NASA’s Curiosity Mars Rover Detects Clues Hinting at a Wetter Past 

During the same relative time period, other clues indicate more oxygen was present in the atmosphere than found currently

This scene shows NASA's Curiosity Mars rover at a location called "Windjana," where the rover found rocks containing manganese-oxide minerals, which require abundant water and strongly oxidizing conditions to form. In front of the rover are two holes from the rover's sample-collection drill and several dark-toned features that have been cleared of dust (see inset images). These flat features are erosion-resistant fracture fills containing manganese oxides. The discovery of these materials suggests the Martian atmosphere might once have contained higher abundances of free oxygen than it does now. Credits: NASA/JPL-Caltech/MSSS
This image shows NASA’s Curiosity Mars rover at a location called “Windjana,” where the rover found rocks containing manganese oxide minerals, which require abundant water and strongly oxidizing conditions to form. In front of the rover are two holes from the rover’s sample-collection drill and several dark-toned features that have been cleared of dust (see inset images). These flat features are erosion-resistant fracture fills containing manganese oxides. The discovery of these materials suggests the Martian atmosphere might once have contained higher abundances of free oxygen than it does now.
Credits: NASA/JPL-Caltech/MSSS

Space news (planetary science: Martian rocks containing manganese oxide minerals; indicating a wetter surface with more atmospheric oxygen than presently found on Mars) – Mars (the Red Planet), 154 million miles (249 kilometers) from Sol, or 141 million miles (228 million kilometers) from Earth, on average –

This view from the Mars Hand Lens Imager (MAHLI) on NASA's Curiosity Mars Rover shows the rock target "Windjana" and its immediate surroundings after inspection of the site by the rover. The drilling of a test hole and a sample collection hole produced the mounds of drill cuttings that are markedly less red than the other visible surfaces. This is material that the drill pulled up from the interior of the rock. This view is from the 627th Martian day, or sol, of Curiosity's work on Mars (May 12, 2014). The open hole from sample collection is 0.63 inch (1.6 centimeters) in diameter. It was drilled on Sol 621 (May 5, 2014). A preparatory "mini drill" hole, to lower right from the open hole, was drilled on Sol 615 (April 29, 2014) and subsequently filled in with cuttings from the sample collection drilling. Two small patches of less-red color to the right of the drill holes are targets "Stephen" (higher) and "Neil," where multiple laser hits by Curiosity's Chemistry and Camera (ChemCam) instrument blasted some of the reddish surface dust off the surface of the rock. The vigorous activity of penetrating the rock with the rover's hammering drill also resulted in slides of loose material near the rock. For comparison to the site before the drilling, see the Sol 609 image of Windjana at http://photojournal.jpl.nasa.gov/catalog/PIA18087. MAHLI was built by Malin Space Science Systems, San Diego. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project's Curiosity rover. Credit: NASA/JPL-Caltech/MSSS
This view from the Mars Hand Lens Imager (MAHLI) on NASA’s Curiosity Mars Rover shows the rock target “Windjana” and its immediate surroundings after inspection of the site by the rover. The drilling of a test hole and a sample collection hole produced the mounds of drill cuttings that are markedly less red than the other visible surfaces. This is material that the drill pulled up from the interior of the rock.
This view is from the 627th Martian day, or sol, of Curiosity’s work on Mars (May 12, 2014).
The open hole from sample collection is 0.63 inch (1.6 centimeters) in diameter. It was drilled on Sol 621 (May 5, 2014). A preparatory “mini drill” hole, to lower right from the open hole, was drilled on Sol 615 (April 29, 2014) and subsequently filled in with cuttings from the sample-collection drilling.
Two small patches of less red color to the right of the drill holes are targets “Stephen” (higher) and “Neil,” where multiple laser hits by Curiosity’s Chemistry and Camera (ChemCam) instrument blasted some of the reddish surface dust off the surface of the rock.
The vigorous activity of penetrating the rock with the rover’s hammering drill also resulted in slides of loose material near the rock. 
MAHLI was built by Malin Space Science Systems, San Diego. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project’s Curiosity rover.
Credit: NASA/JPL-Caltech/MSSS

NASA’s Curiosity Mars rover has found rocks at a place called Windjana containing manganese oxide minerals according to reports from planetary scientists studying samples from the region. On Earth rocks of this type formed during the distant past in the presence of abundant water and atmospheric oxygen. This news added to previous reports of ancient lakes and other groundwater sources during Mar’s past points to a wetter environment in the study region Gale Crater during this time. 

This image from the Navigation Camera (Navcam) on NASA's Curiosity Mars rover shows a sandstone slab on which the rover team has selected a target, "Windjana," for close-up examination and possible drilling. The target is on the approximately 2-foot-wide (60-centimeter-wide) rock seen in the right half of this view. The Navcam's left-eye camera took this image during the 609th Martian day, or sol, of Curiosity's work on Mars (April 23, 2014). The rover's name is written on the covering for a portion of the robotic arm, here seen stowed at the front of the vehicle. The sandstone target's informal name comes from Windjana Gorge in Western Australia. If this target meets criteria set by engineers and scientists, it could become the mission's third drilled rock and the first that is not mudstone. The rock is within a waypoint location called "the Kimberley," where sandstone outcrops with differing resistance to wind erosion result in a stair-step pattern of layers. Windjana is within what the team calls the area's "middle unit," because it is intermediate between rocks that form buttes in the area and lower-lying rocks that show a pattern of striations. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Science Laboratory Project for NASA's Science Mission Directorate, Washington. JPL designed and built the project's Curiosity rover and the rover's Navcam. > Read more: NASA's Curiosity Mars Rover Inspects Site Image Credit: NASA/JPL-Caltech
This image from the Navigation Camera (Navcam) on NASA’s Curiosity Mars rover shows a sandstone slab on which the rover team has selected a target, “Windjana,” for close-up examination and possible drilling. The target is on the approximately 2-foot-wide (60-centimeter-wide) rock seen in the right half of this view.
The Navcam’s left-eye camera took this image during the 609th Martian day, or sol, of Curiosity’s work on Mars (April 23, 2014). The rover’s name is written on the covering for a portion of the robotic arm, here seen stowed at the front of the vehicle.
The sandstone target’s informal name comes from Windjana Gorge in Western Australia. If this target meets criteria set by engineers and scientists, it could become the mission’s third drilled rock and the first that is not mudstone.
The rock is within a waypoint location called “the Kimberley,” where sandstone outcrops with differing resistance to wind erosion result in a stair-step pattern of layers. Windjana is within what the team calls the area’s “middle unit,” because it is intermediate between rocks that form buttes in the area and lower-lying rocks that show a pattern of striations.
NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Science Laboratory Project for NASA’s Science Mission Directorate, Washington. JPL designed and built the project’s Curiosity rover and the rover’s Navcam.
Image Credit: NASA/JPL-Caltech

Planetary scientists used the laser-firing instrument on the Curiosity Mars rover to detect high levels of manganese-oxide in mineral veins found at Windjana. “The only ways on Earth that we know how to make these manganese materials involve atmospheric oxygen or microbes,” said Nina Lanza, a planetary scientist at Los Alamos National Laboratory in New Mexico. “Now we’re seeing manganese oxides on Mars, and we’re wondering how the heck these could have formed?”

