planets  Luna  The moon of the Earth  Surface  Has been dated to 4.6 billion years old 20-2 Moons  Luna  Period of Rotation  27 days 8 hours  Period of Revolution  27 days 8 hours  Diameter  3,476 km  Density  3.34 g/cm3  Surface Temp  -170˚C-134˚C  Surface Gravity  17% of Earths 20-2 Moons  Luna Origins  Formation  Impact  Large body collided with Earth when it was still molten  Ejection  Debris began to revolve around Earth  Formation  Material started to clump to form moon 20-2 Moons  Phases of the Moon  The different appearances of the moon due to changing position  Waxing  The sunlit fraction we can see is getting larger  Waning  The sunlit fraction is getting smaller 20-2 Moons  Luna  Eclipses  Occurs when the shadow of one celestial body falls on another  Lunar  Happens when the Earth comes between the sun and the moon  Solar  Happens when the moon comes between the Earth and the sun 20-3 Small Bodies in the Solar System  Comets  Small body of ice, rock, and cosmic dust loosely packed together  Known as dirty snowballs  Tails  Forms when passing by the sun  Ion Tail  Consists of electrically charged particles  Dust Tail  Melting ice and dirt 20-3 Small Bodies in the Solar System  Comets  Orbits  Ellipse  Ion tail will always point away from the sun 20-3 Small Bodies in the Solar System  Asteroids  Small, rocky bodies in orbit around the sun  Range from a few meters to more than 900 km in diameter  Have irregular shapes  Orbit the sun 20-3 Small Bodies in the Solar System  Asteroids  Asteroid Belt  Where most asteroids are in our solar system  Between Mars and Jupiter 20-3 Small Bodies in the Solar System  Asteroids  Types  Outermost region they are a dark reddish brown to black surface  Organic Material  Middle have dark gray surface  Rich in carbon  Innermost have light gray  Stony or 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