Mars is the fourth planet from the Sun in the Solar System.
The planet is named after Mars, the Roman god of war. It is also
referred to as the "Red Planet" because of its reddish
appearance, due to iron oxide prevalent on its surface.
Mars is a terrestrial planet with a thin atmosphere, having
surface features reminiscent both of the impact craters of the
Moon and the volcanoes, valleys, deserts and polar ice caps of
Earth. It is the site of Olympus Mons, the highest known mountain
in the Solar System, and of Valles Marineris, the largest canyon.
Furthermore, in June 2008 three articles published in Nature
presented evidence of an enormous impact crater in Mars's northern
hemisphere, 10,600 km long by 8,500 km wide. In addition to its
geographical features, Mars’ rotational period and seasonal cycles
are likewise similar to those of Earth.

Mars’ average distance from the Sun is roughly 230 million km
and its orbital period is 687 (Earth) days. The solar day (or
sol) on Mars is only slightly longer than an Earth day: 24 hours,
39 minutes, and 35.244 seconds. A Martian year is equal to 1.8809
Earth years, or 1 year, 320 days, and 18.2 hours.
Mars's axial tilt is 25.19 degrees, which is similar to the
axial tilt of the Earth. As a result, Mars has seasons like the
Earth, though on Mars they are nearly twice as long given its
longer year.
Mars has a relatively pronounced orbital eccentricity of about
0.09; of the seven other planets in the Solar System, only Mercury
shows greater eccentricity. However, it is known that in the
past Mars has had a much more circular orbit than it does currently.
At one point 1.35 million Earth years ago, Mars had an eccentricity
of roughly 0.002, much less than that of Earth today. For the
last 35,000 years Mars' orbit has been getting slightly more
eccentric because of the gravitational effects of the other planets.
The closest distance between the Earth and Mars will continue
to mildly decrease for the next 25,000 years.
Mars has two tiny natural moons, Phobos and Deimos, which orbit
very close to the planet. Their known composition suggests the
moons are captured asteroids but their origin remains uncertain.

Both satellites were discovered in 1877 and are
named after characters in Greek mythology who accompanied their
father Ares, god of war, into battle. Ares was known as Mars
to the Romans.
From the surface of Mars, the motions of Phobos and Deimos appear
very different from that of our own moon. Phobos rises in the
west, sets in the east, and rises again in just 11 hours. Deimos,
being only just outside synchronous orbit—where the orbital period
would match the planet's period of rotation—rises as expected
in the east but very slowly. Despite the 30 hour orbit of Deimos,
it takes 2.7 days to set in the west as it slowly falls behind
the rotation of Mars, then just as long again to rise.
Because Phobos' orbit is below synchronous altitude, the tidal
forces from the planet Mars are gradually lowering its orbit.
In about 50 million years it will either crash into Mars’ surface
or break up into a ring structure around the planet.
Based on orbital observations and the examination of the Martian
meteorite collection, the surface of Mars appears to be composed
primarily of basalt. Much of the surface is deeply covered by
finely grained iron oxide dust.
Liquid water cannot exist on the surface of Mars with its present
low atmospheric pressure, except at the lowest elevations for
short periods, but water ice is in no short supply, with two
polar ice caps made largely of ice. In March 2007, NASA announced
that the volume of water ice in the south polar ice cap, if melted,
would be sufficient to cover the entire planetary surface to
a depth of 11 metres. Additionally, an ice permafrost mantle
stretches down from the pole to latitudes of about 60°.
Recent studies support a theory, first proposed in the 1980s,
that Mars was struck by a Pluto-sized body about four billion
years ago. The event, thought to be the cause of the Martian
hemispheric dichotomy, created the smooth Borealis basin that
covers 40% of the planet.

Of all the planets, Mars's seasons are the most Earth-like,
due to the similar tilts of the two planets' rotational axes.
However, the lengths of the Martian seasons are about twice those
of Earth's, as Mars’ greater distance from the Sun leads to the
Martian year being about two Earth years in length. Martian surface
temperatures vary from lows of about −220 °F during the polar
winters to highs of up to 68 °F in summer. The wide range in
temperatures is due to the thin atmosphere which cannot store
much solar heat, the low atmospheric pressure, and the low thermal
inertia of Martian soil.
If Mars had an Earth-like orbit, its seasons would be similar
to Earth's because its axial tilt is similar to Earth's. However,
the comparatively large eccentricity of the Martian orbit has
a significant effect. Mars is near perihelion when it is summer
in the southern hemisphere and winter in the north, and near
aphelion when it is winter in the southern hemisphere and summer
in the north. As a result, the seasons in the southern hemisphere
are more extreme and the seasons in the northern are milder than
would otherwise be the case.
Mars also has the largest dust storms in our Solar System. These
can vary from a storm over a small area, to gigantic storms that
cover the entire planet. They tend to occur when Mars is closest
to the Sun, and have been shown to increase the global temperature.
To the naked eye, Mars usually appears a distinct yellow, orange,
or reddish color, and varies in brightness more than any other
planet as seen from Earth over the course of its orbit. However
the actual color of Mars is closer to butterscotch, and the redness
seen is actually just dust in the planets atmosphere. NASA's
Spirit rover has taken pictures of a greenish-brown, mud-colored
landscape with blue-grey rocks and patches of light red colored
sand.

When farthest away from the Earth, it is more than seven times
as far from the latter as when it is closest. When least favorably
positioned, it can be lost in the Sun's glare for months at a
time. At its most favorable times (at 15- or 17-year intervals,
and always between late July and late September), Mars shows
a wealth of surface detail to a telescope. Especially noticeable,
even at low magnification, are the polar ice caps.