|
Our Solar System
Our solar system consists of various bodies
of different sizes which orbit the sun. The planets are the most important
of these orbiting objects, and are arrayed in this order (first is closest
to the sun): Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune,
Pluto. |
|
|
The SUN, which is actually just
an ordinary star, lies at the center of our solar system. What makes the sun
so special to us is simply the fact that it is so close to the Earth, only
93 million (92,960,000) miles away. This distance may seem huge, but when
you realize that the closest star to us besides the sun is 25.3 trillion (25,300,000,000,000)
miles away, you can see how giant space really is. Besides the obvious effects
the sun has on our lives, solar activity also contributes to weather patterns
on Earth. For instance, between the years 1640 and 1710, there were almost
no sunspots on the surface of the sun. This coincided with a period of very
cold weather on Earth known as the "Little Ice Age." Solar eclipses are particularly
fascinating to watch. During a solar eclipse, the moon, the Earth, and the
sun line up so that the moon lies between the sun and Earth. From our point
of view on Earth, the sun is blocked completely by the moon for a few minutes.
Another beautiful sight visible from Earth are the aurorae, or northern lights.
These brightly colored bands usually appear in the sky in locations near the
north and south poles. The bright colors occur when high-energy particles
from the sun are swept into our atmosphere and make the atoms there glow.
The sun gets its energy from nuclear fusion, which is a nuclear process where
four hydrogen atoms are converted into one helium atom. Since the total atomic
mass of four hydrogen atoms is 0.7 percent more than the atomic mass of the
helium atom, there is a little bit of extra mass left over at the end of this
conversion process. In his famous E = mc^2 equation, Einstein proved that
mass and energy are transferable. The extra mass created in the nuclear process
described above is converted into energy. This nuclear fusion occurs in the
central core of the sun, where the temperature is about 15 million degrees
Fahrenheit and the pressure is 250 billion times the pressure of the Earth's
atmosphere. |
|
|
|
MERCURY is the closest planet
to the sun, and so it is also the fastest moving, orbiting the sun at 107,136
mph. This fast speed led the Romans to name it after Mercury, who was the
speedy messenger of the Roman gods. Since Mercury is so close to the sun,
it is difficult to see from Earth. It is visible only right after sunset or
right before sunrise. Mercury has no moons. Nearly 4,000 of the best photographs
of Mercury were taken by the Mariner 10 space mission in 1974. Those pictures
show that Mercury is a small rock that resembles the moon. However, it has
long cliffs and shallow craters instead of the deep craters found on the moon.
At the center of the planet is a large iron core. One year on Mercury is only
88 Earth days long, while one day on Mercury is equal to 59 days on Earth!
This means that since Mercury has no atmosphere, and the sun shines continuously
on the surface for 59 Earth days in a row, the daytime temperatures on Mercury
can reach as high as 800 degrees Fahrenheit, under which conditions even metals
such as lead would be melted! When it is nighttime on the surface, the temperature
is -250 degrees Fahrenheit! |
|
|
|
VENUS is the closest planet to
Earth, and is the third brightest object in our sky after the sun and moon.
Although it is similar to our planet in size, mass, and density, its surface
environment is quite different. The atmosphere is made up of 96% carbon dioxide
and small amounts of acids. One feature of the atmosphere is the greenhouse
effect, in which heat (infrared radiation) is trapped near the surface because
it gets reflected back down by the clouds. Venus is therefore very hot, approximately
900 degrees Fahrenheit. The surface has been studied by the Pioneer Venus
1 and Magellan spacecrafts, which used radar to peer through the clouds and
make maps. They found that most of the surface is covered by craters and hills.
There are also indications that Venus had a lot of volcanic activity in the
past. The atmospheric pressure at the surface is 90 times Earth's pressure!
Venus does not have any moons. |
|
|
|
Our planet, EARTH, is very unique.
The environment is rich enough to support life, and many life forms thrive.
Unlike any of the other planets, Earth is covered by vast quantities of water.
In fact, more than 70% of the surface is under the ocean. Temperatures on
Earth are very moderate compared to the other planets. Humans can live relatively
comfortably at almost any location on the surface. Our only moon is a quarter
the size of Earth. It rotates on its axis at exactly the same rate that it
orbits the Earth, and so we always see the same side of the moon. There is
no air or water on the surface of the moon, and there is also no geological
activity. The moon is the only other place in the universe that people have
traveled to. |
|
|
|
MARS is a rocky red planet about
half the size of Earth. It orbits the sun every 1.88 Earth years, and a day
on Mars lasts about as long as one on Earth does. The planet's axis of rotation
is also similar to the Earth's, which means that Mars experiences seasons
as well. One unique feature is the polar ice caps, which are a combination
of water ice and frozen carbon dioxide. The ice caps melt and rebuild according
to the seasons, just as they do on Earth. The surface features on Mars are
huge: the Valles Marinaris is a valley longer than the whole United States,
and Olympus Mons is a volcano larger than Arizona and three times higher than
the Hawaiian Island volcanoes. Three spacecraft have landed on Mars, and they
have sent back pictures of a relatively flat surface covered with red rocks.