On this view of the Curiosity rover mission's waypoint called "the Kimberley," the red dot indicates the location of a sandstone target, "Windjana," that researchers selected for close-up inspection and possibly for drilling. The view is an excerpt from an April 11, 2014, observation by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. A larger scene from the same observation is at http://photojournal.jpl.nasa.gov/catalog/PIA18081. In the image's enhanced color, Curiosity itself appears as the bright blue object at the two-o'clock position relative to the butte in the lower center of the scene. That butte is called "Mount Remarkable" and stands about 16 feet (5 meters) high. The rover subsequently drove to within its robotic arm's reach of Windjana. For scale, the distance between the parallel wheel tracks visible in the image is about 9 feet (2.7 meters). In the area of the Kimberley waypoint, sandstone outcrops with differing resistance to wind erosion result in a stair-step pattern of layers. Windjana is within what the team calls the area's "middle unit," because it is intermediate between rocks that form buttes in the area and lower-lying rocks that show a pattern of striations. If Windjana meets criteria set by engineers and scientists, it could become the mission's third drilled rock and the first that is not mudstone. This view is an enhanced-color product from HiRISE observation ESP_036128_1755, available at the HiRISE website at http://uahirise.org/releases/msl-kimberley.php. The exaggerated color, to make differences in Mars surface materials more apparent, makes Curiosity appear bluer than the rover really looks. HiRISE is one of six instruments on NASA's Mars Reconnaissance Orbiter. The University of Arizona, Tucson, operates HiRISE, which was built by Ball Aerospace & Technologies Corp., Boulder, Colo. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter and Mars Science Laboratory projects for NASA's Science Mission Directorate, Washington. JPL designed and built the Mars Science Laboratory Project's Curiosity rover. Image Credit: NASA/JPL-Caltech/Univ. of Arizona
On this view of the Curiosity rover mission’s waypoint called “the Kimberley,” the red dot indicates the location of a sandstone target, “Windjana,” that researchers selected for close-up inspection and possibly for drilling.
The view is an excerpt from an April 11, 2014, observation by the High-Resolution Imaging Science Experiment (HiRISE) camera on NASA’s Mars Reconnaissance Orbiter. In the image’s enhanced color, Curiosity itself appears as the bright blue object at the two-o’clock position relative to the butte in the lower center of the scene. That butte is called “Mount Remarkable” and stands about 16 feet (5 meters) high. The rover subsequently drove to within its robotic arm’s reach of Windjana. For scale, the distance between the parallel wheel tracks visible in the image is about 9 feet (2.7 meters).
In the area of the Kimberley waypoint, sandstone outcrops with differing resistance to wind erosion result in a stair-step pattern of layers. Windjana is within what the team calls the area’s “middle unit,” because it is intermediate between rocks that form buttes in the area and lower-lying rocks that show a pattern of striations.
The exaggerated color, to make differences in Mars surface materials more apparent, makes Curiosity appear bluer than the rover really looks.
HiRISE is one of six instruments on NASA’s Mars Reconnaissance Orbiter. The University of Arizona, Tucson, operates HiRISE, which was built by Ball Aerospace & Technologies Corp., Boulder, Colo. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter and Mars Science Laboratory projects for NASA’s Science Mission Directorate, Washington. JPL designed and built the Mars Science Laboratory Project’s Curiosity rover.
Image Credit: NASA/JPL-Caltech/Univ. of Arizona

Planetary scientists are looking at other processes that could create the manganese-oxide they found in rocks in Mar’s Gale Crater region. Possible culprits at this point include microbes, but even optimistic planetary scientists are finding little fan fair accompanying their ideas. Lanza said, “These high manganese materials can’t form without lots of liquid water and strongly oxidizing conditions. Here on Earth, we had lots of water but no widespread deposits of manganese oxides until after the oxygen levels in our atmosphere rose.”

NASA's Curiosity Mars rover used the Mars Hand Lens Imager (MAHLI) instrument on its robotic arm to illuminate and record this nighttime view of the sandstone rock target "Windjana." The rover had previously drilled a hole to collect sample material from the interior of the rock and then zapped a series of target points inside the hole with the laser of the rover's Chemistry and Camera (ChemCam) instrument. The hole is 0.63 inch (1.6 centimeters) in diameter. The precision pointing of the laser that is mounted atop the rover's remote-sensing mast is evident in the column of scars within the hole. That instrument provides information about the target's composition by analysis of the sparks of plasma generated by the energy of the laser beam striking the target. Additional ChemCam laser scars are visible at upper right, on the surface of the rock. This view combines eight separate MAHLI exposures, taken at different focus settings to show the entire scene in focus. The exposures were taken after dark on the 628th Martian day, or sol, of Curiosity's work on Mars (May 13, 2014). The rover drilled this hole on Sol 621 (May 5, 2014). MAHLI includes light-emitting diodes as well as a color camera. Using the instrument's own lighting yields an image of the hole's interior with less shadowing than would be seen in a sunlit image. The camera's inspection of the interior of the hole provides documentation about what the drill bit passed through as it penetrated the rock -- for example, to see if it cut through any mineral veins or visible layering. MAHLI was built by Malin Space Science Systems, San Diego. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project's Curiosity rover. Credit: NASA/JPL-Caltech/MSSS
NASA’s Curiosity Mars rover used the Mars Hand Lens Imager (MAHLI) instrument on its robotic arm to illuminate and record this nighttime view of the sandstone rock target “Windjana.” The rover had previously drilled a hole to collect sample material from the interior of the rock and then zapped a series of target points inside the hole with the laser of the rover’s Chemistry and Camera (ChemCam) instrument. The hole is 0.63 inch (1.6 centimeters) in diameter.
The precision pointing of the laser that is mounted atop the rover’s remote-sensing mast is evident in the column of scars within the hole. That instrument provides information about the target’s composition by analysis of the sparks of plasma generated by the energy of the laser beam striking the target. Additional ChemCam laser scars are visible at upper right, on the surface of the rock.
This view combines eight separate MAHLI exposures, taken at different focus settings to show the entire scene in focus. The exposures were taken after dark on the 628th Martian day, or sol, of Curiosity’s work on Mars (May 13, 2014). The rover drilled this hole on Sol 621 (May 5, 2014).
MAHLI includes light-emitting diodes as well as a color camera. Using the instrument’s own lighting yields an image of the hole’s interior with less shadowing than would be seen in a sunlit image. The camera’s inspection of the interior of the hole provides documentation about what the drill bit passed through as it penetrated the rock — for example, to see if it cut through any mineral veins or visible layering.
MAHLI was built by Malin Space Science Systems, San Diego. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project’s Curiosity rover.
Credit: NASA/JPL-Caltech/MSSS

Geologists have found high concentrations of manganese oxide minerals is an important marker of a major shift in Earth’s atmospheric composition, from relatively low oxygen levels during the distant past, to the oxygen-rich environment we live in today. Planetary scientists studying the rocks they found in Gale Crater suggest the presence of these materials indicates oxygen levels on Mars rose also, before declining to the present low levels detected. The question is how was Mar’s oxygen-rich atmosphere formed?

November 3, 2015 Lanza at the summit of Hvannadalsnukur, the highest mountain in Iceland, practicing glacier travel techniques similar to those needed for Antarctic fieldwork. Lanza at the summit of Hvannadalsnukur, the highest mountain in Iceland, practicing glacier travel techniques similar to those needed for Antarctic fieldwork. Credit: Los Alamos National Laboratory
November 3, 2015
Planetary scientist Lanza at the summit of Hvannadalsnukur, the highest mountain in Iceland, practicing glacier travel techniques similar to those needed for exploring the farthest reaches of the planet and possibly the solar system.
Credit: Los Alamos National Laboratory

“One potential way that oxygen could have gotten into the Martian atmosphere is from the breakdown of water when Mars was losing its magnetic field,” said Lanza. “It’s thought that at this time in Mars’ history, water was much more abundant. Yet without a protective magnetic field to shield the surface, ionizing radiation started splitting water molecules into hydrogen and oxygen. Because of Mars’ relatively low gravity, the planet wasn’t able to hold onto the very light hydrogen atoms, but the heavier oxygen atoms remained behind. Much of this oxygen went into rocks, leading to the rusty red dust that covers the surface today. While Mars’ famous red iron oxides require only a mildly oxidizing environment to form, manganese oxides require a strongly oxidizing environment, more so than previously known for Mars.

Lanza added, “It’s hard to confirm whether this scenario for Martian atmospheric oxygen actually occurred. But it’s important to note that this idea represents a departure in our understanding for how planetary atmospheres might become oxygenated. Abundant atmospheric oxygen has been treated as a so-called biosignature or a sign of extant life, but this process does not require life.

