The Solar System
Source: NASA
| The following planetary information is bases on comparisons of each planet to earth. |
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Mercury The small and rocky planet Mercury is the closest planet to the Sun; it speeds around the Sun in a wildly elliptical (non-circular) orbit that takes it as close as 47 million km and as far as 70 million km from the Sun. Mercury completes a trip around the Sun every 88 days, speeding through space at nearly 50 km per second, faster than any other planet. Because it is so close to the Sun, temperatures on its surface can reach a scorching 467 degrees Celsius. But because the planet has hardly any atmosphere to keep it warm, nighttime temperatures can drop to a frigid -183 degrees Celsius. Because Mercury is so close to the Sun, it is hard to see from Earth except during twilight. Until 1965, scientists thought that the same side of Mercury always faced the Sun. Then, astronomers discovered that Mercury completes three rotations for every two orbits around the Sun. If you wanted to stay up for a Mercury day, you'd have to stay up for 176 Earth days! The Caloris Basin, one of the largest features on Mercury, is about 1,300 km in diameter. It was the result of an asteroid impact on the planet's surface early in the solar system's history, the probable cause of the strange surfaces on the opposite side of the planet. Over the next half-billion years, Mercury actually shrank in radius from 2 to 4 km as the planet cooled from its formation. The outer crust, called the lithosphere, was compressed and grew strong enough to prevent the planet's magma from reaching the surface, effectively ending the planet's period of geologic activity. Evidence of Mercury's active past is seen in the smooth plains in the Caloris basin. Mercury is the second smallest planet in the solar system, larger only
than Pluto, the most distant planet in our solar system. If Earth were
the size of a baseball, Mercury would be the size of a golf ball. Viewed
from Mercury, the Sun would look almost three times as large as it does
from Earth. Mercury is the second densest body in the solar system after
Earth, with an interior made of a large iron core with a radius of 1,800
to 1,900 km, nearly 75 percent of the planet's diameter and nearly the
size of Earth's Moon. Mercury's outer shell, comparable to Earth's outer
shell (called the mantle) is only 500 to 600 km thick. |
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Venus
At first glance, if Earth had a twin, it would be Venus. The two planets are similar in size, mass, composition, and distance from the Sun. But there the similarities end. Venus has no ocean. Venus is covered by thick, rapidly spinning clouds that trap surface heat, creating a scorched greenhouse-like world with temperatures hot enough to melt lead and pressure so intense that standing on Venus would feel like the pressure felt 900 meters deep in Earth's oceans. These clouds reflect sunlight in addition to trapping heat. Because Venus reflects so much sunlight, it is usually the brightest planet in the sky. Venus sluggishly rotates on its axis once every 243 Earth days, while it orbits the Sun every 225 days - its day is longer than its year! Besides that, Venus rotates retrograde, or "backwards," spinning in the opposite direction of its orbit around the Sun. From its surface, the Sun would seem to rise in the west and set in the east. Earth and Venus are similar in density and chemical compositions, and both have relatively young surfaces, with Venus appearing to have been completely resurfaced 300 to 500 million years ago. The surface of Venus is covered by about 20 percent lowland plains, 70 percent rolling uplands, and 10 percent highlands. Volcanism, impacts, and deformation of the crust have shaped the surface. No direct evidence of currently active volcanoes has been found, although large variations of sulfur dioxide in the atmosphere lead some scientists to suspect that volcanoes may be active. Although no rainfall, oceans, or strong winds exist to erode surface
features, some weathering and erosion does occur. The surface is brushed
by gentle winds, no stronger than a few kilometers per hour, enough
to move grains of sand, and radar images of the surface show wind streaks
and sand dunes. In addition, the corrosive atmosphere probably chemically
alters rocks. Impact cratering is also affected by the dense atmosphere:
craters smaller than 1.5 to 2 km across do not exist on Venus, largely
because small meteors burn up in Venus? dense atmosphere before they
can reach the surface. With few exceptions, features on Venus are named for accomplished women from all of Earth's cultures. Venus' interior is probably very similar to that of Earth, containing an iron core about 3,000 km in radius and a molten rocky mantle covering the majority of the planet. Recent results from the Magellan spacecraft suggest that Venus' crust is stronger and thicker than had previously been thought. Venus has no satellites and no intrinsic magnetic field, but the solar wind rushing by Venus creates a pseudo-field around the planet. |
