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The word "comet", which originates from a Greek word
meaning "long-haired", indicates that these objects look like hairy
stars with tails stretching across the sky. What we see in a bright comet is actually sunlight scattered by
dust particles and the glow of fluorescent molecules or
ions. Cometary nuclei - "dirty snowballs" - consist of ices (mostly water
ice) and dust. They come in all sizes, from a few tens of metres to
several tens of kilometres. Whenever a cometary nucleus is heated by
sunlight, some of its ices are turned into gases (by sublimation),
which escape with some dust particles. The gases and dust form a
bright halo, a few tens of thousands of kilometres around the nucleus,
whose size is just a few kilometres, and are progressively pushed away
from the Sun by the solar wind and by solar radiation pressure.
The famous Comet Halley, whose nucleus is about 15
kilometres across, describes its elliptical orbit in about 75
years. The comets we can see nowadays are mostly on elongated orbits
around the Sun, and are progressively loosing all their ices. They have been preserved for aeons in two huge reservoirs, the
so-called Kuiper belt, which corresponds to small bodies that
remained at solar distances between 30 and 100 times the Earth
distance (i.e., about 5 to 15 billion km from the Sun), and the
so-called Oort cloud, which is made up of small bodies formed
at solar distances between 5 and 30 times the Earth distance (i.e.,
about 1 to 5 billion km from the Sun), and which have later been
pushed to the outer edge of the Solar System. Gravitational perturbations by background stars or gravitational
tides have changed the orbits of some of these nuclei and eventually
injected them into the inner solar system. As they are still quite
representative of the disk out of which the Solar System formed, such
nuclei are thus very indicative of the matter that hit the terrestrial
planets at the early epoch of heavy bombardment. Indeed, the discovery through past cometary missions of large
amounts of water in comets and of complex organic molecules in the
tiny aggregates of cometary dust, strongly suggest that cometary impacts could have
provided the early Earth with all the building blocks for Life,
i.e. water and prebiotic molecules, that is to say carbonaceous
compounds. Such impacts might also have allowed an early development
of Life, now most likely now extinct, on the planet Mars.
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Life in the Universe
Formation of Planetary Systems
Planetary Formation
Small Bodies
Asteroids
Comets
Deep Impacts
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Last updated September 3, 2001