Octavia E. Butler accelerating again on touchdown

NASA Perseverance Rover Drive

Three abrasions and 4 pattern cores later, the rover has lastly left the SITA area and continues on the return leg of the crater flooring expedition. A significant distinction between the “out” journey and this return journey is the driving velocity of the fixture. As we headed towards Seta earlier within the mission, our common every day drive distance was shorter, partly as a result of we had been doing scientific reconnaissance at necessary stops alongside the best way, and partly as a result of we had been nonetheless studying how one can drive with our rover. The best way to maximize effectivity. Now, on the return journey to Octavia E. Butler’s Touchdown, we’re going again at excessive velocity!

Since leaving Seetah a couple of days in the past, Perseverance has already logged two large record-setting 240+ meter drives at 340 and 341. these drives set file For the longest single-sol complete distance recorded by any Martian rover (243.3 m) and single-sol autonav file by any Martian rover (226.5 m). If it is a signal of an impending drive sooner or later, we’ll be zooming by way of the remainder of the crater flooring marketing campaign to Delta very quickly.

Mars Persistence Sol 345

Mars Perseverance Sol 345 – Entrance Left Hazard Avoidance Digital camera: NASA’s Mars Perseverance rover acquired this picture of the area in entrance of it utilizing its onboard Entrance Left Hazard Avoidance Digital camera A. This picture exhibits the rover arm reaching the Rimplus outcrop, taken right here. our present location. The particles layers beneath this outcrop would be the focus of friction and proximity science with PIXL, SHERLOC, and WATSON on the subsequent few flooring. credit score: NASA/JPL-Caltech

So the place are we now? We’re at the moment in entrance of an outcrop known as “Rimplas”, on our option to a fast abrasion and proximity science pit cease (should get our final samples from the cease crater flooring sooner or later – keep tuned for future weblog posts) !) This location is near the place the firmament was about 170 years in the past 177 years in the past, close to the Artubi outcrop the place we noticed the intriguing layered rocks. We now contemplate these layered rocks to be a part of the Artubi “members” (a gaggle of rocks with frequent traits) beneath the Rochette Caprock Member, which had been sampled in our first rock core. These enigmatic layers haven’t but been eroded and studied intimately with the PIXL, SHERLOC, and WATSON devices, so our present cease is on the layered rocks within the rimplasse. This is hoping we’ve got our 6 . Will occurth Friction patches this weekend!

Written by Vivian Solar, Science Operations Techniques Engineer, Employees Scientist NASA,JPL

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