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Transcript
Minor Bodies of the Solar System
Section 3
Section 3: Satellites of Other Planets
Preview
• Key Ideas
• Moons of Mars
• Moons of Jupiter
• Moons of Saturn
• Moons of Uranus and Neptune
• Pluto’s Moons
• Moons in the Solar System
• Rings of the Gas Giants
Minor Bodies of the Solar System
Section 3
Key Ideas
• Compare the characteristics of the two moons of Mars.
• Describe how volcanoes were discovered on Io.
• Name one distinguishing characteristic of each of the
Galilean moons.
• Compare the characteristics of the rings of Saturn with
the rings of the other outer planets.
Minor Bodies of the Solar System
Section 3
Moons of Mars
• All of the planets in our solar systems except Mercury
and Venus have moons. In addition, Saturn, Jupiter,
Uranus, and Neptune all have rings.
• Mars has two tiny moons named Phobos and Deimos,
which revolve around Mars relatively quickly.
• Phobos and Deimos are irregularly shaped chunks of
rock and are thought to be captured asteroids.
• The surfaces of Phobos and Deimos are dark like maria
on Earth’s moon, and both have many craters.
Minor Bodies of the Solar System
Section 3
Moons of Jupiter
• Galilean moon any one of the four largest satellites of
Jupiter—Io, Europa, Ganymede, and Callisto—that were
discovered by Galileo in 1610
• In addition to the four large moons discovered by
Galileo, scientists have observed dozens of smaller
moons around Jupiter.
• Of Jupiter’s four Galilean moons, three are larger than
Earth’s moon.
Minor Bodies of the Solar System
Section 3
Moons of Jupiter continued
Io
• Io, the innermost of Jupiter’s four Galilean moons, moves inward
and outward in its orbit around Jupiter because of the tidal forces, or
gravitational pull, of the other moons of Jupiter.
• Calculations show the tidal forces cause Io’s surface to move in and
out by 100 m. The friction from this surface flexing results in the
melting of the interior of Io, and leads to volcanism.
• Data gathered from the Galileo spacecraft show that Io has a giant
iron core and may possess a magnetic field.
• Much of what scientists know about Jupiter’s moon comes from the
information gathered by the Galileo spacecraft, which orbited Jupiter
from 1995 to 2003.
Minor Bodies of the Solar System
Section 3
Moons of Jupiter continued
Europa
• Europa is the second closest Galilean moon to Jupiter.
Europa is about the size of Earth’s moon, but is much less
dense.
• Astronomers think that Europa has a rock core that is covered
with a crust of ice that is about 100 km thick.
• Scientists have concluded that an ocean of liquid water may
exists under this blanket of ice.
• If liquid water exists, simple life forms could also exist there.
Minor Bodies of the Solar System
Section 3
Moons of Jupiter continued
Ganymede
• Ganymede is the third Galilean moon from Jupiter and is also the
largest moon in the solar system, even larger than the planet
Mercury.
• Ganymede has a relatively small mass because it is probably
composed mostly of ice mixed with rock.
• The surface of Ganymede has dark, crater-filled areas, and light
areas that may be ridges and valleys.
• Ganymede is the only moon in the solar system that is known to
have its own magnetic field. This magnetic field is completely
surrounded by Jupiter’s much more powerful magnetic field.
Minor Bodies of the Solar System
Section 3
Moons of Jupiter continued
Callisto
• Callisto is the farthest Galilean moon from Jupiter.
• Callisto is similar to Ganymede in size, density, and
composition, except Callisto’s surface is much rougher.
• Callisto is one of the most densely cratered moons in our
solar system.
Minor Bodies of the Solar System
Section 3
Reading check
Name one feature of each of the Galilean moons.
Io’s surface is covered with many active volcanoes.
Europa’s surface is covered by an enormous ice sheet.
Ganymede is the largest moon in the solar system and has
a strong magnetic field. Callisto’s surface is heavily
cratered.
Minor Bodies of the Solar System
Section 3
Moons of Saturn
• Saturn has dozens of moons, most of which are small, icy bodies
that have many craters. Only five moons are fairly large.
Titan
• Saturn’s largest moon is Titan, which has a diameter of over
5,000 km.
• Titan’s has a thick atmosphere composed mainly of nitrogen.
Saturn’s Other Moons
• Saturn’s icy moons resemble Jupiter’s icy Galilean moons.
Enceladus has erupting geysers and so may have underground
water near its surface.
• Saturn’s other smaller moons have irregular shapes. Scientists think
that many of the smallest moons were captured by Saturn’s
gravitational pull.
Minor Bodies of the Solar System
Section 3
Moons of Uranus and Neptune
• Uranus’s four largest moons, Oberon, Titania, Umbriel,
and Ariel, were known by the mid-1800’s.
• A fifth moon, Miranda, was discovered in 1948.
Scientists now know that Uranus has over two dozen
moons.
• Neptune has at least 13 moons. One of these moons,
Triton, revolves around Neptune in a backward, or
retrograde, orbit.
Minor Bodies of the Solar System
Section 3
Pluto’s Moons
• Although Pluto is no longer officially considered a planet, it does
have at least three moons.
• Pluto’s largest moon Charon, is almost half the size of Pluto itself. In
fact, because Pluto and Charon are so similar in mass, they both
orbit a common balance point, or barycenter, that is located between
them.
• Charon completes one orbit around Pluto in 6.4 days, the same
length of time as a day on Pluto. Because of these equal lengths,
Charon stays in the same place in Pluto’s sky.
• Pluto also has two small moons, named Nix and Hydra, which also
orbit the barycenter between Pluto and Charon.
Minor Bodies of the Solar System
Moons in the Solar System
Click below to watch the Visual Concept.
Section 3
Minor Bodies of the Solar System
Section 3
Reading check, continued
Identify two ways Charon is different from other moons.
Charon is almost half the size of the object it orbits.
Charon’s orbital period is the same length as Pluto’s day,
so only one side of Pluto always faces the moon.
Minor Bodies of the Solar System
Section 3
Rings of the Gas Giants
• Saturn’s set of rings was discovered over 300 years ago.
Each of the rings circling Saturn is divided into hundreds of
small ringlets, which are composed of billions of pieces of
rock and ice.
• Scientists think that the rings are the remains of a large
cometlike body that entered Saturn’s system and was ripped
apart by tidal forces.
• Jupiter has a single, thin ring made of microscopic particles
that may have been given off by Io. Uranus also has a dozen
thin rings. Neptune’s relatively small number of rings are
clumpy rather than thin and uniform.