Chapter 27 – The Planets and the Solar System Page 586 Do you think it is possible to count the...
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Transcript of Chapter 27 – The Planets and the Solar System Page 586 Do you think it is possible to count the...
Chapter 27 – The Planets and the Solar System
Page 586 Do you think it is possible to count the
rings of Saturn? The rings look solid in the image, do
you think they are? What do you think they are made of? What do we know about the planets?
Chapter 27.1
The Inner Planets
Two Planetary Neighborhoods
Inner Planets – Mercury, Venus, Earth, Mars
All have rocky crust Dense mantle layers and cores Because of their Earth like
appearance they are also known as terrestrial planets
Distance Between Planets Outer Planets – Jupiter, Saturn, Uranus,
Neptune and Pluto 1st four are called Jovian – or Jupiter like Very large gaseous planets with no
rocky crust Low density due to size Have ring systems Pluto is an oddball – not dense enough
to be terrestrial; too small to be Jovian
Mercury
Nearest to the Sun Orbits the sun in 88 days Smallest of terrestrials Mercury surface resembles the
moon’s Rotates every 59 days Temperature – day 400°C; night –
200°C
Chapter 27.2
Venus – Earth’s Sister Planet – 2nd planet from the Sun Near each other similar in
diameter, mass and gravity Venus is the only planet to
rotate from east to west Rotates every 243 days Orbits every 225 days Thick yellow clouds make
surface impossible to see
Magellan radar mapped it Fault system Yellow clouds made of sulfuric acid Surface is hot due to greenhouse
effect (CO2) causing surface to be 475°C
Visible from Earth in the morning or early evening – “evening star”
Mars – 4th planet from the Sun
687 day orbit Axis tilted about the same as
earth’s giving it seasons. However they are 2 times as long
Very thin atmosphere (1% of Earth’s) mostly CO2
Has ice caps – thought to be water covered by frozen CO2
Spacecraft have photographed and landed on Mars surface
Largest known volcano in the solar system “Olympus Mons”
Has a valley system suggesting water once ran on its surface
Page 543, 5 Martian landings
Outer Planets
Jovian Planets – Jupiter, Saturn, Uranus and Neptune
Much larger than terrestrials – smallest, Uranus, is 15 times more massive than earth
No solid surfaces – their “surface” is an uppermost gas layer
Composed mainly of light elements H and He
All Jovian planets have ring systems
Jupiter – 5th Planet from the Sun 11.9 year orbit 10 hour rotation Has 2 times more mass than all the other
planets combined Radiates 2 times as much energy back into
space as it receives from the sun Galileo probe entered Jupiter’s atmosphere
in 1995 – found no thick clouds and higher than expected temperatures
Saturn – 6th planet from the Sun
30 year orbit 10 hour rotation Lowest density of all planets,
less than 1 Saturn also radiates more
energy than it receives from the sun, like Jupiter it has internal heat sources
Uranus – 7th planet from the sun
84 year orbit 17.2 hour rotation It’s rotational axis is tipped
almost completely over It’s magnetic field is not tipped
Chapter 27.3
Neptune – 8th planet (most of the time) 165 year orbit Rotation 16.1 hours Neptune was found after
astronomers predicted its location mathematically in 1846
Winds over 2000 km/hr Becomes the 9th planet when Pluto is
taken close to the Sun due to Pluto’s highly elliptical orbit
Pluto
248 year orbit Smallest planet in the Solar
System Its moon, Charon, is ½ its size Most of its atmosphere is
frozen. However, it thaws slightly when it nears the sun
Planetary Satellites (moons)
Satellites of Earth and Mars
Earth has one moon Mars has 2 tiny moons, Deimos
and Phobos Phobos circles mars 3 times a
day Mercury and Venus have no
satellites
Jupiter’s Moons
At least 63 Galilean moons – Io, Europa,
Ganymede and Callisto are the 4 largest discovered by Galileo
Io is geologically active Nine active volcanoes No signs of crater impacts Galileo spacecraft found it has an
iron core surrounded by a molten silicate rock
Heat on Io is caused by tidal forces from Jupiter
Europa Surface is thought to be frozen
water It is thought liquid water may
exist under the ice
Ganymede – the largest Larger than Pluto and Mercury Surface of ice
Callisto – most heavily cratered object in the solar system
Saturn’s Moons
At least 31 moons Largest is Titan
Only moon in solar system to have a substantial atmosphere
Uranus’s Moons
At least 27 5 major moons are Titania,
Oberon, Umbriel, Ariel, and Miranda All lack atmosphere and are
heavily cratered
Neptune’s Moons
At least 13 moons – Triton is the largest
Solar System Debris
Comets and TNOs (Trans Neptune Objects)
Comets described as dirty snowballs Spend most of their time beyond
the orbit of Neptune Do not become visible until they
travel inside Jupiter’s orbit
Has 2 parts, nucleus and tail Tail always points away from the
sun due to solar winds Most famous comet is Halley’s, it
appears once every 76 years – last visit 1986
Asteroids – solid rocklike masses
Uneven surface causes their brightness to change
Revolve same direction as planets
Most in asteroid belt between Mars and Jupiter
Meteors and Meteoroids
Meteoroid – rock or ice fragment traveling in space, they differ from asteroids in that they are smaller in size
Meteor – when a meteoroid enters earth’s atmosphere and burns up “shooting star”
Meteor shower – occurs when earth passes into debris left by a comet that crossed earth’s path – very predictable, named after the constellation in the background.
Chapter 27.4
Meteorite A large meteoroid that survives earth’s
atmosphere and strikes its surface 3 types
Stony – resemble earth’s rocks, mostly made of silicates
95% Irons – mostly iron
5% Stony irons
<1% Most found in the ice of Antarctica
Impact Craters – bowl shaped depressions that remain after a meteor or other object strikes earth
Rare on earth because The atmosphere burns up most
meteoroids Earth is geologically active
Best known is Barringer Meteor Crater in AZ