NASA’s Planning on Visiting the Water Worlds of the Solar System and Beyond

Next stop the ocean worlds of Enceladus and Europa

This illustration shows Cassini diving through the Enceladus plume in 2015. New ocean world discoveries from Cassini and Hubble will help inform future exploration and the broader search for life beyond Earth.
Credits: NASA/JPL-Caltech

Space news (planetary science: water worlds of the solar system; Enceladus and Europa) – planets and moons around the solar system and exoplanets across the universe covered with water

This graphic illustrates how scientists on NASA’s Cassini mission think water interacts with rock at the bottom of the ocean of Saturn’s icy moon Enceladus, producing hydrogen gas (H2).
The Cassini spacecraft detected the hydrogen in the plume of gas and icy material spraying from Enceladus during its deepest and last dive through the plume on Oct. 28, 2015. Cassini also sampled the plume’s composition during previous flybys, earlier in the mission. From these observations, scientists have determined that nearly 98 percent of the gas in the plume is water vapor, about 1 percent is hydrogen, and the rest is a mixture of other molecules including carbon dioxide, methane, and ammonia.
The graphic shows water from the ocean circulating through the seafloor, where it is heated and interacts chemically with the rock. This warm water, laden with minerals and dissolved gasses (including hydrogen and possibly methane) then pours into the ocean creating chimney-like vents.
The hydrogen measurements were made using Cassini’s Ion and Neutral Mass Spectrometer, or INMS, instrument, which sniffs gasses to determine their composition.
The finding is an independent line of evidence that hydrothermal activity is taking place in the Enceladus ocean. Previous results from Cassini’s Cosmic Dust Analyzer instrument, published in March 2015, suggested hot water is interacting with rock beneath the ocean; the new findings support that conclusion and indicate that the rock is reduced in its geochemistry. With the discovery of hydrogen gas, scientists can now conclude that there is a source of chemical free energy in Enceladus’ ocean.
The Cassini mission is a cooperative project of NASA, ESA (the European Space Agency) and the Italian Space Agency. The Jet Propulsion Laboratory, a division of Caltech in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The Ion and Neutral Mass Spectrometer was designed and built by NASA Goddard Space Flight Center, Greenbelt, Maryland; the team is based at Southwest Research Institute (SwRI) in San Antonio.
For more information about the Cassini mission, visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov.
Image Credit: NASA.

The solar system’s awash in water! NASA missions have provided verifiable facts showing ocean worlds and moons exist in our solar system and beyond, other than Earth. Planetary bodies where water is locked in a frozen embrace and even flowing beneath miles of ice. Liquid water exobiologists are keen to explore for life forms they would love to meet and get to know a little better during the next phase of the human journey to the beginning of space and time. Watch this YouTube video on NASA’s search for life on the ocean worlds of the solar system.

Best Evidence Yet for Reoccurring Water Vapor Plumes Erupting from Jupiter’s Moon
When Galileo discovered Jupiter’s moon Europa in 1610, along with three other satellites whirling around the giant planet, he could have barely imagined it was such a world of wonder.
This revelation didn’t happen until 1979 when NASA’s Voyager 1 and 2 flew by Jupiter and found evidence that Europa’s interior, encapsulated under a crust of ice, has been kept warm over billions of years. The warmer temperature is due to gravitational tidal forces that flex the moon’s interior — like squeezing a rubber ball — keeping it warm. At the time, one mission scientist even speculated that the Voyagers might catch a snapshot of geysers on Europa.
Such activity turned out to be so elusive that astronomers had to wait over three decades for the peering eye of Hubble to monitor the moon for signs of venting activity. A newly discovered plume seen towering 62 miles above the surface in 2016 is at precisely the same location as a similar plume seen on the moon two years earlier by Hubble. These observations bolster evidence that the plumes are a real phenomenon, flaring up intermittently in the same region on the satellite.
The location of the plumes corresponds to the position of an unusually warm spot on the moon’s icy crust, as measured in the late 1990s by NASA’s Galileo spacecraft. Researchers speculate that this might be circumstantial evidence for material venting from the moon’s subsurface. The material could be associated with the global ocean that is believed to be present beneath the frozen crust. The plumes offer an opportunity to sample what might be in the ocean, in the search for life on that distant moon. Credits: NASA/JPL

