Even rover will leave Vera Rubin Ridge


This shot from the Mast Camera (Mastcam) on Mars Rover Curiosity NASA was released on December 19 (Sun 2265). The rover's ultimate drill site on Vera Rubin Ridge is shown, apart from the crystal department, it will cost the next year; explored. Credit: NASA / JPL-Caltech / MSSS

After exploring Mars & Vera Rubin Ridge for over a year, Curiosity rover recently moved on. But a new 360-video can be enabled. public visit the Curiosity on the ridge, a region called "Rock Hall". A video was created from a broader view by the rover on December 19. It's a & # 39; including images of its next destination – an area that the crew has been calling the "clay unit" and recently named "Torridon Glen – and the floor of Gale Crater, home to Mount Sharp, the geverical thing the rover has been dating from 2014.

Although the rover is left on the back, the Curiosity team still tells a story about creating. Although there have been a number of walks to date, none have to explain in general why the ridge has stopped eroding compared to the # 39; granite around it. But the rover's investigation found that the ridge-shaped rocks were sediment set in an old lake, similar to rock rigs under the ridge.

"We have made a great deal of opportunity," said Abigail Fraeman, a member of the NAS Science Propulsion Laboratory curricular team in Pasadena, California. "We leave with a different view of the ridge than our ones."

NASA was an orbiter that was checking its & # 39; The back has marked a strong indicator of hematite, a mineral mineral, often in water. He reported hematite, along with other signs of old water, such as crystals. These signs appeared in packets, causing the crew to expect surface water affecting some of the back over their legs over time differently than others. Another search was that the hematite names were not always mapped with a & quot; corresponding to the space from space.

"All the way helps us to understand the reasons that affect our campaigns to see Mars," said Fraeman . "Looking up at a rover, let's find a lot more of these hematite names. It shows how orbiter and rover science contributes to each other. "

The ridge has also been a backdrop for a roller-coaster year: vigorousness returned active, just with stunning hard rock only. Despite this, the team got samples from the three main rock of the ridge. To find around memory memory, engineers also made rover computers (the spacecraft was designed by two to keep it on track if a person catches it). Although the case is still proven, work has been adversely affected by its & # 39; mission.

The new rover home, Glen Torridon, is in excavation between Vera Rubin Ridge and its rest of the mountain. The clay unit to this area is because of it; Data shows that the rocks in which there are waterproof miners and that it can give scientists more knowledge of the oldest lochs that were present in the Gale Crater out and throughout the early history Post-

"As well as identifying a previous wet environment, it is known that the clay minerals will be absorbed and preserved organic bullets," said Scientist Curiosity Ashwin Vasavada Project of JPL. "That's making this area is particularly promising, and the team is already reviewing the area for the next drill site."

Finding anxiety of both crude minerals and organic molecules in many of the drowned rocks since they came ashore in 2012. Organic molecules are chemicals. If both the water and the organic bulbs were present when the rocks were created, the clay unit could be an example of an old habitat that lived on an old Mars-place that could be & # 39; Supporting life, if it ever been.

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