HST News &
Updates Archive
September 4, 1997:
HST Update:
Hubble Reveals Huge Crater On
The Surface Of The Asteroid Vesta
(Go back to the most
recent update)
Crater On The Surface Of The
Asteroid Vesta
Astronomers have used
NASA's Hubble Space Telescope to discover a giant
impact crater on the asteroid Vesta. The crater is
a link in a chain of events thought responsible for
forming a distinctive class of tiny asteroids as
well as some meteorites that have reached the
Earth.
The giant crater is 285
miles across, which is nearly equal to Vesta's 330
mile diameter. If Earth had a crater of
proportional size, it would fill the Pacific Ocean
basin. Astronomers had predicted the existence of
one or more large craters, reasoning that if Vesta
is the true "parent body" of some smaller asteroids
then it should have the wound of a major impact
that was catastrophic enough to knock off big
chunks. The observations are described in the
September 5 issue of Science Magazine.
"In hindsight we should
have expected finding such a large crater on
Vesta," says Peter Thomas of Cornell University,
Ithaca, NY. "But it's still a surprise when it's
staring you in the face." Another surprising
finding is that such a large crater, relative to
Vesta's size, might have been expected to cause
more damage to the rest of the minor planet.
"This is a unique
opportunity to study the effects of a large impact
on a small object," says Michael Gaffey of
Rensselaer Polytechnic Institute, Troy, New York.
"This suggests that more asteroids from the early
days of the solar system may still be
intact."
The collision gouged out
one percent of the asteroid's volume, blasting over
one-half million cubic miles of rock into space.
This tore out an eight-mile deep hole that may go
almost all the way through the crust to expose the
asteroid's mantle (Vesta is large enough to be
differentiated like Earth - with a volcanic crust,
core and mantle, making it a sort of
"mini-planet".)
Because of the asteroid's
small diameter and low gravity, the crater
resembles smaller craters on the Moon that have a
distinctive central peak. Towering eight miles,
this cone-shaped feature formed when molten rock
"sloshed" back to the bull's-eye center after the
impact.
One clue for a giant
crater came in 1994 when Hubble pictures showed
that one side of Vesta's football shape appeared
flattened. "We knew then there was something on
Vesta that was unusual," says Thomas.
The astronomers had to
wait for a better view from Hubble when Vesta made
it closest approach to Earth in a decade, in May
1996, when the asteroid was 110 million miles
away.
A total of 78 Wide Field
Planetary Camera 2 pictures were taken. The team
then created a topographic model of the asteroid's
surface by noting surface irregularities along the
limb and at the terminator (day/night boundary)
where shadows are enhanced by the low Sun
angle.
The immense crater lies
near the asteroid's south pole. This is probably
more than coincidental, say researchers. The
excavation of so much material from one side of the
asteroid would have shifted its rotation axis so
that it settled with the crater near one
pole.
Unlike some other large
asteroids that have jumbled surfaces due to the
asteroids breakup and recollapse, the rest of
Vesta's surface is largely intact, despite the
cataclysm. This is based on previous measurements
showing it has a surface of basaltic rock - frozen
lava - which oozed out of the asteroid's presumably
hot interior shortly after its formation 4.5
billion years ago, and has remained largely intact
ever since.
Approximately six percent
of the meteorites that fall to Earth are similar to
Vesta's mineralogical signature, as indicated by
their spectral characteristics. Vesta's spectrum is
unique among all the larger asteroids. The crater
may be the ultimate source of many of these
meteorites.
Most meteorites are
believed to come from other asteroids, but their
specific objects of origin cannot be determined in
most cases. Thus the distinctive mineralogical
makeup of these meteorites means that Vesta is the
only world other than the Earth, the Moon and Mars
for which scientists have samples of specifically
known origin.
A mystery has been that
the meteorites could not have traveled directly
from Vesta because at Vesta's location in the
asteroid belt, there are no perturbing
gravitational forces which would cause pieces to
fall into orbits intersecting the inner planets
like apples shaken out of a tree. However, Vesta's
"daughter" asteroids -- literally "chips off the
block" which have color characteristics similar to
Vesta, are near a "chaotic zone" in the asteroid
belt where Jupiter's gravitational tug can redirect
fragments into orbits which intersect Earth's
orbit.
A good determination of
the shape of Vesta was necessary for the next step
in interpretation, which will use multi-color
images of Vesta obtained with HST to study the
detailed mineralogy of surface regions including
the region of the giant crater. Also, a team led by
Don McCarthy of The University of Arizona plans to
obtain additional images of Vesta at longer
wavelengths this fall using the new Near Infrared
and Multi-Object Spectrometer (NICMOS) science
instrument on board Hubble.