Papers published by the journal Science and written by Cassini mission scientists and researchers working with the Hubble Space Telescope indicate hydrogen gas believed pouring from the subsurface ocean of Enceladus could potentially provide chemical energy life could use to survive and evolve. Watch this YouTube video called “NASA: Ingredients for Life at Saturn’s moon Enceladus“, it shows the proof scientists used to come to these conclusions. Their work provides new insights concerning possible oceans of water on moons of Jupiter and Saturn and other ocean moons in the solar system and beyond. 

Best Evidence Yet for Reoccurring Water Vapor Plumes Erupting from Jupiter’s Moon
When Galileo discovered Jupiter’s moon Europa in 1610, along with three other satellites whirling around the giant planet, he could have barely imagined it was such a world of wonder.
This revelation didn’t happen until 1979 when NASA’s Voyager 1 and 2 flew by Jupiter and found evidence that Europa’s interior, encapsulated under a crust of ice, has been kept warm over billions of years. The warmer temperature is due to gravitational tidal forces that flex the moon’s interior — like squeezing a rubber ball — keeping it warm. At the time, one mission scientist even speculated that the Voyagers might catch a snapshot of geysers on Europa.
Such activity turned out to be so elusive that astronomers had to wait over three decades for the peering eye of Hubble to monitor the moon for signs of venting activity. A newly discovered plume seen towering 62 miles above the surface in 2016 is at precisely the same location as a similar plume seen on the moon two years earlier by Hubble. These observations bolster evidence that the plumes are a real phenomenon, flaring up intermittently in the same region on the satellite.
The location of the plumes corresponds to the position of an unusually warm spot on the moon’s icy crust, as measured in the late 1990s by NASA’s Galileo spacecraft. Researchers speculate that this might be circumstantial evidence for material venting from the moon’s subsurface. The material could be associated with the global ocean that is believed to be present beneath the frozen crust. The plumes offer an opportunity to sample what might be in the ocean, in the search for life on that distant moon. Credits: NASA/JPL

“This is the closest we’ve come, so far, to identifying a place with some of the ingredients needed for a habitable environment,” said Thomas Zurbuchen, associate administrator for NASA’s Science Mission Directorate at Headquarters in Washington. ”These results demonstrate the interconnected nature of NASA’s science missions that are getting us closer to answering whether we are indeed alone or not.”

Portrait of Thomas Zurbuchen taken on Monday, October 17, 2016, at NASA Headquarters in Washington. Photo Credit: (NASA/Aubrey Gemignani)

Researchers believe they have found evidence indicating hydrogen gas could be pouring out of hydrothermal vents on the floor of Saturn’s moon Enceladus and into these oceans of water. Any microbes existing in these distant waters could use this gas as a form of chemical energy to operate biological processes. By combining hydrogen with carbon dioxide dissolved in this ocean of water in a chemical reaction called methanogenesis, geochemists think methane could be produced which could act as the basis of a tree of life similar to the one observed on Earth. 