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Earth Earth, our home planet, is the only planet in our solar system known to harbor life - life that is incredibly diverse. All of the things we need to survive are provided under a thin layer of atmosphere that separates us from the uninhabitable void of space. Earth is made up of complex, interactive systems that are often unpredictable. Air, water, land, and life - including humans - combine forces to create a constantly changing world that we are striving to understand. Viewing Earth from the unique perspective of space provides
the opportunity to see Earth as a whole. Scientists around the world
have discovered many things about our planet by working together and
sharing their findings. Oceans at least 4 km deep cover nearly 70 percent of Earth's surface. Fresh water exists in the liquid phase only within a narrow temperature span (0 degrees to 100 degrees Celsius). This temperature span is especially narrow when contrasted with the full range of temperatures found within the solar system. The presence and distribution of water vapor in the atmosphere is responsible for much of Earth's weather. Near the surface, an ocean of air that consists of 78 percent nitrogen, 21 percent oxygen, and 1 percent other ingredients envelops us. This atmosphere affects Earth's long-term climate and short-term local weather; shields us from nearly all harmful radiation coming from the Sun; and protects us from meteors as well - most of which burn up before they can strike the surface. Satellites have revealed that the upper atmosphere actually swells by day and contracts by night due to solar activity. Our planet's rapid spin and molten nickel-iron core
give rise to a magnetic field, which the solar wind distorts into
a teardrop shape. The solar wind is a stream of charged particles
continuously ejected from the Sun. The magnetic field does not fade
off into space, but has defi- nite boundaries. When charged particles
from the solar wind become trapped in Earth's magnetic field, they
collide with air molecules above our planet's magnetic poles. These
air molecules then begin to glow and are known as the aurorae, or
the Northern and Southern Lights. From the vantage point of space we are able to observe our planet globally, as we do other planets, using similar sensitive instruments to understand the delicate balance among its oceans, air, land, and life.
Earth's Moon |
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Mars
We know that Mars is a small rocky body once thought to be very Earth-like. Like the other "terrestrial" planets - Mercury, Venus, and Earth - its surface has been changed by volcanism, impacts from other bodies, movements of its crust, and atmospheric effects such as dust storms. It has polar ice caps that grow and recede with the change of seasons; areas of layered soils near the Martian poles suggest that the planet's climate has changed more than once, perhaps caused by a regular change in the planet's orbit. Martian tectonism - the formation and change of a planet's crust - differs from Earth's. Where Earth tectonics involve sliding plates that grind against each other or spread apart in the seafloors, Martian tectonics seem to be vertical, with hot lava pushing upwards through the crust to the surface. Periodically, great dust storms engulf the entire planet. The effects of these storms are dramatic, including giant dunes, wind streaks, and wind-carved features. Scientists believe that 3.5 billion years ago, Mars experienced the largest known floods in the solar system. This water may even have pooled into lakes or shallow oceans. But where did the ancient flood water come from, how long did it last, and where did it go? In May 2002, scientists announced the discovery of a key piece in the puzzle: the Mars Odyssey spacecraft had detected larged quantities of water ice close to the surface - enough to fill Lake Michigan twice over. The ice is mixed into the soil only a meter (about 3 feet) below the surface of a wide area near the Martian south pole. Many questions remain. At present, Mars is too cold and its atmosphere is too thin to allow liquid water to exist at the surface for long. More water exists frozen in the polar ice caps, and enough water exists to form ice clouds, but the quantity of water required to carve Mars' great channels and flood plains is not evident on - or near - the surface today. Images from NASA's Mars Global Surveyor spacecraft suggest that underground reserves of water may break through the surface as springs. The answers may lie deep beneath Mars' red soil. The full face of Mars as seen by the Hubble Space Telescope. Mars has some remarkable geological characteristics, including the largest volcanic mountain in the solar system, Olympus Mons (27 km high and 600 km across); volcanoes in the northern Tharsis region that are so huge they deform the planet's roundness; and a gigantic equatorial rift valley, the Valles Marineris. This canyon system stretches a distance equivalent to the distance from New York to Los Angeles; Arizona's Grand Canyon could easily fit into one of the side canyons of this great chasm. Mars also has two small moons, Phobos and Deimos. Although no one knows how they formed, they may be asteroids snared by Mars' gravity.
