The 4-year-old atmosphere-sniffing MAVEN mission is embarking on a new campaign today to tighten its orbit around Mars. The operation will reduce the highest point of the MAVEN spacecraft’s elliptical orbit from 3,850 to 2,800 miles (6,200 to 4,500 kilometers) above the surface and prepare it to take on additional responsibility as a data-relay satellite for NASA’s Mars 2020 rover, which launches next year.
“The MAVEN spacecraft has done a phenomenal job teaching us how Mars lost its atmosphere and providing other important scientific insights on the evolution of the Martian climate,” said Jim Watzin, director of NASA’s Mars Exploration Program. “Now we’re recruiting it to help NASA communicate with our forthcoming Mars rover and its successors.”
While MAVEN’s new orbit will not be drastically shorter than its present orbit, even this small change will significantly improve its communications capabilities. “It’s like using your cell phone,” said Bruce Jakosky, MAVEN principal investigator from the University of Colorado Boulder. “The closer you are to a cell tower, the stronger your signal.” [More at link]
Sols 2315-17, February 11, 2019, update by MSL scientist Suzanne Schwenzer: Curiosity is driving across the clay-bearing unit, which is still a very new terrain with many details yet to be understood. The region is covered in little pebbles – and has lots of small sand patches, too, both of which we continue to investigate. The Navigation camera image above shows the APXS being deployed on the sand patch Alba that was investigated on sol 2313. After that, the drive took us a little further north, to be exact, Curiosity drove 39 metres from the last location.
The parking location presented us with the same pebbly-strewn surface as before, with the occasional small sand feature. With this terrain being new, and some small-scale sedimentary features spotted by the eagle-eyed sedimentologists on the team, we decided to use ChemCam on three pebbly targets, “Dauntless,” “Otter,” and Thistle.” The team also found – for the first time in this new unit – a pebble large enough to get a full APXS raster on one continuous piece of rock. Yes, this is how small the pebbles are! We used the opportunity, named the target “Emerald,” and investigated it using a 3-spot APXS raster… [More at link]
An elongated pit in Margaritifer Terra. There is nothing more interesting than a feature that resembles a giant amoeba. Margaritifer Terra is an ancient, heavily cratered region, centered just south of the Martian equator, and covers 2600 kilometers at its widest extent.
No signal from Opportunity has been heard since Sol 5111 (June 10, 2018) during the historic global dust storm. Opportunity likely experienced a low-power fault, a mission clock fault and an up-loss timer fault. The team is continuing to listen for the rover over a broad range of times, frequencies and polarizations using the Deep Space Network (DSN) Radio Science Receiver.
The team has begun mission clock fault recovery commanding “in the blind,” in the hopes of catching the rover during an awake period, as their strategy of last resort. Since loss of signal, over 835 recovery commands have been radiated to the rover. [More at link]
THEMIS Image of the Day, February 11, 2019. Today’s VIS image shows part of the extensive volcanic flows that make up Daedalia Planum. The different layers and surface textures are due to flows at different times, or the affect of cooling as the flow narrows and extends far from the lava source.
Daedalia Planum volcanic flows originate at or near Arsia Mons.
In this image the ripples in the sand tell us which way the wind was moving and how it was diverted around these rock formations. (Typically the wind direction is perpendicular to the crest of the dune or in this case, the ripples.) [More at link]
After exploring Mars’ Vera Rubin Ridge for more than a year, NASA’s Curiosity rover recently moved on. But a new 360-video lets the public visit Curiosity’s final drill site on the ridge, an area nicknamed “Rock Hall.” The video was created from a panorama taken by the rover on Dec. 19. It includes images of its next destination – an area the team has been calling the “clay-bearing unit” and recently named “Glen Torridon” – and the floor of Gale Crater, home to Mount Sharp, the geological feature the rover has been climbing since 2014.
Even though the rover has left the ridge, Curiosity’s team is still piecing together the story of its formation. While there have been a number of clues so far, none fully explains why the ridge has resisted erosion compared with the bedrock around it. But the rover’s investigation did find that the rocks of the ridge formed as sediment settled in an ancient lake, similar to rock layers below the ridge.
“We’ve had our fair share of surprises,” said Curiosity science team member Abigail Fraeman of NASA’s Jet Propulsion Laboratory in Pasadena, California. “We’re leaving with a different perspective of the ridge than what we had before.”
A NASA orbiter studying the ridge had previously identified a strong signal from hematite, an iron-rich mineral that often forms in water. Curiosity confirmed the presence of hematite, along with other signs of ancient water, like crystals. These signs appeared in patches… [More at link]
THEMIS Image of the Day, February 8, 2019. Sand dunes cover part of the floor of this unnamed crater in Noachis Terra. Their dark tint suggests they are relatively free of light-toned dust, hence probably active under winds currently.