Dramatic plumes, both large and small, spray water ice and vapor from many locations along the famed “tiger stripes” near the south pole of Saturn’s moon Enceladus. The tiger stripes are four prominent, approximately 84-mile- (135-kilometer-) long fractures that cross the moon’s south polar terrain.
This two-image mosaic is one of the highest resolution views acquired by Cassini during its imaging survey of the geyser basin capping the southern hemisphere of Saturn’s moon Enceladus. It clearly shows the curvilinear arrangement of geysers, erupting from the fractures. .From left to right, the fractures are Alexandria, Cairo, Baghdad, and Damascus.
As a result of this survey, 101 geysers were discovered: 100 have been located on one of the tiger stripes (PIA17188), and the three-dimensional configurations of 98 of these geysers have also been determined (PIA17186). The source location of the remaining geyser could not be definitively established. These results, together with those of other Cassini instruments, now strongly suggest that the geysers have their origins in the sea known to exist beneath the ice underlying the south polar terrain.
These findings from the imaging survey, of which the two images composing this mosaic are a part, were presented in a paper by Porco, DiNino, and Nimmo and published in the online version of the Astronomical Journal in July 2014: http://dx.doi.org/10.1088/0004-6256/148/3/45.
A companion paper, by Nimmo et al., is available at http://dx.doi.org/10.1088/0004-6256/148/3/46.
The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency, and the Italian Space Agency. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The imaging operations center is based at the Space Science Institute in Boulder, Colo.
For more information about the Cassini-Huygens mission visit http://saturn.jpl.nasa.gov and http://www.nasa.gov/cassini. The Cassini imaging team homepage is at http://ciclops.org.
Photojournal notes: This image has been rotated 180 degrees from its original orientation published on February 2, 2010.
Image Credit:
NASA/JPL/Space Science Institute

On Earth, this process is thought to be at the root of the tree of life, and could even be essential, critical to the origin of life on our little blue dot. Life existing on our planet requires three main ingredients, liquid water, a source of energy for metabolic processes, and specific chemical ingredients to develop and continue to thrive. This study shows Enceladus could have the right ingredients for life to exist, but planetary scientists and exobiologists are looking for evidence of the presence of sulfur and phosphorus. 

This set of images from NASA’s Cassini mission shows how the gravitational pull of Saturn affects the amount of spray coming from jets at the active moon Enceladus. Enceladus has the most spray when it is farthest away from Saturn in its orbit (inset image on the left) and the least spray when it is closest to Saturn (inset image on the right).
Water ice and organic particles gush out of fissures known as “tiger stripes” at Enceladus’ south pole. Scientists think the fissures are squeezed shut when the moon is feeling the greatest force of Saturn’s gravity. They theorize the reduction of that gravity allows the fissures to open and release the spray. Enceladus’ orbit is slightly closer to Saturn on one side than the other. A simplified version of that orbit is shown as a white oval.
Scientists correlate the brightness of the Enceladus plume to the amount of solid material being ejected because the fine grains of water ice in the plume are very bright when lit from behind. Between the dimmest and brightest images, they detected a change of about three to four times in brightness, approximately the same as moving from a dim hallway to a brightly lit office.
This analysis is the first clear finding that shows the jets at Enceladus vary in a predictable manner. The background image is a mosaic made from data obtained by Cassini’s imaging science subsystem in 2006. The inset image on the left was obtained on Oct. 1, 2011. The inset image on the right was obtained on Jan. 30, 2011.
A related image, PIA17039, shows just the Enceladus images. The Saturn system mosaic was created from data obtained by Cassini’s imaging cameras in 2006.
The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency, and the Italian Space Agency. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington, DC. The Cassini orbiter was designed, developed and assembled at JPL. The visual and infrared mapping spectrometer was built by JPL, with a major contribution by the Italian Space Agency. The visual and infrared mapping spectrometer science team is based at the University of Arizona, Tucson.
For more information about the Cassini-Huygens mission, visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov/.
Image Credit:
NASA/JPL-Caltech/University of Arizona/Cornell/SSI

Previous data shows the rocky core of this moon is similar to meteorites containing these two elements, so they’re thought to be chemically similar in nature, and scientists are looking for the same chemical ingredients of life found on Earth, primarily carbon, nitrogen, oxygen, and of course hydrogen, phosphorus, and sulphur.

Linda Spilker
Cassini Project Scientist. Credits: NASA

“Confirmation that the chemical energy for life exists within the ocean of a small moon of Saturn is an important milestone in our search for habitable worlds beyond Earth,” said Linda Spilker, Cassini project scientist at NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, California.

