Mars is the fourth planet from the Sun
(between the Earth and Jupiter) and has long been referred to as the Red Planet,
because it appears to shine with a reddish hue when viewed from Earth. However,
recent NASA photographs indicate that the planet isn't really red at all - but
is more of a tan or butterscotch color. The diameter of Mars is approximately
6794 kilometers (4219 miles), which is considerably smaller than the diameter of
the Earth (12,763 km / 7926 mi). A Martian day is surprisingly similar in length
to one on Earth (24 hours and 37 minutes), but a Martian year is nearly twice as
long (687 days). Mars has two moons, Diemos and Phobos, both of which are
irregularly shaped and pitted with craters. Diemos orbits Mars once every 31
hours; Phobos speeds through the Martian sky three times a day, circling the
planet every seven hours.
Except for
Earth,
Mars has long been the subject of much debate as to whether it does
currently or once harbored life of any sort. Although the question of whether
life once existed in Mars's distant past has yet to be answered, scientists
generally conclude that life on the Mars of today is an impossibility. Mission
biologists contend that Mars is now self-sterilizing: the combination of the
solar ultraviolet radiation saturating the surface, the extreme dryness of the
soil, and the oxidizing nature of the soil chemistry prevent the formation of
living organisms on the Martian surface.
Mars has
the most highly varied and interesting terrain of any of the terrestrial
planets, some of it quite spectacular:
- Olympus Mons: the largest mountain in the
Solar System rising 24 km (78,000 ft.) above the surrounding plain. Its base is
more than 500 km in diameter and is rimmed by a cliff 6 km (20,000 ft) high
(right).
- Tharsis: a huge bulge on the Martian
surface that is about 4000 km across and 10 km high.
- Valles Marineris: a system of canyons
4000 km long and from 2 to 7 km deep (top of page);
- Hellas Planitia: an impact crater in the
southern hemisphere over 6 km deep and 2000 km in diameter.
Much of the Martian surface is very old and cratered, but there are also much
younger rift valleys, ridges, hills and plains.
The
Martian atmosphere is very different from Earth; it is composed primarily of
carbon dioxide (95.32%), with small amounts of other gases, such as Nitrogen
(2.7%), Argon (1.6%), and Oxygen (0.13%). Martian air contains only 1/1000th as
much water as Earth's air, but it can still condense to form clouds, fog, and
even frost. The average recorded temperature on Mars is -63° C (-81°F), with a
maximum temperature of 20° C (68° F) and a minimum of -140° C (-220° F).
Evidence suggests that long ago, under a denser Martian atmosphere, water may
have flowed on the planet. Many features strongly resemble shorelines, river
beds, gorges, and islands. The recent Pathfinder mission indicated that the
jumble of rocks near the landing site had been deposited by a great rushing
flood.
The Red Planet has two small
moons that rotate very close to the surface. Phobos has a 22 kilometer diameter
and is 9,378 kilometers from Mars. Deimos is 23,459 kilometers from the planet
and has a 12 kilometer diameter. Both moons were discovered by a man named Hall
in 1877.
Perhaps
the most enduring image from the surface of Mars (and certainly the most
controversial) is that of "The Face," which was first photographed by
Viking Orbiter 1 in 1976. Subsequent images from the Mars Global Surveyor
spacecraft of this outropping in the Cydonia region show that it is nothing more
than a bumpy hill.
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