Members of the Vesta
research team are Principal Investigator Ben
Zellner of Georgia Southern University; the
Co-Investigators are Richard Binzel, MIT, Michael
Gaffey, Rensselaer Polytechnic Institute, Alex
Storrs, Space Telescope Science Institute, Peter
Thomas, Cornell University and Dr. Ed Wells,
Computer Sciences Corporation.
The Space Telescope
Science Institute is operated by the Association of
Universities for Research in Astronomy, Inc. (AURA)
for NASA, under contract with the Goddard Space
Flight Center, Greenbelt, MD. The Hubble Space
Telescope is a project of international cooperation
between NASA and the European Space Agency
(ESA).
July 1,
1997
HST Update:
World's Most Powerful Telescopes Team Up
With A Lens In Nature To Discover Farthest Galaxy In The
Universe
(Go back to the most
recent update)
Star Cluster Used as Lens
An international team of astronomers has
discovered the most distant galaxy found in the
universe to date, by combining the unique sharpness
of the images from NASA's Hubble Space Telescope
with the light-collecting power of the W. M. Keck
Telescopes -- with an added boost from a
gravitational lens in space.
The results show the young
galaxy is as far as 13 billion light-years from us,
based on an estimated age for the universe of
approximately 14 billion years. This would place
the galaxy far back in time during the "formative
years" of galaxy birth and evolution, less than a
billion years after the birth of the universe in
the Big Bang.
The detailed image shows
that bright dense knots of massive stars power this
object. Due to the firestorm of starbirth within
it, the galaxy is intrinsically one of the
brightest young galaxies in the universe, blazing
with the brilliance of more than ten times our own
Milky Way.
Predicted by Einstein's
theory of general relativity, gravitational lenses
are collections of matter (such as clusters of
galaxies) that are so massive they warp space in
their vicinity, allowing the light of even
more-distant objects to curve around the central
lens-mass and be seen from Earth as greatly
magnified.
If dust rises to the
elevations where the water-ice clouds form, ice
condenses on dust grains and the heavier ice/dust
particles quickly fall back out of the atmosphere.
Though the dust could extend at low altitudes over
the landing site, researchers say current
prevailing winds should take the dust northward.
"If dust diffuses to the
landing site, the sky could turn out to be pink
like that seen by Viking," says Philip James of the
University of Toledo. Otherwise, Pathfinder will
likely show blue sky with bright clouds."
The imaging team includes
Steve Lee of the University of Colorado at
Boulder's Laboratory for Atmospheric and Space
Physics, Todd Clancy of Boulder's Space Science
Institute, Phillip James of the University of
Toledo, Mike Wolff of the Space Science Institute
and Jim Bell of Cornell University.
Images and text reproduced
for educational use with permission from The Space
Telescope Science Institute. The Space Telescope
Science Institute is operated by the Association of
Universities for Research in Astronomy, Inc.
(AURA), for NASA, under contract with the Goddard
Space Flight Center. The Hubble Space Telescope is
a project of international cooperation between NASA
and the European Space Agency (ESA).
June 19, 1997
HST Update:
Pele Erupts on Io
(Go back to the most
recent update)
Eruption on limb of Io
The Hubble Space Telescope has snapped a picture
of a 400-km-high (250-mile-high) plume of gas and
dust from a volcanic eruption on Io, Jupiter Io was
passing in front of Jupiter when this image was
taken by the Wide Field and Planetary Camera 2 in
July 1996.
The plume appears as an
orange patch just off the edge of Io in the eight
o'clock position, against the blue background of
Jupiter's clouds. Io's volcanic eruptions blasts
material hundreds of kilometers into space in giant
plumes of gas and dust. In this image, material
must have been blown out of the volcano at more
than 2,000 mph to form aplume of this size, which
is the largest yet seen on Io.
Until now, these plumes
have only been seen by spacecraft near Jupiter, and
their detection from the Earth-orbiting Hubble
Space Telescope opens up new opportunities for
long-term studies of these remarkable phenomena.
The plume seen here is
from Pele, one of Io's most powerful volcanos.
Pele's eruptions have been seen before. In March
1979, the Voyager 1 spacecraft recorded a
300-km-high eruption cloud from Pele. But the
volcano was inactive when the Voyager 2 spacecraft
flew by Jupiter in July 1979. This Hubble
observation is the first glimpse of a Pele eruption
plume since the Voyager expeditions.
Io's volcanic plumes are
much taller than those produced by terrestrial
volcanos because of a combination of factors. The
moon's thin atmosphere offers no resistance to the
expanding volcanic gases; its weak gravity
(one-sixth that of Earth) allows material to climb
higher before falling; and its biggest volcanos are
more powerful than most of Earth's volcanos.