This image from the Navigation Camera (Navcam) on NASA's Curiosity Mars rover shows two holes at top center drilled into a sandstone target called "Windjana." The farther hole, with larger pile of tailings around it, is a full-depth sampling hole. It was created by the rover's hammering drill while the drill collected rock-powder sample material from the interior of the rock. The nearer hole was created by a shallower test drilling into the rock in preparation for the sample collection. Each hole is 0.63 inch (1.6 centimeters) in diameter. The full-depth hole is about 2.6 inches (6.5 centimeters) deep, drilled during the 621st Martian day, or sol, of Curiosity's work on Mars (May 5, 2014). The test hole is about 0.8 inch (2 centimeters) deep, drilled on Sol 615 (April 29, 2014). This image was taken on Sol 621 (May 5). The sandstone target's informal name comes from Windjana Gorge in Western Australia. The rock is within a waypoint location called "The Kimberley," where sandstone outcrops with differing resistance to wind erosion result in a stair-step pattern of layers. Windjana is within what the team calls the area's "middle unit," because it is intermediate between rocks that form buttes in the area and lower-lying rocks that show a pattern of striations. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Science Laboratory Project for NASA's Science Mission Directorate, Washington. JPL designed and built the project's Curiosity rover and the rover's Navcam. Credit: NASA/JPL-Caltech
This image from the Navigation Camera (Navcam) on NASA’s Curiosity Mars rover shows two holes at top center drilled into a sandstone target called “Windjana.” The farther hole, with larger pile of tailings around it, is a full-depth sampling hole. It was created by the rover’s hammering drill while the drill collected rock-powder sample material from the interior of the rock. The nearer hole was created by a shallower test drilling into the rock in preparation for the sample collection. Each hole is 0.63 inch (1.6 centimeters) in diameter. The full-depth hole is about 2.6 inches (6.5 centimeters) deep, drilled during the 621st Martian day, or sol, of Curiosity’s work on Mars (May 5, 2014). The test hole is about 0.8 inch (2 centimeters) deep, drilled on Sol 615 (April 29, 2014). This image was taken on Sol 621 (May 5).
The sandstone target’s informal name comes from Windjana Gorge in Western Australia. The rock is within a waypoint location called “The Kimberley,” where sandstone outcrops with differing resistance to wind erosion result in a stair-step pattern of layers. Windjana is within what the team calls the area’s “middle unit,” because it is intermediate between rocks that form buttes in the area and lower-lying rocks that show a pattern of striations.
NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Science Laboratory Project for NASA’s Science Mission Directorate, Washington. JPL designed and built the project’s Curiosity rover and the rover’s Navcam.
Credit: NASA/JPL-Caltech

The Curiosity rover has been investigating Gale Crater for around four years and recent evidence supports the possibility conditions needed to form these deposits were present in other locations. The concentrations of manganese oxide discovered were found in mineral-filled cracks in sandstones in a region of the crater called “Kimberley”. NASA’s Opportunity rover has been exploring the surface of the planet since 2004 and recently reported similar high manganese deposits in a region thousands of miles away. Supporting the idea environments required to form similar deposits could be found well beyond Gale Crater.

NASA's Curiosity Mars rover used the camera at the end of its arm in April and May 2014 to take dozens of component images combined into this self-portrait where the rover drilled into a sandstone target called "Windjana." The camera is the Mars Hand Lens Imager (MAHLI), which previously recorded portraits of Curiosity at two other important sites during the mission: "Rock Nest" (http://photojournal.jpl.nasa.gov/catalog/PIA16468) and "John Klein" (http://photojournal.jpl.nasa.gov/catalog/PIA16937). Winjana is within a science waypoint site called "The Kimberley," where sandstone layers with different degrees of resistance to wind erosion are exposed close together. The view does not include the rover's arm. It does include the hole in Windjana produced by the hammering drill on Curiosity's arm collecting a sample of rock powder from the interior of the rock. The hole is surrounded by grayish cuttings on top of the rock ledge to the left of the rover. The Mast Camera (Mastcam) atop the rover's remote sensing mast is pointed at the drill hole. A Mastcam image of the drill hole from that perspective is at http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0626MR0026780000401608E01_DXXX&s=626. The hole is 0.63 inch (1.6 centimeters) in diameter. The rover's wheels are 20 inches (0.5 meter) in diameter. Most of the component frames of this mosaic view were taken during the 613th Martian day, or sol, of Curiosity's work on Mars (April 27, 2014). Frames showing Windjana after completion of the drilling were taken on Sol 627 (May 12, 2014). The hole was drilled on Sol 621 (May 5, 2014). MAHLI was built by Malin Space Science Systems, San Diego. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project's Curiosity rover. > NASA’s Mars Curiosity Rover Marks First Martian Year with Mission Successes Image Credit: NASA/JPL-Caltech/MSSS
NASA’s Curiosity Mars rover used the camera at the end of its arm in April and May 2014 to take dozens of component images combined into this self-portrait where the rover drilled into a sandstone target called “Windjana.” The camera is the Mars Hand Lens Imager (MAHLI), which previously recorded portraits of Curiosity at two other important sites during the mission: “Rock Nest” 
Winjana is within a science waypoint site called “The Kimberley,” where sandstone layers with different degrees of resistance to wind erosion are exposed close together.
The view does not include the rover’s arm. It does include the hole in Windjana produced by the hammering drill on Curiosity’s arm collecting a sample of rock powder from the interior of the rock. The hole is surrounded by grayish cuttings on top of the rock ledge to the left of the rover. The Mast Camera (Mastcam) atop the rover’s remote sensing mast is pointed at the drill hole. The hole is 0.63 inch (1.6 centimeters) in diameter. The rover’s wheels are 20 inches (0.5 meter) in diameter.
Most of the component frames of this mosaic view were taken during the 613th Martian day, or sol, of Curiosity’s work on Mars (April 27, 2014). Frames showing Windjana after completion of the drilling were taken on Sol 627 (May 12, 2014). The hole was drilled on Sol 621 (May 5, 2014).
MAHLI was built by Malin Space Science Systems, San Diego. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project’s Curiosity rover.
> NASA’s Mars Curiosity Rover Marks First Martian Year with Mission Successes
Image Credit: NASA/JPL-Caltech/MSSS

What’s next for Curiosity?

NASA’s Curiosity rover’s currently collecting drilled rock powder from the 14th drill site called the Murray formation on the lower part of Mount Sharp. Plans call for NASA’s mobile laboratory to head uphill towards new destinations as part of a two-year mission extension starting near the beginning of October. 

NASA's Curiosity Mars rover completed a shallow "mini drill" activity on April 29, 2014, as part of evaluating a rock target called "Windjana" for possible full-depth drilling to collect powdered sample material from the rock's interior. This image from Curiosity's Mars Hand Lens Imager (MAHLI) instrument shows the hole and tailings resulting from the mini drill test. The hole is 0.63 inch (1.6 centimeters) in diameter and about 0.8 inch (2 centimeters) deep. When collecting sample material, the rover's hammering drill bores as deep as 2.5 inches (6.4 centimeters). This preparatory activity enables the rover team to evaluate interaction between the drill and this particular rock and to view the potential sample-collection target's interior and tailings. Both the mini drill activity and acquisition of this image occurred during the 615th Martian day, or sol, of Curiosity's work on Mars (April 29, 2014). MAHLI was built by Malin Space Science Systems, San Diego. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project's Curiosity rover. Credit: NASA/JPL-Caltech/MSSS
NASA’s Curiosity Mars rover completed a shallow “mini drill” activity on April 29, 2014, as part of evaluating a rock target called “Windjana” for possible full-depth drilling to collect powdered sample material from the rock’s interior. This image from Curiosity’s Mars Hand Lens Imager (MAHLI) instrument shows the hole and tailings resulting from the mini drill test. The hole is 0.63 inch (1.6 centimeters) in diameter and about 0.8 inches (2 centimeters) deep.
When collecting sample material, the rover’s hammering drill bores as deep as 2.5 inches (6.4 centimeters). This preparatory activity enables the rover team to evaluate the interaction between the drill and this particular rock and to view the potential sample-collection target’s interior and tailings. Both the mini-drill activity and acquisition of this image occurred during the 615th Martian day, or sol, of Curiosity’s work on Mars (April 29, 2014).
MAHLI was built by Malin Space Science Systems, San Diego. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Science Laboratory Project for the NASA Science Mission Directorate, Washington. JPL designed and built the project’s Curiosity rover.
Credit: NASA/JPL-Caltech/MSSS

The rover will go forward about a-mile-and-a-half (two-and-a-half-kilometers) to a ridge capped with material rich in the iron-oxide mineral hematite first identified by observations made with NASA’s Mars Reconnaissance Orbiter. Just beyond this area, there’s also a region with clay-rich bedrock planetary scientists want to have a closer look.

