nucleus: relatively solid and stable,
mostly ice and gas with a small amount of dust and other solids;
coma: dense cloud of water, carbon
dioxide and other neutral gases sublimed from the nucleus;
hydrogen cloud: huge (millions of
km in diameter) but very sparse envelope of neutral hydrogen;
Components of a comet
lumps of ice and dust
periodically come into the center of the solar system
close enough to the Sun,
heat makes them start to evaporate.
Jets of gas and dust form long tails
These tails can sometimes be millions of miles long.
Components of a comet
dust tail: up to 10 million km long smoke-sized dust
most prominent part of a comet to the unaided eye;
ion tail: as much as several hundred million km long
composed of plasma interactions with the solar wind.
Comet West
shows two distinct tails.
thin blue plasma tail made up of gases
broad white tail made up of microscopic dust particles.
What’s next
Eventually- becomes just
another rocky mass in the solar system.
comets are said to be short-lived, on a cosmological time scale.
Many scientists believe
that some asteroids are extinct comet nuclei
http://www.solarviews.com/eng/comet.htm
An explanation
Dutch astronomer Jan Oort
In 1950
hypothesized that comets came from a vast shell of icy bodies about 50,000
times farther from the Sun than Earth is.
astronomer Gerard Kuiper
A year later
some comet-like debris from the formation of the solar system beyond Neptune.
The Oort cloud is an immense spherical cloud
surrounding the planetary system
extending approx 3 light years,
about 30 trillion kilometers from the Sun.
considered the edge of the Sun's orb of
physical, gravitational, or dynamical influence.
Oort Cloud
source of long-period
comets
Halleys and Swift-Tuttle.
come from an average
distance of 44,000 astronomical units.
appear at any time and come from any direction.
Bright comets can usually
be seen every 5-10 years.
Two recent Oort cloud
comets were Hyakutake and Hale-Bopp.
Hyakutake was average in size, but came to 0.10 AU (15,000,000 km) from
Earth
Hale-Bopp, at comparable distances from the sun, making it appear
quite bright, a distance of 1.32 AU (197,000,000 km) to the Earth.
Asteroids
rocky
and metallic object orbit the Sun
too small to be considered planets.
known as minor planets.
range in size from Ceres
1000 km, down to the size of pebbles.
found inside Earth's orbit to beyond Saturn's orbit.
Most contained within
a main belt
between the orbits of Mars and Jupiter.
Some have orbits that
cross Earth's path
some have even hit the Earth in times past.
theory
material left over from
the formation of the solar system.
never coalesced into a planet.
another theory suggests
remains of a planet
destroyed in a massive collision long ago.
Asteroids
asteroids are material
from the very early solar system,
scientists interested
in composition.
asteroid belt empty space
asteroids are separated
by very large distances.
visited by the Galileo spacecraft
Gaspra
243 Ida.
253 Mathilde
June 27, 1997
the spacecraft NEAR -
high-speed close encounter
first close-up look of
a carbon rich C-type asteroid.
Ida
http://www.solarviews.com/cap/ast/vida1.htm
This animation shows the shape and surface of Ida. North is located at
the top and the camera view is situated at the equatorial plane of Ida.
The animation starts at -90 degrees longitude.
S-type asteroids composed of metal-rich silicates
Gaspra
S-type asteroids composed of metal-rich silicates.
Ceres
the largest known rock
in the solar system.
Texas-sized asteroid
about 930 kilometers (580 miles) across,
first asteroid
ever detected.
identified in 1801 by astronomer Giuseppe Piazzi,
noted over a few nights a shifting point in the sky
`wasn't one of the planets, their moons or a star.
Meteoroid
http://www.solarviews.com/eng/meteor.htm
What is a Meteroids
Asteroids that are on a collision course with Earth are called meteoroids.
When a meteoroid strikes our atmosphere at high velocity, friction causes
this chunk of space matter to incinerate in a streak of light known as
a meteor.
If the meteoroid does not burn up completely, what's left strikes Earth's
surface and is called a meteorite.
Meterorites
92.8 percent are composed
of silicate (stone), and
5.7 percent are composed
of iron/ nickel
the rest are a
mixture of the three materials.
Stony meteorites - hardest
to identify
they look very much like terrestrial rocks.
One of the primary goals of studying meteorites
is to determine the history and origin of their parent bodies.