Moons of Mars
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Jupiter With its numerous moons and several rings, the Jupiter system is a "mini-solar system." Jupiter is the most massive planet in our solar system, and in composition it resembles a small star. In fact, if Jupiter had been between fifty and one hundred times more massive, it would have become a star rather than a planet. On January 7, 1610, while skygazing from his garden in Padua, Italy,
astronomer Galileo Galilei was surprised to see four small "stars"
near Jupiter. He had discovered Jupiter's four largest moons, now called
Io, Europa, Ganymede, and Callisto. Collectively, these four moons are
known today as the Galilean satellites. At first glance, Jupiter appears striped. These stripes are dark belts and light zones created by strong east-west winds in Jupiter's upper atmosphere. Within these belts and zones are storm systems that have raged for years. The southern hemisphere's Great Red Spot has existed for at least 100 years, and perhaps longer, as Galileo reported seeing a similar feature nearly 400 years ago. Three Earths could fit across the Great Red Spot. Jupiter's core is probably not solid but a dense, hot liquid with a consistency like thick soup. The pressure inside Jupiter may be 30 million times greater than the pressure at Earth's surface. As Jupiter rotates, a giant magnetic field is generated in its electrically conducting liquid interior. Trapped within Jupiter's magnetosphere - the area in which magnetic field lines encircle the planet from pole to pole - are enough charged particles to make the inner portions of Jupiter's magnetosphere the most deadly radiation environment of any of the planets, both for humans and for electronic equipment. The "tail" of Jupiter's magnetic field - that portion stretched behind the planet as the solar wind rushes past - has been detected as far as Saturn's orbit. Jupiter's rings and moons are embedded in an intense radiation belt of electrons and ions trapped in the magnetic field. The Jovian magnetosphere, which comprises these particles and fields, balloons one to three extending more than one billion kilometers behind Jupiter - as far as Saturn's orbit. Discovered in 1979 by NASA's Voyager 1 spacecraft, Jupiter's rings
were a surprise: a flattened main ring and an inner cloud-like ring,
called the halo, are both composed of small, dark particles. A third
ring, known as the gossamer ring because of its transparency, is actually
three rings of microscopic debris from three small moons: Amalthea,
Thebe, and Adrastea. Jupiter's ring system may be formed by dust kicked
up as interplanetary meteoroids smash into the giant planet's four small
inner moons. The main ring probably comes from the tiny moon Metis.
These photos of the four Galilean satellites of Jupiter were taken by Voyager 1 during its approach to the planet in early March 1979. Io (top left), Europa (top right), Ganymede (bottom left) and Callisto (bottom right) are shown in their correct relative sizes: Ganymede and Callisto are both larger than the planet Mercury; Io and Europa are about the same size as the Moon. Image processing also preserves tne relative contrasts of the satellites. Thus it is apparent that Europa has the least contrast; Io the greatest. Io is coveredwith active volcanos and a surface composed largely of sulfur. Europa is apparently very different; Voyager 1 did not approach Europa closely enough to show its surface in great detail; that remains for Voyager 2. Ganymede and Callisto are both composed mostly of water and water ice; they have large quantities of ice exposed on their surfaces. The Io photo was taken from 1.7 million miles (2.9 million kilometers); Europa, 1.7 million miles (2.9 million kilometers); Ganymede, 2 million miles (3.4 million kilometers); and Callisto, 4.1 million miles (6.9 million kilometers). Resolution of all photos except Callisto is about 30 miles (50 kilometers), and for Callisto it is 60 miles (100 kilometers). The Voyager Project is managed and controlled for NASA's Office of Space Science by the Jet Propulsion Laboratory. The following is a list of all presently known moons of Jupiter: Metis, Adrastea, Amalthea, Thebe, Io, Europa, Ganymede, Callisto, Leda, Himalia, Elara, Pasiphae, Sinope, Lysithea, Carne, Ananke, W1302, W1700, W1700_2, W1704, W1704_2, W1800, W1903_s, W1805, W1902, W1904, W2002_2, and 2 unnamed moons. |
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Saturn
Like the other giant planets - Jupiter, Uranus, and Neptune - Saturn
is a gas giant made mostly of hydrogen and helium. Its volume is 755
times greater than Earth's. Winds in the upper atmosphere reach 500
meters per second in the equatorial region. (In contrast, the strongest
hurricane-force winds on Earth top out at about 110 meters per second.)