The foreground of this scene from the Mast Camera (Mastcam) on NASA's Curiosity Mars rover shows purple-hued rocks near the rover's late-2016 location on lower Mount Sharp. The scene's middle distance includes higher layers that are future destinations for the mission. Variations in color of the rocks hint at the diversity of their composition on lower Mount Sharp. The purple tone of the foreground rocks has been seen in other rocks where Curiosity's Chemical and Mineralogy (CheMin) instrument has detected hematite. Winds and windblown sand in this part of Curiosity's traverse and in this season tend to keep rocks relatively free of dust, which otherwise can cloak rocks' color. The three frames combined into this mosaic were acquired by the Mastcam's right-eye camera on Nov. 10, 2016, during the 1,516th Martian day, or sol, of Curiosity's work on Mars. The scene is presented with a color adjustment that approximates white balancing, to resemble how the rocks and sand would appear under daytime lighting conditions on Earth. Sunlight on Mars is tinged by the dusty atmosphere and this adjustment helps geologists recognize color patterns they are familiar with on Earth. The view spans about 15 compass degrees, with the left edge toward southeast. The rover's planned direction of travel from its location when this scene was recorded is generally southeastward. The orange-looking rocks just above the purplish foreground ones are in the upper portion of the Murray formation, which is the basal section of Mount Sharp, extending up to a ridge-forming layer called the Hematite Unit. Beyond that is the Clay Unit, which is relatively flat and hard to see from this viewpoint. The next rounded hills are the Sulfate Unit, Curiosity's highest planned destination. The most distant slopes in the scene are higher levels of Mount Sharp, beyond where Curiosity will drive. Figure 1 is a version of the same scene with annotations added as reference points for distance, size and relative elevation. The annotations are triangles with text telling the distance (in kilometers) to the point in the image marked by the triangle, the point's elevation (in meters) relative to the rover's location, and the size (in meters) of an object as big as the triangle at that distance. Malin Space Science Systems, San Diego, built and operates Mastcam. NASA's Jet Propulsion Laboratory, a division of Caltech in Pasadena, manages the Mars Science Laboratory Project for NASA's Science Mission Directorate, Washington, and built the project's Curiosity rover. Image Credit: NASA/JPL-Caltech/MSSS
The foreground of this scene from the Mast Camera (Mastcam) on NASA’s Curiosity Mars rover shows purple-hued rocks near the rover’s late-2016 location on lower Mount Sharp. The scene’s middle distance includes higher layers that are future destinations for the mission.
Variations in color of the rocks hint at the diversity of their composition on lower Mount Sharp. The purple tone of the foreground rocks has been seen in other rocks where Curiosity’s Chemical and Mineralogy (CheMin) instrument has detected hematite. Winds and windblown sand in this part of Curiosity’s traverse and in this season tend to keep rocks relatively free of dust, which otherwise can cloak rocks’ color.
The three frames combined into this mosaic were acquired by the Mastcam’s right-eye camera on Nov. 10, 2016, during the 1,516th Martian day, or sol, of Curiosity’s work on Mars. The scene is presented with a color adjustment that approximates white balancing, to resemble how the rocks and sand would appear under daytime lighting conditions on Earth. Sunlight on Mars is tinged by the dusty atmosphere and this adjustment helps geologists recognize color patterns they are familiar with on Earth.
The view spans about 15 compass degrees, with the left edge toward the southeast. The rover’s planned direction of travel from its location when this scene was recorded is generally southeastward.
The orange-looking rocks just above the purplish foreground ones are in the upper portion of the Murray formation, which is the basal section of Mount Sharp, extending up to a ridge-forming layer called the Hematite Unit. Beyond that is the Clay Unit, which is relatively flat and hard to see from this viewpoint. The next rounded hills are the Sulfate Unit, Curiosity’s highest planned destination. The most distant slopes in the scene are higher levels of Mount Sharp, beyond where Curiosity will drive.
Figure 1 is a version of the same scene with annotations added as reference points for distance, size and relative elevation. The annotations are triangles with text telling the distance (in kilometers) to the point in the image marked by the triangle, the point’s elevation (in meters) relative to the rover’s location, and the size (in meters) of an object as big as the triangle at that distance.
Malin Space Science Systems, San Diego, built and operates Mastcam. NASA’s Jet Propulsion Laboratory, a division of Caltech in Pasadena, manages the Mars Science Laboratory Project for NASA’s Science Mission Directorate, Washington, and built the project’s Curiosity rover.
Image Credit: NASA/JPL-Caltech/MSSS

NASA has been exploring these key exploration sites on lower Mount Sharp as part of an effort to investigate evidence the Red planet was once a much wetter environment, which contrasts with the pictures of Mars we have received from our orbiters and rovers. A wetter environment where life could have taken root and grown.

“We continue to reach higher and younger layers on Mount Sharp,” said Curiosity Project Scientist Ashwin Vasavada, of NASA’s Jet Propulsion Laboratory, Pasadena, California. “Even after four years of exploring near and on the mountain, it still has the potential to completely surprise us.”

Planetary scientists found the Murray formation consists primarily of mudstone, which on Earth would form from mud accumulated on the bottom on an ancient lake. This seems to indicate any lake environment that existed on the Red Planet lasted awhile, but we’ll need to investigate this possibility more. Plans are for Curiosity to investigate the upper regions of the Murray formation, ahead, for at least one year of the mission. 

“We will see whether that record of lakes continues further,” Vasavada said. “The more vertical thickness we see, the longer the lakes were present, and the longer habitable conditions existed here. Did the ancient environment change over time? Will the type of evidence we’ve found so far transition to something else?”

Vasavada said, “The Hematite and the Clay units likely indicate different environments from the conditions recorded in the older rock beneath them and different from each other. It will be interesting to see whether either or both were habitable environments.”

Read about the ferocious wind nebula astronomers have observed for the first time.

Learn how astronomers determine distances to objects on the other side of the Milky Way.

Help NASA find and classify young planetary systems to study by becoming a Disk Detective.

Find out more about NASA’s contributions to the human journey to the beginning of space and time.

Learn more about NASA Jet Propulsion Laboratory and its mission here.

Discover more about the Red Planet.

Read more about NASA’s Curiosity rover.

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The Death of the Sun 

Will leave behind a hot, shining corpse called a white dwarf

This image of NGC 2440 shows the colourful
This image of NGC 2440 shows the colourful “last hurrah” of a star like our Sun. The star is ending its life by casting off its outer layers of gas, which formed a cocoon around the star’s remaining core. Ultraviolet light from the dying star makes the material glow. The burned-out star, called a white dwarf, is the white dot in the centre. Credits: NASA/Hubble

Space news (astrophysics: the death of a Sun-like star; planetary nebula NGC 2440) – 4,000 light-years from Earth toward the constellation Puppis, watching the stunning, colorful last moments of a star like our own Sun –

Death is not extinguishing the light: it is only putting out the lamp because the dawn has come (quote by Rabindranath Tagore)

NGC 2440 is another planetary nebula ejected by a dying star, but it has a much more chaotic structure than NGC 2346. The central star of NGC 2440 is one of the hottest known, with a surface temperature near 200,000 degrees Celsius. The complex structure of the surrounding nebula suggests to some astronomers that there have been periodic oppositely directed outflows from the central star, somewhat similar to that in NGC2346, but in the case of NGC 2440 these outflows have been episodic, and in different directions during each episode. The nebula is also rich in clouds of dust, some of which form long, dark streaks pointing away fromthe central star. In addition to the bright nebula, which glows becauseof fluorescence due to ultraviolet radiation from the hot star, NGC 2440 is surrounded by a much larger cloud of cooler gas which is invisible in ordinary light but can be detected with infrared telescopes. NGC 2440 lies about 4,000 light-years from Earth in thedirection of the constellation Puppis. The Hubble Heritage team made this image from observations of NGC 2440acquired by Howard Bond (STScI) and Robin Ciardullo (Penn State). Credit: NASA/ESA and The Hubble Heritage Team (AURA/STScI).
NGC 2440 is a planetary nebula ejected by a dying star, with a little bit of extra character thrown in for visual entertainment. The central star of NGC 2440 has a surface temperature of around 200,000 degrees Celsius and chaotic nature suggesting periodic oppositely flowing outbursts, similar to the process seen in NGC 2346. In the case of this planetary nebula, however,  the outflows were periodic, and in different directions during each period. The Hubble Heritage team made this image from observations of NGC 2440 acquired by Howard Bond (STScI) and Robin Ciardullo (Penn State).
Credit: NASA/ESA and The Hubble Heritage Team (AURA/STScI).