Mars has two moons, Phobos and Deimos, which are probably asteroids captured
by Mars' orbit long ago. |
|
|
|
The ASTEROID BELT lies between
Mars and Jupiter. The first asteroids, or minor planets, were discovered in
the very early 1800s. Eventually over 4,000 of them were found. Astronomers
had calculated that another planet should lie between Mars and Jupiter, and
the asteroid belt seemed to solve this problem. Asteroids are composed of
raw material from the creation of our solar system. For some reason, this
material did not come together to form one planet. Asteroids are the source
of most meteors that have hit the Earth. |
|
|
|
JUPITER is named after the king
of the Roman gods. It is the largest planet, yet it spins very quickly on
its axis- one day is about 10 Earth hours. The atmosphere is composed mainly
of hydrogen and helium, although it is the small amounts of gases like ammonia
and methane which make the bands on Jupiter look so colorful. It is very turbulent
in the atmosphere, with huge storms frequently lasting years. The Great Red
Spot is a storm which has been in existence for 300 years, and covers an area
larger than Earth! Jupiter is a gas giant with a very faint ring system. The
atmosphere is so thick that it is impossible to see the rocky core that is
probably at the center of this huge body. There are 16 moons orbiting Jupiter.
The four brightest ones- Io, Europa, Ganymede, and Callisto- are visible from
Earth through a small telescope. They were first discovered in 1610 by Galileo,
who was using a telescope that he built. These four moons are therefore called
the Galilean satellites. |
|
|
|
SATURN is one of the most beautiful
and unusual sights in the sky. It is a giant gas planet about ten times the
size of Earth. Its density is so low that it would float in a (very) big dish
of water. Like Jupiter, Saturn has an atmosphere of hydrogen and helium and
is often very stormy. The most unique feature of Saturn is its bright and
colorful ring system, which is easily visible from Earth with a small telescope.
The rings are composed of billions of small rock and ice particles which reflect
the sunlight and are held together by gravity and a few of Saturn's moons.
The dark separation between the two main rings is called the Cassini division.
Saturn has 18 moons. The largest is Titan, which is actually larger than Mercury
and Pluto. |
|
|
|
URANUS was found in 1781 by the
astronomer William Herschel. Like Saturn and Jupiter, Uranus is a gas giant
with a helium and hydrogen atmosphere. Uranus has a faint ring system that
cannot be seen from Earth except with a very large telescope. The rings were
discovered only 23 years ago, when Uranus passed in front of a star, which
appeared to blink as it passed the rings. Uranus has at least 15 moons, some
of which are probably captured asteroids. |
|
|
|
NEPTUNE was discovered in 1846,
after astronomers calculated where its orbit should be in order to cause strange
motions in Uranus' orbit. Neptune's atmosphere is also composed of hydrogen
and helium, and it has a very faint ring system that cannot be seen from Earth.
For 20 years out of every 248 years (one orbit of Pluto), Neptune is actually
the farthest planet from the sun. This was the case from 1979 until 1999.
Pluto is now once again the last planet in the solar system. Neptune has eight
moons. |
|
|
|
PLUTO is usually (see 'Neptune'
above) the farthest planet from the sun. It was found in 1930. Pluto is quite
different from the other gas giants in the outer reaches of the solar system.
In fact, it is simply a rock composed of frozen methane. There is an on-going
debate about whether Pluto should be considered a planet, since it more closely
resembles an asteroid or moon. Some astronomers believe that it is an escaped
moon of Neptune, and others believe that it could be the remains of a large
comet. Pluto is extremely cold, with a surface temperature of only about -360
degrees Fahrenheit. Pluto's only moon, Charon, was discovered in 1978. |
|
|
|
REFERENCES FOR THIS
PAGE:
M. Chartrand, The Audubon Society Field
Guide to the Night Sky, Knopf, 1991.
K. Kuhn, In Quest of the Universe, West
Publishing Company, 1994.
The photographs used on
this page are reproduced for educational purposes from the NASA, STScI, and
Hubble Space Telescope Picture Galleries. |
|
 |
|