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Mars Pathfinder Update - 07/09/97
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 9, 1997
3 p.m. Pacific Daylight Time
Six days after landing in an ancient outflow channel called
Ares Vallis, the Mars Pathfinder lander and rover continue to
operate extremely well, returning unprecedented amounts of data
during daily downlink sessions.
Yesterday, Pathfinder returned 85 megabits of data on the
Martian atmosphere, weather, soil and a rock called "Barnacle
Bill," the first rock on Mars ever to be studied up close and
personal. Additional rover and lander imaging was also returned.
Tonight the operations team will perform a low-gain antenna
session
from 6:30 p.m.- 7 p.m. PDT to acquire data on the health of the
lander and rover. A three-hour high-gain transmission will begin
later this evening, at 10 p.m. - 1:30 a.m. PDT, at the higher
data rate.
The rover has completed its soil analysis of the smooth,
moat-like terrain around a large boulder named "Yogi." After
completing the analysis, the rover retracted the alpha proton X-
ray spectrometer, then conducted a wheel abrasion experiment in
which it dug into the soil and disturbed the crusty material as
it was turning its wheels. This soil abrasion test is one of
many technology and mobility experiments planned for the rover to
help engineers understand the dynamics of its mobility on Martian
soil for future generations of rovers.
"We used the rover as sort of a bulldozer to push this rock
and crusty material up," said Dr. Matthew Golombek, Pathfinder
project scientist at a 1 p.m. PDT press briefing. "Next the
rover moved slightly to the left and imaged Yogi with its front
cameras, then turned around and imaged the lander with its front
cameras. After that, the rover will photograph Yogi at close
range. That data will be returned tonight."
Further preliminary analysis of "Barnacle Bill" showed that
its texture seems to be consistent with volcanic "andesites," the
second most common volcanic rock on Earth, said Dr. Jeff Johnson,
of the U.S. Geological Survey in Flagstaff, AZ, who is on the
Imager for Mars Pathfinder (IMP) camera team.
Scientists will use reflectance spectra collected by the
lander and rover cameras to determine whether the rock, which
measures about 40 centimeters (1.3 feet) across and 1.1 to 1.5
centimeters (8-to-10-inches) tall, is a sedimentary rock composed
of many different rock fragments, or whether it is "homogenous,"
which would be consistent with scientists' first impression that
it is a volcanic rock.
On a lighter note, Dr. Peter Smith, principal investigator
of the IMP team, shared some of his personal insights on what
it's like to be living on local Mars time, which means working on
a 24-hour, 37-minute clock each day.
"When you say good morning, and the sun is setting, now
that's living on Martian solar time. When your sunglasses start
looking like this (holding up the red-and-blue stereo glasses
used to view images in 3-D), that's living on Martian time. When
you start admiring strange-looking rocks and giving them names,
then telling your friends, that's living on Martian time. When
your days are called Sols, and your nights are called days,
that's living on Martian time. But when you start laughing at the
engineers' jokes, you know you're living on Martian time."
Next on the rover's schedule of investigations are two rocks
that appear white or very light in color: "Casper" and "Scubee-
Dubee-Doo," located off to the left of the Pathfinder lander.
Among the many images planned in the next week are shots of the
Martian sunset and sunrise; pictures of the Martian moons Phobos
and Deimos; and pictures of "Twin Peaks," two sloping hills that
are about 800 meters (about half a mile) away from the landing
site.
The next scheduled press briefing will be held at 12:30 p.m.
Pacific Daylight Time on July 10 in JPL's von Karman Auditorium.
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