PUBLIC INFORMATION OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109. TELEPHONE (818) 354-5011
http://www.jpl.nasa.gov
Mars Pathfinder Mission Status
July 7, 1997
1 p.m. Pacific Daylight Time
Moderate weather yesterday, temperatures hovering around
minus 76 degrees Fahrenheit, pressure about 6.8 millibars, steady
light winds blowing from the southeast. Afternoon temperatures
reached about 10 degrees Fahrenheit. The forecast for today: 10
degrees Fahrenheit, cooling overnight to about minus 105 degrees
Fahrenheit.
A little extreme for an Earthly weather report? Perhaps, but
with that, scientists on the Mars Pathfinder mission today
presented the first weather report from Ares Vallis, an outflow
channel on the surface of Mars.
Four days into surface operations, the Mars Pathfinder
lander, rover and instruments are performing perfectly and
returning a wealth of new data on the rocks, soils and atmosphere
of Mars.
"The site is everything we hoped it would be," said Dr.
Matthew Golombek, Pathfinder project scientist, at a 10 a.m. PDT
press briefing. "We are finding more and more surprises as we
look in detail at the rocks and terrain."
Images presented this morning included the first photograph
of the lander taken by the rover. The image showed final
retraction of the airbags in a very high, puffy clump that
blocked most of the lander from view.
Meanwhile, the lander's Imager for Mars Pathfinder (IMP)
camera has provided a new perspective on rocks and hills on the
Martian horizon now that it is deployed on its mast and
photographing the site at an elevation of 1.0 meters (3.2 feet)
above the lander, said Dr. Peter Smith, IMP principal
investigator from the University of Arizona.
Another new image presented this morning showed Sojourner
Truth, the 23-pound rover that has begun to explore rocks around
the landing site, as it was gathering data overnight on "Barnacle
Bill." This rock, which was about 36 centimeters (1.2 feet) from
the rover after it exited the lander, is thought to be about 8-
to-10-inches tall, Smith said, and has a very distinctive surface
that looks almost as if it is covered with barnacle-shaped
objects.
"Here we have proof that Sojourner sort of nestled up and
kissed Barnacle Bill," Golombek said as the photograph was
presented.
"We have also received data from the rover's first soil
experiment. The APXS (alpha proton X-ray spectrometer) is
working perfectly," Golombek continued. "However, because we
started taking data earlier in the day than we originally
planned, the temperatures on Mars were warmer than the detectors
liked and we have a bit of noise in the spectra. The team needs
an extra day to try to figure out how to subtract that noise
out."
The science team said a full chemical analysis of both the
Martian soil and Barnacle Bill would be reported at tomorrow's 11
a.m. PDT press briefing. Meanwhile, Sojourner will travel to a
larger rock later today, called "Yogi," and study the composition
of the soil around it using the alpha proton X-ray spectrometer.
Several scientists have commented that a smooth depression of
soil around the rock resembles a moat.
Looking south at a pair of sloping hills, called "Twin
Peaks," that are about a mile away, Smith pointed out new
observations made possible by the fully deployed IMP camera. A
depression in the landscape in front of the peaks suggests the
presence of a channel. "This is actually a channel back behind
those rocks, we're on the edge of a channel," he said.
A high resolution close-up of the Martian soil near the base
of the lander also revealed a texture perfectly preserved in the
Martian environment. Dr. Jim Bell of Cornell University explained
the calibration targets that are used to achieve the true color
of the Martian landscape. Color variations allow scientists to
identify different types of minerals that are present in the
environment. The bright reddish color of the soil, for example,
points to the presence of oxidized iron in surface materials.
"The surface of Mars is rusting," Bell said. "We don't know
when or how fast it's rusting, but we hope to find these things
out. Not all of the surfaces are the same, though. There's lots
of diversity and variation in the landscape. We can see some
surfaces that are much less red, for example, and more consistent
with volcanic rocks."
Building on comments made yesterday by Dr. Ronald Greeley
(Arizona State University) about the evidence for floods in this
region, Dr. Michael Malin, an interdisciplinary scientist, said
the floods were so catastrophic that they would have filled up
the Mediterranean basin here on Earth. Evidence, he said, can be
seen in the variety of rocks, sediments and "puddles" left in the
Martian soil that materials from the highlands were swept into
this flood basin.
A full color, 360-degree panorama of the Pathfinder landing
site will be presented at tomorrow's 11 a.m. press briefing, as
will data about the composition of the Martian soil and Barnacle
Bill.
Briefings are carried live on NASA TV, which is available on
GE-2, transponder 9C at 85 degrees west longitude, vertical
polarization, with a frequency of 3880 MHz, and audio of 6.8 MHz.
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