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Organization  Our Solar System consists of: Comets orbiting the Sun Asteroids orbiting the Sun Planets orbiting the Sun ○ Moons orbiting the planets.

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Presentation on theme: "Organization  Our Solar System consists of: Comets orbiting the Sun Asteroids orbiting the Sun Planets orbiting the Sun ○ Moons orbiting the planets."— Presentation transcript:

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2 Organization  Our Solar System consists of: Comets orbiting the Sun Asteroids orbiting the Sun Planets orbiting the Sun ○ Moons orbiting the planets Dwarf Planets orbiting the Sun

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5 Planets  Planets form 3 main groups Inner Planets (Terrestrial) Outer Planets (Jovian) Dwarf Planets  Separating the Inner from Outer is the Asteroid Belt Between Mars/Jupiter

6 Inner Planets (Terrestrial)  Mercury, Venus, Earth, Mars Small in size Rocky surfaces Few or no moons No ring systems

7 Mercury  1/3 the size of Earth  Very eccentric orbit  Very slow rotation It rotates 1and1/2 times each year  Basically no atmosphere  Temp. ranges from -173C to 427C -279F to 801F  No moons

8 Venus  Similar to Earth in mass, diameter and density  Very thick atmosphere  Has a slow rotation that is backwards compared to most of the planets  Day is longer than a year  Avg. temp is 464C Roughly 900F  No moons

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10 Earth

11 Mars  Smaller than Earth  Thin atmosphere  Large volcanoes on the surface  Enormous canyons  Ice caps of CO 2 at the poles with most likely water underneath  2 moons (Phobos, Deimos)  Seasons / 24 hour day  -133C to 27C  -207F to 80F  Avg. -55C -67F

12 Olympus Mons

13 Valles Marineris

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15 The Martian Surface  Has key chemical ingredients for life S,N,H,O,P,C (methane?)  Clay minerals and surface features indicate a once aqueous environment  Groundwater beneath  Volcanism, wind, impacting objects affect the surface the most

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17 Outer Planets (Jovian)  Jupiter, Saturn, Uranus, Neptune  Large in size  Gaseous surfaces  Many moons  Have a ring system

18 Jupiter  Largest planet  Banded system of clouds Over 200 mi/h  Composed of hydrogen/helium  More than 60 moons  Fast rotation Less than 10 hours

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21 Saturn  Similar to Jupiter in structure  Saturn’s rings Pieces of ice that range from microscopic to house-sized Formed from destroyed moons or leftover material from the formation of Saturn  More than 60 moons

22 Uranus  Blue appearance from methane gas in the atmosphere  Has a 90 degree tilt Maybe from a collision or gravitational influence from a large moon that passed by  At least 27 moons

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24 Neptune  Similar structure as Uranus  Distinctive clouds  Once had The Great Dark Spot  14 moons

25 Moons of the Planets

26 Moons  Moons orbit the planets directly rather than the sun.  Some moons may be larger than planets, but since they don’t directly orbit the sun, they are not considered planets

27 Moons of Mars  Phobos  Deimos  Irregularly shaped  Most likely captured asteroids due to Mars’ proximity to the Asteroid Belt

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29 Moons of Jupiter  More than 60  4 Biggest: Mainly ice and rock Io- volcanically active Ganymede Europa- may have a subsurface ocean Callisto

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31 Moons of Saturn  More than 60  Titan being the largest moon in the solar system Has an atmosphere made of nitrogen and methane

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33 Moons of Uranus  At least 27  Miranda is a unique moon Unusual criss-crossing marks across the surface

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35 Moons of Neptune  At least 13  Triton being the largest of the 13 Retrograde orbit Nitrogen geysers

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37 Comets

38  Small, icy bodies (1-10km diameter)  Some are found beyond Neptune Kuiper Belt  Mainly found beyond Pluto in the Solar System Oort Cloud  Occasionally can be sent towards the inner parts of the Solar System Highly eccentric orbit

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41 Parts  Nucleus- solid portion Ice/Rock  Coma – gases surrounding nucleus  Tail- part of the coma pushed away due to solar wind

42 Meteor Shower

43 Origin of Meteor Showers

44 List of Meteor Showers

45 Next Sightings  Comet P Comet P  Current List Current List  Magnitude Magnitude

46 Eugene Shoemaker

47 Shoemaker-Levy 9

48 Asteroids

49  Small bodies of rock  Mainly found between Mars and Jupiter  Occasionally the collide, break, and head towards Earth as Meteoroids. Meteor- In atmosphere Meteorite- On land in Earth

50 Meteor Crater, Arizona

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52 Our Moon

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59 Properties of the Moon  Mainly volcanic rock  No atmosphere Extreme temperatures No wind or weather No sound  Heavily cratered

60 Lunar Surface  The surface is composed of light and dark colored rocks Lunar Highlands Lunar Maria

61 Lunar Highlands  Heavily Cratered  Light in Color  Mountainous

62 Lunar Maria  Lunar “seas”  Smooth and flat  Dark in color Basalts  Few craters

63 Other Features  Impact Craters  Rays  Rilles

64 Impact Craters and Rays

65 Rilles  Originally thought to be dried up rivers  Now believed to be collapsed lava tubes

66 Formation of the Moon  Moon is believed to have been hit by a Mars sized object early in Earth’s formation.  This caused enough Earth material to be blasted from the surface that eventually formed the Moon.

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71 Phases of the Moon

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73 Tides

74 Causes  The Moon and Sun both have a gravitational effect on the Earth  The solid Earth gets pulled slightly in the direction of those bodies in space  This creates a bulge of water on the sides facing towards and away from the Moon.

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77 Eclipses

78 Types  Lunar  Solar  Annular

79 Lunar  When the Moon crosses into the shadow of the Earth

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81 Solar  When the Moon’s shadow is cast upon the Earth

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83 Annular  When the Moon casts a shadow on the Earth, but the shadow doesn’t quite reach the Earth

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