What the Spirit rover’s Microscopic Imager found

herkenhoff-figure-11[Editor’s note: From a paper by Ken Herkenhoff and 31 co-authors recently published in the Journal of Geophysical Research.]

Overview of Spirit Microscopic Imager Results

The Microscopic Imager (MI) on NASA’s Spirit rover returned the highest‐resolution images of the Martian surface available at the time of the 2004‐2010 mission. Designed to survive 90 Mars days (sols) and search for evidence of water in the past, Spirit returned data for 2210 sols, far exceeding all expectations.

This paper summarizes the scientific insights gleaned from the thousands of MI images acquired during the last five years of the mission, supplementing the summary of the first 450 sols of the Spirit MI investigation published previously (Herkenhoff et al., 2006). Along with data from the other instruments on Spirit, MI images guided the scientific interpretation of the geologic history of the rocks and soils observed in Gusev crater on Mars.

We conclude that the geologic history of the area explored by Spirit has been dominated by impacts and volcanism, and that water, perhaps very hot water, was involved in the evolution of some of the rocks and soils. More recently, winds have moved soil particles and abraded rocks, as observed elsewhere on Mars.

These results have improved our understanding of Mars’ history and informed planning of future missions to Mars. [More at link]

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HiRISE: Spring frost on a cold world

PSP_007448_2475Winter on Mars comes with a blanket of carbon dioxide snow. During the spring “thaw,” this snow evaporates into the atmosphere, lingering longest in the shallow depressions such as the troughs of polygon patterned ground.

Enhanced color shows the carbon dioxide snow as bluish-white patches among areas of rusty red bare ground. We took this image in 2008 as a possible landing site for the Phoenix Lander that arrived on Mars later that same year. [More at link]

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‘SpaceBok’ hopping robot tested in ESA Mars Yard

SpaceBok_robot_node_full_image_2This walking and hopping robot is currently being tested in European Space Agency’s Mars Yard. SpaceBok is a quadruped robot designed by a Swiss student team from ETH Zurich and ZHAW Zurich, under the supervision of Professor Marco Hutter and PhD student Hendrik Kolvenbach, for future missions to the Moon or Mars.

“Legged robots can traverse unstructured terrain and could be used to explore areas of interest, such as craters, which rovers are unable to reach,” explains team member Patrick Barton. “As they are very versatile, they can change gait to adapt to different terrain.”  [More at link]

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THEMIS: Active dunes in Noachis Terra

Active dune field in a crater (THEMIS_IOTD_20181128)THEMIS Image of the Day, November 28, 2018. Today’s VIS image shows a sand sheet with surface dunes forms on the floor of an unnamed crater in Noachis Terra.

Dark dunes indicate active dunes: Winds stir the sand, which kicks off the light-toned dust, leaving behind the sand. The sands’ dark tone comes from the breakdown of basalt, a dark volcanic rock common all over Mars.

See more THEMIS Images of the Day by geological subject.

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Weather update from Gale Crater

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HiRISE: Looking at martian salts and clays

PSP_005811_1470This 3D perspective view is a composite of both HiRISE and data from CRISM, another instrument onboard MRO. This view covers a small patch of ancient Martian real estate in Terra Sirenum.

CRISM collects spectral data that can be used as a chemical fingerprint for the upper most surface. This information suggests that this small patch of surface is covered with salts (chlorides) represented in green and water-rich clays that appear in blue.

CRISM colors can be added to high-resolution images to enhance our knowledge of these materials. They also match nicely with the surface features in our HiRISE image. For example, a fissure near the center of the image may be a a clue to the origin of the salts… [More at link]

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Curiosity: Mt. Sharp vista

2242-rmiSol 2242, November 26, 2018. While InSight was landing over in Elysium Planitia, Curiosity’s controllers directed the Remote Micro-Imager to shoot an 11-frame composite detailing layers in Mt. Sharp in Gale Crater. Click the image to enlarge it.

Sol 2242 raw images (from all cameras).

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InSight is catching rays on Mars

PIA22575-16NASA’s InSight has sent signals to Earth indicating that its solar panels are open and collecting sunlight on the Martian surface. NASA’s Mars Odyssey orbiter relayed the signals, which were received on Earth at about 5:30 p.m. PST (8:30 p.m. EST). Solar array deployment ensures the spacecraft can recharge its batteries each day. Odyssey also relayed a pair of images showing InSight’s landing site.

“The InSight team can rest a little easier tonight now that we know the spacecraft solar arrays are deployed and recharging the batteries,” said Tom Hoffman, InSight’s project manager at NASA’s Jet Propulsion Laboratory in Pasadena, California, which leads the mission. “It’s been a long day for the team. But tomorrow begins an exciting new chapter for InSight: surface operations and the beginning of the instrument deployment phase.” [More at link]

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HiRISE: The changing climate of Mars

ESP_056563_0960A story of changes in the climate of Mars is told by icy deposits. Remnants of a formerly extensive deposit composed of dry ice layered together with dust and water ice form what is known as the south polar residual cap.

This deposit is shrinking over time as the frozen carbon dioxide turns to vapor. Rounded valleys that give the deposit an appearance resembling Swiss cheese are enlarging over time, exposing an older surface below that is likely made up of water ice.

In the past, the South Pole of Mars was colder than it is today, with an average temperature below the freezing point of carbon dioxide gas. Carbon dioxide from the atmosphere condensed on the polar water ice cap, forming a layered deposit of dry ice together with trace amounts of dust and water ice. More recently, the South Pole of Mars has warmed to an average temperature greater than the freezing point of carbon dioxide gas, and the dry ice deposits are retreating… [More at link]

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Task done, InSight’s MarCO says Farewell to Mars

PIA22833

[Ed. note: For more on this image and the role played by the MarCO CubeSats, see here.]

MarCO-B, one of the experimental Mars Cube One (MarCO) CubeSats, took this image of Mars from about 4,700 miles (6,000 kilometers) away during its flyby of the Red Planet on Nov. 26, 2018. MarCO-B was flying by Mars with its twin, MarCO-A, to attempt to serve as communications relays for NASA’s InSight spacecraft as it landed on Mars. This image was taken at about 12:10 p.m. PST (3:10 p.m. EST) while MarCO-B was flying away from the planet after InSight landed. [More at link]

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