This image is a
contrast-enhanced composite of an ultraviolet image
(2600 Angstrom wavelength), shown in blue, and a
violet image (4100 Angstrom wavelength), shown in
orange. The orange color probably occurs because of
the absorption and/or scattering of ultraviolet
light in the plume. This light from Jupiter passes
through the plume and is absorbed by sulfur dioxide
gas or is scattered by fine dust, or both, while
violet light passes through unimpeded. Future HST
observations may be able to distinguish between the
gas and dust explanations.
Images and text reproduced
for educational use with permission from The Space
Telescope Science Institute. The Space Telescope
Science Institute is operated by the Association of
Universities for Research in Astronomy, Inc.
(AURA), for NASA, under contract with the Goddard
Space Flight Center. The Hubble Space Telescope is
a project of international cooperation between NASA
and the European Space Agency (ESA).
May 20, 1997
HST Update:
Hubble Finds Cloudy, Cold Weather For Mars
Spacecraft
(Go back to the most
recent update)
Global Weather Map of Mars
As two NASA spacecraft speed toward a mid-year
rendezvous with Mars, astronomers using the Hubble
Space Telescope are providing updated planetary
weather reports to help plan the missions.
Hubble's new images show
that the "martian invasion" of spacecraft will
experience considerably different weather
conditions than seen by the last U.S. spacecraft to
land on Mars 21 years ago.
Martian atmospheric
conditions will affect the operation of both the
Mars Pathfinder landing on July 4, and the
September 11 arrival of the Mars Global Surveyor
which will map the planet from orbit. Hubble images
taken barely three weeks apart, on March 10 and
March 30, reveal dramatic changes in some local
conditions, and show overall cloudier and colder
conditions than Viking encountered two decades ago.
(con't) "Because
Pathfinder uses the atmosphere to decrease its
velocity for landing, and because the lander and
rover are solar-powered, understanding the state of
the atmosphere prior to landing is important," said
Dr. Matthew Golombek, Pathfinder project scientist
at NASA's Jet Propulsion Laboratory, Pasadena, CA.
"On July 4, Mars
Pathfinder will enter the atmosphere directly from
approach and slow itself behind an aeroshell with a
parachute, small solid rockets and giant airbags.
The lander carries a small rover to explore the
surface and investigate the kinds of materials
present. Hubble images of Mars are helping us to
adjust our flight path for landing and effectively
plan surface operations," said Golombek.
"It's not the dusty Mars
of the Project Viking days (mid 1970s to early
1980s) or the habitable oasis of science fiction
stories," says Todd Clancy of the Space Science
Institute in Boulder, CO. "We're finding a Mars
that's colder, clearer, cloudier. Hubble is rapidly
changing our view of Mars' environment. The
planet's weather apparently has a flip-side to it."
Hubble's findings also
offer new insights into the differences and
similarities of weather on the other terrestrial
planets. "The planets are similar in many important
ways, so the very major differences between them
are interesting from a viewpoint of understanding
meteorology better," said team leader Phil James of
the University of Toledo in Ohio. "Hubble is
allowing us to look at Mars in ways never before
seen."
In September, NASA's Mars
Global Surveyor will skim across the upper martian
atmosphere to slow down by friction and enter orbit
around the red planet. Atmospheric density is a key
factor in precisely executing this complex and
delicate aerobraking maneuver. Hubble is ideal for
tracking regional dust storms which could pose a
threat to Surveyor by drastically changing the
planet's air density. Such storms can cause a
tenfold increase in the martian atmosphere's drag
at 60 miles above the surface.
Comparing the appearance
of Mars to that in earlier spacecraft observations,
Hubble has found some areas of the martian surface
that have been changed dramatically by wind-blown
dust. The most prominent example is the "classic
dark feature" called Cerberus, which is roughly the
size of California (800 by 250 miles). This feature
has been seen as a low albedo (dark) region by
ground-based telescopic observers since early this
century, and was studied in detail by the Mariner 9
and Viking orbiters in the 1970s.
In Hubble's view, only
three dark splotches remain, probably related to
dark sand being carried out of craters by the wind.
The astronomers think that dust storms in the
region have covered the formerly dark surface with
bright dust, effectively erasing Cerberus from the
map.
Hubble is ideally suited
for long-term study of Mars. When Mars has been
closest to Earth, Hubble has resolved surface
details as small as 25 miles across. This allows
astronomers to track subtleties in the shifting
cloud patterns and periodic dust storms. This
planet-wide "weather satellite" view is
complementary to the close-up views which will be
provided by Mars Pathfinder and Mars Global
Surveyor.
Images and text reproduced
for educational use with permission from The Space
Telescope Science Institute. The Space Telescope
Science Institute is operated by the Association of
Universities for Research in Astronomy, Inc.
(AURA), for NASA, under contract with the Goddard
Space Flight Center. The Hubble Space Telescope is
a project of international cooperation between NASA
and the European Space Agency (ESA).
|