Intro to Our Solar System. Our Solar System Most of the planets in our solar system can be seen...
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Transcript of Intro to Our Solar System. Our Solar System Most of the planets in our solar system can be seen...
Chapter 3: Our Solar System
Intro to Our Solar System
Our Solar System • Most of the planets in our solar system
can be seen without a telescope.
• Uranus and Neptune are the only two too far to see.
• The largest planet is about 10 times larger than Earth across.
Our Solar System
Distances• Astronomers use astronomical units, or
AUs, to measure distance in space.
• 1 AU = distance from Sun to Earth; about 150 million km.
• The first four (inner) planets are relatively close to one another; the outer planets are much more spaced out.
Orbits • More than 99% of the Mass in our
Solar System is the Sun.
• This results in a strong gravitational pull on everything else.
• Each planet (and other objects) orbits the Sun in an elliptical, or oval, shape.
Orbits • All planets orbit in the same direction, and
most other objects do, also.
• Scientists think this is a clue – the solar system formed from a huge cloud of gases and dust; most mass = Sun, the rest clumped together to form planets.
• Not all of them were large enough to planets; resulting in asteroids, comets, and moons.
Chapter 3: Our Solar System
The Inner Planets
Inner Planets • Mercury, Venus, Earth, and Mars
• Called terrestrial planets
• Rocky crust, dense mantles and cores
Processes and Surface Features • They all have layers; the heaviest materials
sank to the center in their collisions and the lightest rose to become crust.
• Four main processes shaped the crust:• Tectonics• Volcanism• Weathering and erosion• Impact cratering
Tectonics • Earth’s crust has tectonic plates that are moved
by convection in the mantle.
• As the plates move, different features (mountains, valleys) are formed.
• The other planets do not have plates, but still are able to move with the mantle.
• Tectonics: process of change in the crust due to motion of material in the mantle.
Volcanism • Occurs when molten rock moves from
the interior to the surface.
• Volcanoes are on Earth, Venus, and Mars.
• When the inside of a planet cools enough, no more molten rock reaches the surface.
Weathering and Erosion• Water and wind are important factors
on Earth.
• Planets without wind still have weathering due to heating and cooling of the surface.
Impact Cratering • When small objects hit a larger object
and leave a resulting indentation.
• Harder to find on Earth
• Easily found on other planets due to less weathering/erosion.
Atmospheres • Mainly formed from volcanic gases.
• Venus, Earth, and Mars have enough gravity to hold in gases like CO2, but lighter gases escaped.
• Earth is mostly nitrogen.
• Can make a planet warmer due to loss of energy
Mercury • Believed to shrink from original size,
creating cliffs. • Large areas of cooled lava. • Several impact craters, suggesting the
surface has not changed much. • Longest cycle of day and night – 3 months
of daylight, 3 months of darkness. • Can get 800+ F during day, and -170 F
during night.
Mercury
Venus • Slightly smaller than Earth. • 8 months to turn once; retrograde
rotation (opposite way than orbit) creates 2 months of daylight and 2 months of darkness.
• Very dense, mostly CO2. • Temp = about 470 F. • Sulfuric acid in atmosphere form thick
clouds.
Mars • About half the size of Earth• Two moons – Deimos and Phobos • Red because of iron/rust • Large valley – Valles Marineris • Large areas of cooled lava; several
volcanoes • Winds up to 300 mph; sand dunes. • Several craters
Mars • Mostly CO2 in atmosphere, but very
low air pressure. • Temps vary from about 60 F in day to -
130 F at night. • Polar caps, mostly made of dry ice. • No liquid water on surface, but there
is frozen water in ground.
Chapter 3: Our Solar System
The Outer Planets
Outer Planets • Jupiter, Saturn, Uranus, and Neptune –
gas giants : mostly made of H, He, and other gases.
• The atmosphere is very thick, almost like a liquid in some places.
• They are all believed to have a large, solid core.
Jupiter • Largest planet • 5.2 AU from Sun• 1 year = 12 Earth years• Fast rotation = fast wind and storms • White clouds made of ammonia; lower
clouds are brown/red and made of chemicals
• Storms form between winds; the largest is the Great Red Spot (100+ years old).
Saturn • Gas particles spread out more,
forming layers of clouds. • Rings: wide, flat zone of small
particles that orbit a planet. • Bright rings made out of water ice
chunks, with moons mixed in. • Axis is tilted at 27 degrees; rings
appear to change b/c of this. • 1 year = almost 30 Earth years.
Uranus and Neptune • Mostly methane, ammonia, and water. • Uranus = blue/green; Neptune = dark
blue – colors are from methane.
Uranus• 1 year = 84 Earth years• Rings and moons around equator • Seems to spin on its side • Scientists think the unusual rotation
was caused from a collision.
Neptune • Sometimes looks white due to
methane clouds• Severe storms, such as the Great Dark
Spot, can be seen in darker shades of blue.
• This storm moved toward the equator, where it is thought that the winds broke up the storm.
Chapter 3: Our Solar System
Other Objects
Pluto • Was once a planet.• Discovered in 1930 • No spacecraft has been close to it. • Has a moon, Charon – they orbit each
other; sometimes called a “double planet”.
• More oval-shaped orbit • 1 year = 248 Earth years
Asteroids • Small, solid, rocky bodies that orbit close to Sun. • Most have irregular shapes• Most between Mars and Jupiter – The Asteroid
Belt • Craters, broken rock, and dust cover them; most
have no atmosphere and no layers, so surfaces don’t change.
• Can hit Earth – 65 mya, a 6 mi asteroid hit Earth and sent dust into the air, most likely changing the temps of Earth and killing off any living organisms.
Comets • Have oval orbits• Have a coma (cloud of material) and a
tail (gets longer closer to the Sun). • Small, icy rock is hard to see without
the parts above. • The tail always points away from the
Sun. • Halley’s Comet – orbits approx. every
75 years; expected to return in 2061.
Meteors & Meteorites • Meteors: Brief streaks of light caused
by hot particles/air in the upper atmosphere. • Usually can see a few/hour in the night
sky. • Usually very quick, only a few seconds.
• Meteorites: space object that reaches Earth’s surface• Usually smooth on the outside from
melting; inside can still be icy.