This dust particle was collected by
spacecraft above Earth’s atmosphere.
It is almost certainly from a comet.
As the ices in a comet nucleus
vaporize, they release dust particles that
not only form the dust tail, but also spread
throughout the solar system.
The Deep Impact spacecraft released an
instrumented probe into the path of Comet
Tempel 1. When the comet slammed into the
probe at 10.2 km/s as shown at right huge
amounts of gas and dust were released. From
the results, scientists conclude that the nucleus
of the comet is rich in dust finer than the
particles of talcum powder. The nucleus is
marked by craters, but it is not solid rock. It is
about the density of fresh fallen snow.
This dust particle was collected by
spacecraft above Earth’s atmosphere.
It is almost certainly from a comet.
Fragments
A microscopic
mineral crystal
from Comet
Wild 2
Dust particles (arrows) were embedded in the
collector when they struck at high velocity.
Direction
of travel
Visual-wavelength images
Visual
Comet 73P/Schwassmann-Wachmann3 Fragment B
NASA
NASA/JPL-Caltech/UMD
NASA
JPL/ NASA
NASA/ESA/H. Weaver/JHU/APL/M. Mutchler and Z. Levay/STScI
As the ices in a comet nucleus
vaporize, they release dust particles that
not only form the dust tail but also spread
throughout the solar system.
The Deep Impact spacecraft released an
instrumented probe into the path of Comet
Tempel 1. When the comet slammed into the
probe at 10.2 km/s as shown at right, huge
amounts of gas and dust were released. From
the results, scientists conclude that the nucleus
of the comet is rich in dust finer than the
particles of talcum powder. The nucleus is
marked by craters, but it is not solid rock. It is
about the density of fresh-fallen snow.
2
The nuclei of comets are not strong and can break up. In 2006,
Comet Schwassmann-Wachmann 3 broke into a number of fragments
that themselves fragmented. Fragment B is shown at the right breaking into
smaller pieces. The gas and dust released by the breakup made the comet
fragments bright in the night sky, and some were visible with binoculars. As
its ices vaporize and its dust spreads, the comet may totally disintegrate and
leave nothing but a stream of debris along its previous orbit.
Comets most often break up as they pass close to the sun or close to a
massive planet like Jupiter. Comet LINEAR broke up in 2000 as it passed by
the sun. The comet that hit Jupiter in 1994 was first ripped to pieces by tidal
stresses from Jupiter’s gravity. Comets can also fragment far from planets,
perhaps because of the vaporization of critical structural areas of ice.
3
2a The Stardust spacecraft flew past the nucleus of Comet Wild 2 and collected dust particles
(as shown above) in an exposed target that was
later parachuted back to Earth. The dust particles hit
the collector at high velocity and became
embedded, but they can be extracted for study.
Some of the collected dust is made of high-temperature minerals that could only have
formed near the sun. This suggests that material from the inner solar nebula was mixed
outward and became part of the forming comets in the outer solar system. Other
minerals found include olivine, a very common mineral on Earth but not one that
scientists expected to find in a comet.
Only seconds before
impact, craters are visible
on the dark surface.
Images of Comet Tempel 1 from
the flyby probe 13 seconds after
the impact probe hit. Gas and dust
are thrown out of the impact crater.