These super-fast winds, combined with heat rising from within the planet's
interior, cause the yellow and gold bands visible in its atmosphere. Saturn has at least 30 satellites. The largest, Titan, is a bit bigger than the planet Mercury. Titan is shrouded in a thick nitrogen-rich atmosphere that might be similar to what Earth's was like long ago. Further study of this moon promises to reveal much about planetary formation and, perhaps, about the early days of Earth as well. In addition to Titan, Saturn has many smaller "icy" satellites. From Enceladus, which shows evidence of surface changes, to Iapetus, with one hemisphere darker than asphalt and the other as bright as snow, each of Saturn's satellites is unique. Saturn, the rings, and many of the satellites lie totally within Saturn's enormous magnetosphere, the region of space in which the behavior of electrically charged particles is influenced more by Saturn's magnetic field than by the solar wind. Recent images by NASA's Hubble Space Telescope show that Saturn's polar regions have aurorae similar to Earth's Northern and Southern Lights. Aurorae occur when charged particles spiral into a planet's atmosphere along magnetic field lines. The next chapter in our knowledge of Saturn is already under way, as the Cassini/Huygens spacecraft began its journey to Saturn in October 1997 and will arrive on July 1, 2004. The Huygens probe will descend through Titan's atmosphere in late November 2004 to collect data on the atmosphere and surface of the moon. Cassini will orbit Saturn more than 70 times during a four-year study of the planet, its moons, rings, and magnetosphere. Cassini/Huygens is a joint NASA/European Space Agency mission. Moons of Saturn
The 8 moons above represent the Major satellites of Saturn. At last count there were 31 moons. The following is a list of all presently known moons of Saturn: Titan, Iapetus, Rhea, Tethys, Dione, Enceladus, Mimas,
Hyperion, Phoebe, Janus, Epimetheus, Atlas, Helene, Calypso, Telesto, |
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Uranus Once considered one of the blander-looking planets, Uranus (pronounced YOOR un nus) has been revealed as a dynamic world with some of the brightest clouds in the outer solar system and 11 rings. Uranus gets its blue-green color from methane gas above the deeper cloud layers (methane absorbs red light and reflects blue light). Uranus was discovered in 1781 by astronomer William Herschel, who at
first believed it to be a comet. This seventh planet from the Sun is
so distant that it takes 84 years to complete an orbit. In 1986, Voyager 2 observed faint cloud markings in the southern latitudes blowing westward between 100 and 600 km/hr. In 1998, the Hubble Space Telescope observed as many as 20 bright clouds at various altitudes in Uranus’ atmosphere. The bright clouds are probably made of crystals of methane, which condense as warm bubbles of gas well up from deep in the atmosphere of Uranus. Uranus currently moves around the Sun with its rotation axis nearly horizontal with respect to the ecliptic plane. This unusual orientation may be the result of a collision with a planet-sized body early in the planet’s history, which apparently changed Uranus’ rotation radically. Uranus’ magnetic field is unusual in that the magnetic axis is tilted 60 degrees from the planet’s axis of rotation and is offset from the center of the planet by one-third of the planet’s radius. Uranus is so far from the Sun that, even though tipped on its side
and experiencing seasons that last over twenty years, the temperature
differences on the summer and winter sides of the planet do not differ
that greatly. Near the cloudtops, the temperature of Uranus is near
-215 °C. Uranus has at least 20 moons, named mostly for characters from the works of Shakespeare and Alexander Pope. Miranda is the strangest Uranian moon. The high cliffs and winding valleys of the moon may indicate partial melting of the interior, with icy material occasionally drifting to the surface. Moons of Uranus
The follow is a list of all the moons of Uranus discovered to date: Cordelia,Ophelia, Bianca, Cressida, Desdemona, Juliet, Portia, Rosalind, Belinda, Puck, Miranda Kuiper, Ariel Lassell, Umbriel , Lassell, Titania Herschel, Oberon Herschel, 1997U1, (Caliban*), Burns & Kavelaars, 1999U1, 1997U2, (Sycorax*), Burns & Kavelaars, 1999U2, 1999U3, 2001U1. *Name has been provisionally approved |
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Neptune