Around 5 billion years in the future, give or take a hundred million, our Sun’s expected to send last hurrahs to the cosmos as seen here in this Hubble Telescope image of planetary nebula NGC 2440. Casting off its outer layers of gas forming a cocoon around the burned-out remains called a white dwarf, it will glow as ultraviolet light it emits strikes the material surrounding it. The Milky Way galaxy’s sprinkled with similar stellar objects astronomers in the 18th and 19th centuries named planetary nebula due to their resemblance when viewed through small telescopes of the time to the disks of distant Uranus and Neptune. Shining at a surface temperature of more than 360,000 degrees Fahrenheit (200,000 degrees Celsius), NGC 2440’s one of the hottest planetary nebula discovered during the human journey to the beginning of space and time. 

It may look like a butterfly, but it's bigger than our Solar System. NGC 2346 is a planetary nebula made of gas and dust that has evolved into a familiar shape. At the heart of the bipolar planetary nebula is a pair of close stars orbiting each other once every sixteen days. The tale of how the butterfly blossomed probably began millions of years ago, when the stars were farther apart. The more massive star expanded to encompass its binary companion, causing the two to spiral closer and expel rings of gas. Later, bubbles of hot gas emerged as the core of the massive red giant star became uncovered. In billions of years, our Sun will become a red giant and emit a planetary nebula - but probably not in the shape of a butterfly, because the Sun has no binary star companion.
Planetary nebula NGC 2346 looks like a butterfly to many viewers, but you could comfortably fit our solar system within its boundaries. Two stars orbit closely together within every sixteen days. In a few billion years, our Sun will expand to become a red giant star and eject material to create a similar looking planetary nebula. Scientists think it will look different, however, because our Sun has no companion star. Credit: Massimo Stiavelli (STScI), Inge Heyer (STScI) et al., & the Hubble Heritage Team (AURA/ STScI/ NASA)

Study of this planetary nebula’s chaotic structure suggests it shed its outer layers of mass in episodic outbursts heading in different directions as seen in the two bowtie-shaped lobes observed in the image at the top. Long, dark clouds of dust forming dark streaks traveling away from NGC 2440 can also be seen, along with expelled helium indicated by blue, oxygen highlighted in blue-green, and nitrogen and hydrogen in red. Matter expelled by the white dwarf glows in different colors, depending on its composition, density, and distance from the hot star.

A full-disk multiwavelength extreme ultraviolet image of the sun taken by SDO on March 30, 2010. False colors trace different gas temperatures. Reds are relatively cool (about 60,000 Kelvin, or 107,540 F); blues and greens are hotter (greater than 1 million Kelvin, or 1,799,540 F). Credits: NASA/Goddard/SDO AIA Team
This is a full-disk multiwavelength extreme ultraviolet image of the sun taken by SDO on March 30, 2010. False colors trace different gas temperatures. Reds are relatively cool (about 60,000 Kelvin, or 107,540 F); blues and greens are hotter (greater than 1 million Kelvin, or 1,799,540 F). In a few billion years it will expand into a red giant star and eject material that will become a similar, but different, looking planetary nebula than NGC 2440. Credits: NASA/Goddard/SDO AIA Team

The final days of stars like the Sun

The present theory concerning the final days of a white dwarf star says it will end its days as a black dwarf star. Unknown billions of years in the future, astronomers believe white dwarf stars could stop emitting light and heat and become cold, stellar bodies. Cold, dark stars our telescopes and present technology would have extreme difficulty detecting accept for the effects of their gravity wells on objects traveling nearby. Unfortunately, our universe is only about 14 billions years old, which is too young for black dwarf stars to exist, if the theory is correct. 

Read about NASA’s recently issued challenge to young innovators to “Think Outside the Box”.

Learn more about NASA’s Next Generation Wide-field Infrared Survey Telescope.

Discover how astronomers measure distances to objects on the other side of the Milky Way.

Learn more about NASA’s contributions to the human journey to the beginning of space and time here.

Learn more about the Sun.

Discover more about planetary nebula here.

Learn more about white dwarf stars.

Learn more about black dwarf stars.

NASA’s Looking to Form Space Technology Partnerships with American Firms 

Aimed at space technologies advancing the commercial space industry and enabling future NASA missions

NASA’s Marshall Space Flight Center (MSFC) additive manufactured injector by was successfully hot fire tested by Vector Space System on Dec. 8, 2016 using Liquid Oxygen/Propylene propellant (LOX/LC3H6). This work was performed under a 2015 STMD ACO Space Act Agreement. Credits: Vector Space System
NASA’s Marshall Space Flight Center (MSFC) additive manufactured injector by was successfully hot fire tested by Vector Space System on Dec. 8, 2016 using Liquid Oxygen/Propylene propellant (LOX/LC3H6). This work was performed under a 2015 STMD ACO Space Act Agreement.
Credits: Vector Space System

Space news (developing new space technology: the commercial space sector; the “Announcement of Collaborative Opportunity (ACO)” solicitation) – NASA headquarters in Washington, D.C., the Office of Space Technology Mission Directorate (STMD) –

Air-bearing test of Affordable Vehicle Avionics (AVA), developed by ARC, tested at MSFC to support the UP Aerospace Spyder Launch Vehicle development. This work is performed under the STMD ACO Space Act Agreement. Credits: NASA/Marshall
Air-bearing test of Affordable Vehicle Avionics (AVA), developed by ARC, tested at MSFC to support the UP Aerospace Spyder Launch Vehicle development. This work is performed under the STMD ACO Space Act Agreement.
Credits: NASA/Marshall

NASA put out a call today for American businesses looking to form long-term partnerships aimed at designing and developing new space technologies to enable the human journey to the beginning of space and time. The Space Technology Mission Directorate (STMD) released an “Announcement of Collaborative Opportunity (ACO)” solicitation you can read that explains the opportunity better.

Dynetics regeneratively cooled engine ready for test at MSFC using Peroxide/ Kerosene (H2O2/ RP) propellant. (January, 2016). This work is performed under the STMD ACO Space Act Agreement. Credits: NASA/Marshall
Dynetics regeneratively cooled engine ready for test at MSFC using Peroxide/ Kerosene (H2O2/ RP) propellant. (January, 2016). This work is performed under the STMD ACO Space Act Agreement.
Credits: NASA/Marshall

NASA’s looking to enable the development of new space technology by forming partnerships with commercial firms in the space industry and providing resources where available and appropriate. Business partners benefit from NASA technical expertise and test facilities, along with hardware and computer software designed and engineered to enable the development of current and new space technologies. Space sector partnerships between NASA and private firms can also reduce the cost of design and development of new space technologies and accelerate the inclusion of emerging commercial space technologies into future space missions. 

