Opportunity: Surveying to the southeast

4166-navcamSol 4166, October 13, 2015. Day by day, Opportunity is surveying the bare outcrops that line the Marathon Valley floor. On Sol 4166, it drove almost 19 meters (62 feet) to the southeast toward the southern wall of the valley. Above is a two-frame Navcam composite showing outcrops varying in tone, suggesting they also vary in composition, or at least degree of alteration, probably by water (click image to enlarge).

Opportunity raw images, its latest mission status, a location map. and atmospheric opacity, known as tau.

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MARCI weather report, October 5-11, 2015

releaseimg_151005_151011During the past week, the large dust storm north of Deuteronilus noted previously had quickly dissipated. In the southern hemisphere, dust storms were observed over Aonia and western Argyre. This activity later reached into Valles Marineris and obscured the canyon floors. As the aphelion cloud-belt continued to develop, water ice clouds over Alba Patera and some of the other Tharsis volcanoes became more optically thick during the afternoon hours… [More at link, including video]

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Curiosity update: ‘Dump and thwack’

PIA19920_modestSol 1133, October 13, 2015, update from USGS scientist Lauren Edgar: Sol 1133 activities are dominated by dumping the “Big Sky” sample and “thwacking” CHIMRA (the Collection and Handling for in-Situ Martian Rock Analysis) to clean out any remnants of the sample.  We have to do this in preparation for the next drill sample, which will likely be the “Greenhorn” target in tomorrow’s plan.  In addition to these arm activities, today’s plan includes several ChemCam and Mastcam observations of “Greenhorn” and “Gallatin Pass” to assess chemical variations across a fracture… [More at link]

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Free access to Gale Crater lakes Science papers

PIA19840_ipTwo of the papers published in Science (October 9, 2015) relating to the discovery of ancient lakes in Gale Crater have been posted online, with the full texts available without charge.

The papers are titled: “Deposition, exhumation, and paleoclimate of an ancient lake deposit, Gale crater, Mars” and “A Habitable Fluvio-Lacustrine Environment at Yellowknife Bay, Gale Crater, Mars.”

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Explaining valley networks with climate models

two valleysThe extensive valley networks on the surface of Mars were probably created by running water billions of years ago, but the source of that water is unknown. Now, a team of Penn State and NASA researchers is using climate models to predict how greenhouse warming could be the source of the water.

[Their study, “Testing the early Mars H2–CO2 greenhouse hypothesis with a 1-D photochemical model,” was published in Icarus.]

“Everyone is looking for life on Mars, and if Mars was habitable early on as indicated by flowing water, then the chances of there being some sort of life there now goes up,” said Natasha Batalha, lead author and graduate student in astronomy and astrophysics, Penn State. “Our work involves using models to best estimate what was happening on the surface of Mars 3.8 billion years ago.” [More at links]

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New Curiosity selfie at Big Sky drilling site

PIA19920_modestThis self-portrait of NASA’s Curiosity Mars rover shows the vehicle at the “Big Sky” site, where its drill collected the mission’s fifth taste of Mount Sharp.

The scene combines dozens of images taken during the 1,126th Martian day, or sol, of Curiosity’s work on Mars (Oct. 6, 2015, PDT), by the Mars Hand Lens Imager (MAHLI) camera at the end of the rover’s robotic arm. The rock drilled at this site is sandstone in the Stimson geological unit inside Gale Crater. The location is on cross-bedded sandstone in which the cross bedding is more evident in views from when the rover was approaching the area, such as http://mars.nasa.gov/multimedia/images/?ImageID=7468.

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THEMIS: The Martian, Part 3: Meridiani Planum

The Martian Meridiani Planum (THEMIS_IOTD_20151014)THEMIS Image of the Day, October 14, 2015. All this week, the THEMIS Image of the Day is following on the real Mars the path taken by fictional astronaut Mark Watney, stranded on the Red Planet in the book and movie, The Martian.

Today’s image shows a part of the flat terrain of northern Meridiani Planum. This area lies about 300 kilometers (190 miles) north of where Mars rover Opportunity is currently exploring the rim rocks of Endeavour Crater. Meridiani is a large expanse of sedimentary rock, mostly flat-lying basalt sandstone with hematite nodules (“blueberries”) embedded in it. Farther south from this scene, Opportunity has examined several craters like these that expose deeper rock layers. They show that the Meridiani sandstone is made of dune sands that were soaked in sulfur-rich water.

Flat terrain may make for dull scenery, but the driving is easy. This area is where astronaut Mark Watney turns his vehicle east toward Schiaparelli Crater. Before arriving here, he was driving south to get out from under a dust storm that threatened to shut off power to the vehicle’s solar cells. At this point he has journeyed about 2,300 kilometers (1,400 miles) from Acidalia.

More THEMIS Images of the Day by geological topic.

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Gale Crater river carried pebbles tens of km as bedload on Peace Vallis alluvial fan

Link outcrop Image1Rounded pebbles on Mars were transported for tens of kilometres in a river, suggests a new study published in Nature Communications [October 13, 2015]. This study makes use of a new technique that may help estimate the distance travelled by pebbles and small particles on other planets.

The discovery by the robotic rover Curiosity of small rounded pebbles in rock formations on Mars suggested that there were streams or rivers flowing on our neighbouring planet in the past, but interpretations regarding these have been uncertain. Reconstructions have suggested that the pebbles became rounded as they rolled, slid and hopped along a river bed, but how far they travelled has not been quantified. Pebble shape can be used to infer the amount of mass lost during particle transport by water, and this mass loss equates to the amount of transport experienced by the pebble.

Douglas Jerolmack [University of Pennsylvania] and colleagues used experiments as well as investigations of river-transported pebbles in Puerto Rico and the USA to show that the distance travelled by a pebble can be estimated using shape alone. They validated their model on Earth before using it to interpret the pebbles found in the Martian rock formations. [More at link]

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Curiosity update: ‘Dumping Big Sky sample’

CR0_497630665PRC_F0500676CCAM03128L1Sol 1132, October 12, 2015, update from USGS scientist Ken Herkenhoff: Columbus Day [October 12] is a federal holiday, but I’m scheduled as SOWG Chair tomorrow so I’m following Sol 1132 tactical planning and discussions of our goals for Sol 1133.  The SAM analysis of the Big Sky drill sample went well and there is no need for another analysis, so the rest of the sample will be dumped out of CHIMRA on Sol 1132.  MAHLI will take pictures of the dump target before and after the sample is dumped, then APXS…. [More at link]

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Opportunity: Searching for water-altered rocks

Sol 4165, October 12, 2015. 4165-pancam-fcMore scouting the outcrops on the Marathon Valley floor. The rocks of greatest interest are those that have a faint reddish tinge in false-color Pancam images (such as these by Holger Isenberg). These are believed to contain clay minerals, which can tell about the water-history of these rocks. (Click to enlarge.)

Opportunity raw images, its latest mission status, a location map. and atmospheric opacity, known as tau.

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