The eighth planet from the Sun, Neptune was the first planet located through mathematical predictions rather than through regular observations of the sky. When Uranus didn’t travel exactly as astronomers expected it to, two mathematicians, working independently of each other, proposed the position and mass of another, as yet unknown planet that could account for Uranus’ orbit. Although "the establishment" ignored the predictions, a young astronomer decided to look for the predicted planet. Thus, Neptune was discovered in 1846. Seventeen days later, its largest moon, Triton, was also discovered. Nearly 4.5 billion kilometers from the Sun, Neptune orbits the Sun
once every 165 years, and therefore it has not quite made a full circle
around the Sun since it was discovered. It is invisible to the naked
eye because of its extreme distance from Earth. Interestingly, due to
Pluto’s unusual elliptical orbit, Neptune is actually the farthest
planet from the Sun for a 20-year period out of every 248 Earth years. In 1989, Voyager 2 tracked a large oval dark storm in Neptune’s southern hemisphere. This hurricane-like "Great Dark Spot" was large enough to contain the entire Earth; spun counterclockwise; and moved westward at almost 1,200 km per hour. Recent images from the Hubble Space Telescope show no sign of the "Great Dark Spot," although a comparable spot appeared in 1997 in Neptune’s northern hemisphere. The planet has several rings of varying widths, confirmed by Voyager
2’s observations in 1989. The outermost ring, Adams, contains
five distinct arcs (incomplete rings) named Liberté, Equalité
1, Equalité 2, Fraternité, and Courage. Next is an unnamed
ring coorbital with the moon Galatea, then Le Verrier, Lassell, Arago,
and Galle. Neptune’s rings are believed to be relatively young
and relatively short-lived. Moons of Neptune The following is a list of all the moon of Neptune to date: Naiad, Thalassa, Despina, Galatea, Triton, Nereid, Proteus, Larissa |
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Pluto True Color Photograph
Discovered by American astronomer Clyde Tombaugh in 1930, Pluto takes
248 years to orbit the Sun. Pluto’s most recent close approach
to the Sun was in 1989. Between 1979 and 1999, Pluto's highly elliptical
orbit brought it closer to the Sun than Neptune, providing rare opportunities
to study this small, cold, distant world and its companion moon, Charon. Pluto and Charon orbit the Sun in a region where there may be a population of hundreds or thousands of similar bodies that were formed early in solar system history. These objects are referred to interchangeably as trans-Neptunian objects, Edgeworth-Kuiper Disk objects or ice dwarves. Pluto is about two-thirds the diameter of Earth’s Moon and may have a rocky core surrounded by a mantle of water ice. Due to its lower density, its mass is about one-sixth that of the Moon. Pluto appears to have a bright layer of frozen methane, nitrogen, and carbon monoxide on its surface. While it is close to the Sun, these ices thaw, rise, and temporarily form a thin atmosphere, with a pressure one one-millionth that of Earth’s atmosphere. Pluto’s low gravity (about 6 percent of Earth’s) causes the atmosphere to be much more extended in altitude than our planet’s. Because Pluto’s orbit is so elliptical, Pluto grows much colder during the part of each orbit when it is traveling away from the Sun. During this time, the bulk of the planet’s atmosphere freezes. In 1978, American astronomers James Christy and Robert Harrington discovered that Pluto has a satellite (moon), which they named Charon. Charon is almost half the size of Pluto and shares the same orbit. Pluto and Charon are thus essentially a double planet. Charon’s surface is covered with dirty water ice and doesn’t reflect as much light as Pluto’s surface. No spacecraft have visited Pluto. NASA is currently considering a mission called New Horizons that would explore both Pluto and the Kuiper Belt region. The earliest it would launch is 2006. Because Pluto is so small and far away, it is difficult to observe from Earth. In the late 1980s, Pluto and Charon passed in front of each other repeatedly for several years. Observations of these rare events allowed astronomers to make crude maps of each body. From these maps it was learned that Pluto has polar caps, as well as large, dark spots nearer its equator. Pluto's Moon Pluto might have other, as-yet undiscovered satellites. |