Stephen Jurczyk, Associate Administrator NASA Credits: Linked
Stephen Jurczyk, Associate Administrator NASA Credits: Linked

“This ACO continues to build on STMD’s strategy to advance commercial space capabilities aligned with NASA’s long-term strategic goals,” said Steve Jurczyk, associate administrator for STMD at NASA Headquarters in Washington. “These partnerships will leverage NASA’s unique engineering expertise and test facilities to increase U.S. industry competitiveness in the space sector.”

Areas of space technology

This opportunity’s a limited one. NASA’s only seeking partnerships in four areas of space technology through this ACO:

  • The design and development of space spacecraft launch systems.
  • New commercial capabilities to produce low-cost yet reliable electronic systems for space.
  • Advanced commercial space telecommunications technologies that can be used during future NASA space missions or infused into their infrastructure.
  • Advanced small spacecraft chemical propulsion systems, sub-kW power level electric propulsion systems, and large-scale chemical cryogenic propulsion systems. 

All partnerships must work on the advancement of commercially-developed space technologies that can benefit both private and government use and the human journey to the beginning of space and time in general. 

Better hurry! All preliminary proposals have to be submitted by March 15, 2017. They’ll provide feedback on your ideas. After that, your final proposal’s due by May 31. 

All awarded funds are in the form of non-reimbursable Space Act Agreements (no funds exchanged). You also need to be a profit-driven US firm looking to make some money and enable the human journey to the beginning of space and time. 

Read about NASA’s Mars 2020 rover and its plans to take over the work being done by the Curiosity rover.

Learn about the new method astronomers are developing to help determine distances to stellar objects on the other side of the Milky Way.

Learn how astronomers study the formation of new stars in the cosmos.

Read more about NASA’s contributions to the human journey to the beginning of space and time here.

Learn more about the work of the genius at the Jet Propulsion Laboratory.

Learn more about the work being done by NASA’s Space Technology Mission Directorate here.

X-ray Light Source CX330 Detected in Bulge of Milky Way

Most isolated young star discovered launching jets of material into surrounding gas and dust

An unusual celestial object called CX330 was first detected as a source of X-ray light in 2009. It has been launching “jets” of material into the gas and dust around it. Credits: NASA/JPL-Caltech
An unusual celestial object called CX330 was first detected as a source of X-ray light in 2009. It has been launching “jets” of material into the gas and dust around it.
Credits: NASA/JPL-Caltech

Space news (astrophysics: massive, young stars in star-forming regions; unusual, isolated young star baffles astronomers) – approximately 27,000 light-years from Earth in an isolated region of the bulge of the Milky Way – 

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NASA’s Chandra X-ray Observatory first detected unusual stellar object CX330. Credits: NASA/Chandra

Astronomers surveying the universe looking for unusual celestial objects to study to add to human knowledge and understanding have found something they haven’t seen before. Unusual celestial object CX 330 was first noticed in data obtained during a survey of the bulge of the Milky Way in 2009 by NASA’s Chandra X-ray Observatory as a source of X-ray light. Additional observations of the source showed it also emitted light in optical wavelengths, but with so few clues to go on, astronomers had no idea what they were looking at. 

During more recent observations of CX 330 during August of 2015, astronomers discovered it had recently been active, launching jets of material into gas and dust surrounding it. During a period from 2007 to 2010, it had increased in brightness by hundreds of times, which made scientists curious to examine previous data obtained from the same region of the bulge. 

Using the unique orbit of NASA's Spitzer Space Telescope and a depth-perceiving trick called parallax, astronomers have determined the distance to an invisible Milky Way object called OGLE-2005-SMC-001. This artist's concept illustrates how this trick works: different views from both Spitzer and telescopes on Earth are combined to give depth perception. Credits: NASA/Spitzer
Using the unique orbit of NASA’s Spitzer Space Telescope and a depth-perceiving trick called parallax, astronomers have determined the distance to an invisible Milky Way object called OGLE-2005-SMC-001. This artist’s concept illustrates how this trick works: different views from both Spitzer and telescopes on Earth are combined to give depth perception. Credits: NASA/Spitzer

Looking at data obtained by NASA’s Wide-field Infrared Survey Explorer (WISE) in 2010, they realized the surrounding gas and dust was heated to the point of ionization.  Comparing this data to observations taken with NASA’s Spitzer Space Telescope in 2007, astronomers determined they were looking at a young star in an outburst phase, forming in an isolated region of the cosmos.

cbritt
Chris Britta Credits: Texas Tech University

“We tried various interpretations for it, and the only one that makes sense is that this rapidly growing young star is forming in the middle of nowhere,” said Chris Britta postdoctoral researcher at Texas Tech University in Lubbock, and lead author of a study on CX330 recently published in the Monthly Notices of the Royal Astronomical Society.

By combining this data with observations taken by a variety of both ground and space-based telescopes they were able to get an even clearer picture of CX330. An object very similar to FU Orionis, but likely more massive, compact, and hotter, and lying in a less populated region of space. Launched faster jets of outflow that heated a surrounding disk of gas and dust to the point of ionization, and increased the flow of material falling onto the star.

tom_maccarone
Tom Maccarone Credits: Texas Tech University

“The disk has probably heated to the point where the gas in the disk has become ionized, leading to a rapid increase in how fast the material falls onto the star,” said Thomas Maccarone, study co-author and associate professor at Texas Tech.

The fact CX 330 lies in an isolated region of space, unlike the previous nine examples of this type of star observed during the human journey to the beginning of space and time, tweaks the interest of astronomers. The other nine examples all lie in star-forming regions of the Milky Way galaxy with ample material for new stars to form from, but the closest star-forming region to this young star is over 1,000 light-years away.

Joel Green Credits: NASA/Space Telescope Science Institute
Joel Green Credits: NASA/Space Telescope Science Institute

“CX330 is both more intense and more isolated than any of these young outbursting objects that we’ve ever seen,” said Joel Green, study co-author and researcher at the Space Telescope Science Institute in Baltimore. “This could be the tip of the iceberg — these objects may be everywhere.”

We really know nothing about CX 330. More observations are required to determine more. It’s possible all young stars go through a similar outburst period as observed in the case of CX 330. The periods are just too brief in cosmological time for astronomers to observe with current technology. The real clue’s the isolation of this example as compared to previous models. 

How did CX 330 become so isolated? One idea often floated is the possibility it formed in a star-forming region, before being ejected to a more isolated region of space. This seems unlikely considering astronomers believe this young star’s only about a million years old. Even if this age’s wrong, this star’s still consuming its surrounding disk of dust and gas and must have formed near its current location. It just couldn’t have traveled the required distance from a star-forming region to its current location, without completely stripping away its surrounding disk of gas and dust. 

Astronomers are learning more about the formation of stars studying CX 330, that’s for sure. Using two competing ideas, called “hierarchical” and “competitive” models, scientists search for answers to unanswered questions concerning CX 330. At this point, they favor the chaotic and turbulent environment of the “hierarchical” model, as a better fit for the theoretical formation of a lone star.

What’s next?

It’s still possible material exists nearby CX 330, such as intermediate to low-mass stars, that astronomers haven’t observed, yet.  When last viewed in August 2015, this young star was still in an outburst phase. During future observations planned with new telescopes in different wavelengths, we could get a better picture of events surrounding this unusual celestial object. Stay tuned to this channel for more information.

For people wondering if planets could form around this young star? Some astronomers are hoping planets will form from the disk of CX 330, they’ll be able to examine closer for the chemical signature of the scars left by the outbursts observed. Unfortunately, at the rate this star’s consuming its surrounding disk of gas and dust, having enough left over for the formation of planets seems unlikely. 

“You said you like it hot, right!” If CX 330’s a really massive star, which seems likely. It’s short, violent lifespan would be a truly hot time for any planet and inhabitants. 

Help NASA discover and classify young planetary systems by becoming a Disk Detective.

Read about China’s recent rejoining of the human journey to the beginning of space and time.

Read about Japan’s new X-ray satellite Hitomi.

For more information on the travel plans to CX 330, contact NASA.

Learn more about NASA’s Wide-field Infrared Survey Explorer (WISE) here.

Discover NASA’s Chandra X-ray Observatory.

For more information of NASA’s Spitzer Space Telescope visit.

