“If HiRISE took the image one second before or one second after, we probably would be looking at an empty Martian landscape,” said Sarah Milkovich, HiRISE investigation scientist at the Jet Propulsion Laboratory (JPL) in Pasadena, Calif. “When you consider that we have been working on this sequence since March and had to upload commands to the spacecraft about 72 hours prior to the image being taken, you begin to realize how challenging this picture was to obtain.”
“Guess you could consider us the closest thing to paparazzi on Mars,” said Milkovich. “We definitely caught NASA’s newest celebrity in the act.”
Curiosity, NASA’s latest contribution to the Martian landscape, landed at 10:32 p.m. PDT Aug. 5 (1:32 a.m. EDT Aug. 6) near the foot of a three-mile tall mountain inside Gale Crater, which is 96 miles in diameter.
In other Curiosity news, one part of the rover team at JPL continues to review the data from Sunday night’s landing while another continues to prepare the 1-ton mobile laboratory for its future explorations of Gale Crater. One key assignment given to Curiosity for its first full day on Mars is to raise its high-gain antenna. Using this antenna will increase the data rate the rover can communicate directly with Earth. The mission will use relays to orbiters as the primary method for sending data home because that method is much more energy efficient for the rover.
Curiosity carries 10 science instruments with a total mass 15 times as large as the science payloads on the Mars rovers Spirit and Opportunity. Some of the tools, such as a laser-firing instrument for checking rocks’ elemental composition from a distance, are the first of their kind on Mars. Curiosity will use a drill and scoop which is located at the end of its robotic arm to gather soil and powdered samples of rock interiors, then sieve and parcel out these samples into the rover’s analytical laboratory instruments.
To handle this science toolkit, Curiosity is twice as long and five times as heavy as Spirit or Opportunity. The Gale Crater landing site places the rover within driving distance of layers of the crater’s interior mountain. Observations from orbit have identified clay and sulfate minerals in the lower layers, indicating a wet history.