The ascent, which spanned 3 0.5 months and climbed 1,640 vertical feet (500 meters), included traversing grades of up to 20%. Along the way, Perseverance conducted scientific observations at multiple stops. The rover's progress and upcoming plans were shared during a Dec. 12 briefing at the American Geophysical Union's annual meeting in Washington.
"During the Jezero Crater rim climb, our rover drivers have done an amazing job negotiating some of the toughest terrain we've encountered since landing," said Steven Lee, deputy project manager for Perseverance at NASA's Jet Propulsion Laboratory in Southern California. "They developed innovative approaches to overcome these challenges - even tried driving backward to see if it would help - and the rover has come through it all like a champ. Perseverance is 'go' for everything the science team wants to throw at it during this next science campaign."
"This campaign brings us completely new scientific riches as Perseverance roves into fundamentally new geology," said Ken Farley, project scientist for Perseverance at Caltech. "It marks our transition from rocks that partially filled Jezero Crater when it was formed by a massive impact about 3.9 billion years ago to rocks from deep down inside Mars that were thrown upward to form the crater rim after impact."
Farley emphasized that these ancient rocks are among the oldest found in the solar system, holding potential insights into the early histories of Mars and Earth.
"The campaign starts off with a bang because Witch Hazel Hill represents over 330 feet of layered outcrop, where each layer is like a page in the book of Martian history," said Candice Bedford, a Perseverance scientist from Purdue University. "As we drive down the hill, we will be going back in time, investigating the ancient environments of Mars recorded in the crater rim. Then, after a steep descent, we take our first turns of the wheel away from the crater rim toward 'Lac de Charmes,' about 2 miles south."
The plains region known as Lac de Charmes is of particular interest due to its geological isolation from the Jezero Crater formation process.
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