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Ferocious Wind Nebula Around Magnetar Observed for First Time

Giving us a rare, unique window into the environment and emission history of the strongest magnets in the cosmos

This X-ray image shows extended emission around a source known as Swift J1834.9-0846, a rare ultra-magnetic neutron star called a magnetar. The glow arises from a cloud of fast-moving particles produced by the neutron star and corralled around it. Color indicates X-ray energies, with 2,000-3,000 electron volts (eV) in red, 3,000-4,500 eV in green, and 5,000 to 10,000 eV in blue. The image combines observations by the European Space Agency's XMM-Newton spacecraft taken on March 16 and Oct. 16, 2014. Credits: ESA/XMM-Newton/Younes et al. 2016
This X-ray image shows extended emission around a source known as Swift J1834.9-0846, a rare ultra-magnetic neutron star called a magnetar. The glow arises from a cloud of fast-moving particles produced by the neutron star and corralled around it. Color indicates X-ray energies, with 2,000-3,000 electron volts (eV) in red, 3,000-4,500 eV in green, and 5,000 to 10,000 eV in blue. The image combines observations by the European Space Agency’s XMM-Newton spacecraft taken on March 16 and Oct. 16, 2014.
Credits: ESA/XMM-Newton/Younes et al. 2016

Space news (astrophysics: wind nebulas; Swift J1834.9-0846) – 13,000 light-years toward the constellation Scutum in the midst of a vast cloud of high-energy, particles surrounding supernova remnant W41 –

Astronomers studying the strongest magnets discovered during the human journey to the beginning of space and time, magnetars, have detected one they haven’t seen before. A magnetar, a rare highly magnetic neutron star with a vast cloud of high-energy, recently-emitted particles called a wind nebula streaming from it. Offering a unique window into the characteristics, environment and emission history of one of the most enigmatic and eye-opening objects ever detected.

“Right now, we don’t know how J1834.9 developed and continues to maintain a wind nebula, which until now was a structure only seen around young pulsars,” said lead researcher George Younes, a postdoctoral researcher at George Washington University in Washington. “If the process here is similar, then about 10 percent of the magnetar’s rotational energy loss is powering the nebula’s glow, which would be the highest efficiency ever measured in such a system.”

This illustration compares the size of a neutron star to Manhattan Island in New York, which is about 13 miles long. A neutron star is the crushed core left behind when a massive star explodes as a supernova and is the densest object astronomers can directly observe. Credits: NASA's Goddard Space Flight Center
This illustration compares the size of a neutron star to Manhattan Island in New York, which is about 13 miles long. A neutron star is the crushed core left behind when a massive star explodes as a supernova and is the densest object astronomers can directly observe.
Credits: NASA’s Goddard Space Flight Center

An object around 13 miles (20 kilometers) in diameter, or about the length of Manhattan Island, only 29 magnetars have been detected, so far. In this particular case, the source of detected emissions is called Swift J1834.9-0846, a rare type of ultra-magnetic neutron star detected by the Swift Gamma-ray Burst Satellite on August 7, 2011. It was subsequently looked at closer a month later by a team led by Younes using the European Space Agency’s (ESA) XMM-Newton X-ray Observatory. It was at this time astronomers realized and confirmed the first wind nebula ever detected around a magnetar.

“For me, the most interesting question is, why is this the only magnetar with a nebula? Once we know the answer, we might be able to understand what makes a magnetar and what makes an ordinary pulsar,” said co-author Chryssa Kouveliotou, a professor in the Department of Physics at George Washington University’s Columbian College of Arts and Sciences.

Neutron stars are the crushed cores of massive stars left over after they have gone supernova and the densest objects astrophysicists have been able to directly observe during the human journey to the beginning of space and time. All neutron star magnetic fields detected, so far, are 100 to 10 trillion times stronger than Earth’s, and magnetar fields reach levels thousands of times stronger. Astrophysicists have no ideas on how magnetic fields of such immense strength are formed. 

 co-author Alice Harding, an astrophysicist at NASA's Goddard Space Flight Center in Greenbelt, Maryland. Credits: NASA
Co-author Alice Harding, an astrophysicist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.
Credits: NASA

“Making a wind nebula requires large particle fluxes, as well as some way to bottle up the outflow so it doesn’t just stream into space,” said co-author Alice Harding, an astrophysicist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. “We think the expanding shell of the supernova remnant serves as the bottle, confining the outflow for a few thousand years. When the shell has expanded enough, it becomes too weak to hold back the particles, which then leak out and the nebula fades away. This naturally explains why wind nebulae are not found among older pulsars, even those driving strong outflows.

“The nebula around J1834.9 stores the magnetar’s energetic outflows over its whole active history, starting many thousands of years ago,” said team member Jonathan Granot, an associate professor in the Department of Natural Sciences at the Open University in Ra’anana, Israel. “It represents a unique opportunity to study the magnetar’s historical activity, opening a whole new playground for theorists like me.”

What’s next?

Astrophysicists think a magnetar outburst’s powered by energy stored in its super-strong magnetic field produced gamma rays and x-rays, along with the gales of accelerated particles making up the nebula wind detected in the case of Swift J1834.9-0846. Now, they have a mystery to figure out, and new theories to deduce to explain the way a magnetar produces a nebula wind. 

Learn about the plasma jets of active supermassive black holes.

Learn what astronomers have discovered about the distribution of common chemicals during the early moments of the cosmos.

Read about NASA’s Juno spacecraft’s five year journey to Jupiter.

Join NASA’s journey to the beginning of space and time here.

Learn more about neutron stars.

Read more about magnetars here.

Discover NASA’s Goddard Space Flight Center.

Learn more about the discoveries of NASA’s Swift Gamma-ray Burst Satellite here.

Read more about Swift J1834.9-0846.

Read about the work of the European Space Agency here.

Discover the ESA’s XMM-Newton X-ray Observatory.

NASA’s Successor to Curiosity Rover Working Toward Summer Launch in 2020

To investigate Martian rocks for evidence of past life in advance of sending humans to work and live on the Red Planet

An artist concept image of where seven carefully-selected instruments will be located on NASA’s Mars 2020 rover. The instruments will conduct unprecedented science and exploration technology investigations on the Red Planet as never before. IMAGE CREDIT: NASA
An artist concept image of where seven carefully-selected instruments will be located on NASA’s Mars 2020 rover. The instruments will conduct unprecedented science and exploration technology investigations on the Red Planet as never before.
IMAGE CREDIT: NASA

Space news (missions to Mars: successor to Curiosity rover; Mars 2020 rover) – NASA’s Jet Propulsion Laboratory in Pasadena, California –

Planning for NASA's 2020 Mars rover envisions a basic structure that capitalizes on the design and engineering work done for the NASA rover Curiosity, which landed on Mars in 2012, but with new science instruments selected through competition for accomplishing different science objectives. Mars 2020 is a mission concept that NASA announced in late 2012 to re-use the basic engineering of Mars Science Laboratory to send a different rover to Mars, with new objectives and instruments, launching in 2020. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages NASA's Mars Exploration Program for the NASA Science Mission Directorate, Washington. Credits: NASA/JPL-Caltech
Planning for NASA’s 2020 Mars rover envisions a basic structure that capitalizes on the design and engineering work done for the NASA rover Curiosity, which landed on Mars in 2012, but with new science instruments selected through competition for accomplishing different science objectives. Mars 2020 is a mission concept that NASA announced in late 2012 to re-use the basic engineering of Mars Science Laboratory to send a different rover to Mars, with new objectives and instruments, launching in 2020. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages NASA’s Mars Exploration Program for the NASA Science Mission Directorate, Washington.
Credits: NASA/JPL-Caltech

NASA managers are looking forward to shifting gears on the Mars rover program in the 2020s. NASA’s Mars 2020 rover’s expected to arrive at the Red Planet around February 2021, carrying a science instrument package designed to build upon the success of NASA’s Mars Curiosity rover. It will investigate regions of the planet astrobiologists think were once favorable to microbial life, by collecting soil and rock samples, and then leaving them on the surface for a future Mars mission to collect for the possible return to Earth.

