Curiosity resumes operations after switching back to Side-B computer

PIA23047-16Updated March 12, 2019, 10:40 a.m. PDT (1:40 p.m EDT): Curiosity experienced a computer reset on its Side-A computer on Wednesday, March 6, 2019 (Sol 2,339), that triggered the rover’s safe mode. This was the second computer reset in three weeks; both resets were related to the computer’s memory.

The mission team decided to switch from the Side-A computer back to the rover’s Side-B computer, which it operated on for most of the mission until November of 2018. Side-B recently experienced its own memory issue; the team has since further diagnosed the matter, reformatting the Side-B computer to isolate areas of “bad” memory. As of today, Curiosity is out of safe mode, and the team is configuring the rover for new science operations in the clay unit. Curiosity is expected to return to science operations as early as Wednesday… [More at link]

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MARCI weather report, March 4-10, 2019

MARCI-March-10-2019Dust-lifting activity continued in localized regions in both the northern and southern hemispheres of Mars this past week. Looking to the ancient southern highlands, local-scale dust storms propagated eastward from Sirenum to Aonia. Southern Noachis Terra also encountered a few transient dust-lifting events. Dusty conditions also occurred over the younger-looking plains of the northern hemisphere as the seasonal ice cap continued its seasonal retreat. Peering just south of this activity, some dust clouds traveled southward into the plains of Utopia and Chryse near the middle and end of the week… [More at link, including video]

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Opportunity: Last panorama and images

PIA22908_fig1Over 29 days last spring, NASA’s Mars Exploration Rover Opportunity documented this 360-degree panorama from multiple images taken at what would become its final resting spot in Perseverance Valley. Located on the inner slope of the western rim of Endurance Crater, Perseverance Valley is a system of shallow troughs descending eastward about the length of two football fields from the crest of Endeavor’s rim to its floor.

“This final panorama embodies what made our Opportunity rover such a remarkable mission of exploration and discovery,” said Opportunity project manager John Callas of NASA’s Jet Propulsion Laboratory in Pasadena, California. [Ed. note: Click image above to see full annotated panorama.]

“To the right of center you can see the rim of Endeavor Crater rising in the distance. Just to the left of that, rover tracks begin their descent from over the horizon and weave their way down to geologic features that our scientists wanted to examine up close. And to the far right and left are the bottom of Perseverance Valley and the floor of Endeavour crater, pristine and unexplored, waiting for visits from future explorers.” [More at link, including final data and images]

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MAVEN: High solar wind pressure hastens loss of atmosphere

53864576_10157365482347868_5534831089140367360_nNew MAVEN research shows that high solar wind pressure influences Mars’ magnetic fields in ways that can increase the global loss of atmosphere to space.

Planetary atmospheres are constantly bombarded by energy and radiation from the Sun, and over time this energy input can strip away an atmosphere to space. This process has been particularly devastating at Mars, where the loss of most of its original atmosphere has left the planet cold and desolate.

This loss may have been in part due to the planet’s lack of a global magnetic field. While the Earth possesses a large magnetic field that diverts much of the solar energy input, Mars does not. However, Mars does possess smaller pockets of magnetic field that are rooted in the planet’s crust and extend outward through the atmosphere, a unique feature in the solar system.

These magnetic fields are able to shield Mars’ atmosphere on a small scale but are susceptible to changes in the strength of solar activity. MAVEN scientists have demonstrated [in the journal Geophysical Research Letters] that during these periods of increased solar output, the magnetic pockets across Mars are compressed to a smaller size, leaving the planet’s atmosphere more exposed and more likely to escape to space. [More at links]

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HiRISE: Uncommon clay

ESP_054681_1475Uncommon clay. There are some uncommon clays in this sedimentary plain, as first detected in low resolution by the OMEGA instrument on the Mars Express Orbiter. Note the tight cluster of impacts. This image is in the Terra Cimmeria region of Mars.

HiRISE Picture of the Day archive [More at links]

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THEMIS: Big impacts and little in Terra Cimmeria

Terra Cimmeria craters (THEMIS_IOTD_20190313)THEMIS Image of the Day, March 13, 2019. This VIS image contains three craters. There is a quarter of the largest crater in the top half of the image, half of a smaller crater at the very top, and the full crater in the lower half of the image.

Investigating the relative ages of each crater indicates the largest crater formed first followed at some point by the smaller craters – the half-crater at the top occurs on top of the big crater as does the ejecta from the bottom crater.

Because the visible ejecta does not reach the smaller crater at the top it is difficult to determine the relative ages of the two smaller craters. Both have similar floor morphology, but different rim morphology. The crater in the bottom of the image has a very complex rim, including both rim gullies (top side) and ridge and spur eroded features (bottom side).

These differences may be related to the different materials of the largest crater. One crater impacted into the floor and the other into the ejecta blanket of the largest crater. Near surface morphology as well as deeper materials can modify the pressure wave created by impact. These craters are located in Terra Cimmeria.

Explore more THEMIS Images of the Day by geological subject.

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HiRISE: Streaking on Mars

ESP_054686_1825Streaking on Mars. Wind streaking, that is. Here’s the suggester’s rationale for acquiring this image: “There’s a field of two-tailed bright wind streaks here that are really neat. They seem unique to the area. It would be nice to get a closer look.” Indeed.

HiRISE Picture of the Day archive [More at links]

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Latest weather at Gale Crater and Elysium Planitia

Daily Elysium charts and data (temperature, wind speed, atmospheric pressure) here.

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THEMIS: Daedalia Planum lava flows

Daedalia Planum flows (THEMIS_IOTD_20190312)THEMIS Image of the Day, March 12, 2019. Today’s VIS image shows a small part of Daedalia Planum.(Note that sunlight in this image is coming from the right.)

The lava flows originate from Arsia Mons, one of the large volcanoes in the Tharsis region. The different surface textures are created by differences in the lava viscosity and cooling rates. The lobate margins of each flow can be traced back to the start of each flow – or to the point where they are covered by younger flows. Flows in Daedalia Planum can be as long as 180 km.

Explore more THEMIS Images of the Day by geological subject.

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HiRISE: A margin of lava

ESP_054681_1835A margin of lava. This lava margin in Cerberus Palus is part of the Athabasca Valles flow. There are also lava coils in this region, something we did not know existed on Mars until HiRISE took an image. The lava coils are extremely long as compared to those that form on Earth.

HiRISE Picture of the Day archive [More at links]

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