Terrain-Relative Navigation helps us land safely on Mars - especially when the land below is full of hazards like steep slopes and large rocks!
Terrain-Relative Navigation helps us land safely on Mars – especially when the land below is full of hazards like steep slopes and large rocks! The Mars 2020 spacecraft follows an entry, descent, landing process similar to that used in landing the Mars rover, Curiosity. It also has major new technologies that improve entry, descent, and landing: Range Trigger, Terrain-Relative Navigation, MEDLI and its EDL caneras and microphone. Credits: NASA/JPL

“The Mars 2020 rover is the first step in a potential multi-mission campaign to return carefully selected and sealed samples of Martian rocks and soil to Earth,” said Geoffrey Yoder, acting associate administrator of NASA’s Science Mission Directorate in Washington. “This mission marks a significant milestone in NASA’s Journey to Mars, to determine whether life has ever existed on Mars, and to advance our goal of sending humans to the Red Planet.”

The surface operations phase is the time when the rover conducts its scientific studies on Mars. After landing safely, Mars 2020 has a primary mission span of at least one Martian year (687 Earth days). The Mars 2020 rover uses a depot caching strategy for its exploration of Mars.
The surface operations phase is the time when the rover conducts its scientific studies on Mars. After landing safely, Mars 2020 has a primary mission span of at least one Martian year (687 Earth days).
The Mars 2020 rover uses a depot caching strategy for its exploration of Mars. Credits: NASA/JPL

NASA engineers, scientists and mission planners are ready to begin final design and construction of the next Mars rover. In the end, Mars 2020 will look like its six-wheeled, one-ton predecessor, Curiosity, but with a science instrument package designed to begin a new phase of exploration of the surface of Mars. It will begin exploring specifically selected regions of the planet for signs of life and the resources needed for future colonists to survive. Using two science instruments mounted on the rover’s robotic arm and two instruments on the mast, NASA’s Mars 2020 rover’s expected to show us new things about the Red Planet.

Current plans call for the Mars 2020 rover to use an upgraded version of the same sky crane landing system used by Curiosity. Engineers and designers have added a few improvements to the system opening up more potential landing sites on Mars with this edition. Giving mission planners more options to explore the Red Planet to a greater degree and hopefully provide a few more answers to the questions we have all been asking ourselves about Mars. 

Mars Science Laboratory (MSL) Entry Descent & Landing (EDL) activities in SFOF MSA Fishbowl. Pre-Landing. Date: 05 August/2012 Photographer: T. Wynne
Allen Chen, Mars 2020 entry, descent, and landing lead at NASA’s Jet Propulsion Laboratory conducting Mars Science Laboratory (MSL) Entry Descent & Landing (EDL) activities in SFOF MSA Fishbowl. Pre-Landing. 
Date: 05 August/2012
Photographer: T. Wynne

“By adding what’s known as range trigger, we can specify where we want the parachute to open, not just at what velocity we want it to open,” said Allen Chen, Mars 2020 entry, descent and landing lead at NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, California. “That shrinks our landing area by nearly half.”

NASA is developing the capabilities needed to send humans to an asteroid by 2025 and Mars in the 2030s – goals outlined in the bipartisan NASA Authorization Act of 2010 and in the U.S. National Space Policy, also issued in 2010.
NASA is developing the capabilities needed to send humans to an asteroid by 2025 and Mars in the 2030s – goals outlined in the bipartisan NASA Authorization Act of 2010 and in the U.S. National Space Policy, also issued in 2010. Credits: NASA/JPL

Engineers and designers have also added a suite of cameras and a microphone providing data onboard computers will analysis during descent and landing of the rover. This will help the spacecraft land in a safe zone and capture the sounds and imagery of the entry, descent, and landing as never before. We expect this data to eventually make for a thrilling video and improve the chances of future Mars missions. 

“As it is descending, the spacecraft can tell whether it is headed for one of the unsafe zones and divert to safe ground nearby,” said Chen. “With this capability, we can now consider landing areas with unsafe zones that previously would have disqualified the whole area. Also, we can land closer to a specific science destination, for less driving after landing.”

“Nobody has ever seen what a parachute looks like as it is opening in the Martian atmosphere,” said JPL’s David Gruel, assistant flight system manager for the Mars 2020 mission. “So this will provide valuable engineering information.”

“This will be a great opportunity for the public to hear the sounds of Mars for the first time, and it could also provide useful engineering information,” said Mars 2020 Deputy Project Manager Matt Wallace of JPL.

Mars 2020 rover goes forward

As the optimist said, “So far, so good.” NASA has completed stage three of a four-stage approval process needed for the Mars 2020 rover to go for launch. Now engineers and designers get to work assembling the final systems of NASA’s next Mars rover. Fortunately, they have already done a lot of the work during the building of Curiosity, and even have some spare parts and hardware that should work just fine laying around somewhere in the Jet Propulsion Laboratory. 

“Since Mars 2020 is leveraging the design and some spare hardware from Curiosity, a significant amount of the mission’s heritage components have already been built during Phases A and B,” said George Tahu, Mars 2020 program executive at NASA Headquarters in Washington. “With the KDP to enter Phase C completed, the project is proceeding with final design and construction of the new systems, as well as the rest of the heritage elements for the mission.”

Read and learn about the latest method astrophysicists have developed to help determine distances to objects on the other side of the Milky Way.

Learn more about the titanic, massive plasma jets astronomers have detected emanating from near some supermassive black holes.

Read about some of China’s contributions to the human journey to the beginning of space and time.

Read more about NASA’s Mars 2020 rover.

Join NASA’s journey to the beginning of space and time here.

Follow NASA’s Curiosity rover as it explores the surface of Mars.

Learn what NASA’s Spirit and Opportunity rovers have told us about the Red Planet here.

Learn more about NASA’s Jet Propulsion Laboratory.

 

3D Printing in Space Challenges Young Innovators to “Think Outside the Box”

In the design of an item or tool astronauts living and working on the International Space Station could use to complete a number of different tasks 

First 3D printer, Portal, to be tested onboard the International Space Station. Credits: Made In Space
First 3D printer, Portal, to be tested onboard the International Space Station.
Credits: Made In Space

Space news (Space Education Programs: Future Engineers; 3D Printing in Space Challenges, “Think Outside the Box” challenge) – design an item that assembles, telescopes, hinges, accordions, grows, or expands to become larger than the printing bounds of the AMF 3D printer on the International Space Station – 

Made in Space CTO Jason Dunn (left) and P.I. of the 3DP Experiment Mike Snyder look to optimize the first 3D printer for space.
Made in Space CTO Jason Dunn (left) and P.I. of the 3DP Experiment Mike Snyder look to optimize the first 3D printer for space.

Junior and teen aspiring engineers recently put their thinking hats on and came up with a few tools and items star voyagers on the International Space Station will find useful. Founding member of innovative education platform Future Engineers and partner NASA issued a challenge to young innovators to “think outside the box” in solving problems astronauts (star voyagers) will face while living and working in space during the decades ahead. The challenge to design a tool or item star voyagers on the International Space Station could use to make living in a microgravity environment easier. Aspiring inventors and young innovators answered the challenge with some stunning, innovative tools and items we’re sure astronauts living and working on the space station will find valuable. You can check out the aspiring engineers and their innovative space tools here.

Testing of the Made In Space 3D printer involved 400-plus parabolas of microgravity test flights. Credits: Credit: Made In Space
Testing of the Made In Space 3D printer involved 400-plus parabolas of microgravity test flights. Credit: Made In Space

Read about what astronomers have discovered about the distribution of elements during the first moments of the cosmos.

Help NASA look for young planetary systems that could contain a cradle for a new human Genesis to begin by becoming a Disk Detective.

Learn more about China’s more recent contributions to the human journey to the beginning of space and time.

Check out all of the 3D Printing in Space Challenges issued to young innovators and aspiring engineers by NASA at Future Engineers.

Learn more about the International Space Station.

Join NASA’s journey to the beginning of space and time here.

Learn more about innovative education platform Future Engineers.