This illustration shows NASA’s Cassini spacecraft about to make one of its dives between Saturn and its innermost rings as part of the mission’s grand finale.
Cassini will make 22 orbits that swoop between the rings and the planet before ending its mission on Sept. 15, 2017, with a final plunge into Saturn. The mission team hopes to gain powerful insights into the planet’s internal structure and the origins of the rings, obtain the first-ever sampling of Saturn’s atmosphere and particles coming from the main rings, and capture the closest-ever views of Saturn’s clouds and inner rings.
During its time at Saturn, Cassini has made numerous dramatic discoveries, including a global ocean that showed indications of hydrothermal activity within the icy moon Enceladus, and liquid methane seas on its moon Titan.
The Cassini mission is a cooperative project of NASA, ESA (the European Space Agency) and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington.
For more information about the Cassini-Huygens mission, visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov.
Image Credit: NASA/JPL-Caltech

Cassini detected hydrogen in plumes of gas and frozen matter spewing from Enceladus during the spacecraft’s deepest pass over its surface on October 28, 2015. This combined with previous data obtained by Cassini’s Ion and Neutral Mass Spectrometer (INMS) during earlier flybys around 2005, helped scientists determine that nearly 98 percent of the material spraying from the surface of the moon is water. The remaining two percent is thought to be around 1 percent hydrogen with some carbon dioxide, methane, ammonia and assorted unknown molecules in the mix. 

Cassini has shown us two independent detections of possible water spewing from the surface of Enceladus. NASA and its partners are currently looking over proposals to send spacecraft to determine if there is an ocean of water beneath its surface by taking a sample. The Europa Life Finder (ELF) is the proposal NASA’s seriously looking at undertaking at this point, but reports indicate a few other proposals are also being discussed. We’ll provide additional information on other proposals as they’re released to media outlets.

“Although we can’t detect life, we’ve found that there’s a food source there for it. It would be like a candy store for microbes,” said Hunter Waite, lead author of the Cassini study.

Two different observations of possible plumes of water spraying from the icy surface of Saturn’s moon Enceladus provides proof hydrothermal activity is occurring beneath. Geophysicists believe hot water is combining chemically with rock and other matter at the bottom of an ocean of water underneath its icy surface to produce hydrogen gas. Hydrogen gas exobiologists think could be used as energy, food of a sort, to sustain life forms exobiologists want to meet and learn more about. A meeting that would change our place in the cosmos, the way we think about the universe, and reality.

Looking for an interplanetary vacation destination? Consider a visit to Europa, one of the Solar System’s most tantalizing moons. Ice-covered Europa follows an elliptical path in its 85-hour orbit around our ruling gas giant Jupiter. Heat generated from strong tidal flexing by Jupiter’s gravity keeps Europa’s salty subsurface ocean liquid all year round. That also means even in the absence of sunlight Europa has energy that could support simple life forms. Unfortunately, it is currently not possible to make reservations at restaurants on Europa, where you might enjoy a dish of the local extreme shrimp. But you can always choose another destination from Visions of the Future.

Astronomers and researchers working with the Hubble Space Telescope in 2016 reported on an observation of a possible plume erupting from the icy surface of Europa in the same general location Hubble observed a possible plume in 2014. This location also corresponds to the unusually warm region with cracks in the icy surface observed by NASA’s Galileo spacecraft back in the 1990s. This provides evidence this phenomenon could be periodic, intermittent in this region of the moon. Mission planners are looking at this region as a possible location to obtain a sample of water erupting from a possible ocean of water beneath its icy surface. Watch this video on Europa.

Estimates of the size of this most recently observed plume indicate it rose about 62 miles (~100 kilometers) from the surface of Europa, while the plume in 2014 only reached a height of around 30 miles (50 kilometers). 

William Sparks
Space Telescope Science Institute. Credits: Space Science Institute/NASA/JPL

“The plumes on Enceladus are associated with hotter regions, so after Hubble imaged this new plume-like feature on Europa, we looked at that location on the Galileo thermal map. We discovered that Europa’s plume candidate is sitting right on the thermal anomaly,” said William Sparks of the Space Telescope Science Institute in Baltimore, Maryland. Sparks led the Hubble plume studies in both 2014 and 2016.

One interesting thought’s the plumes and the hot spot is somehow linked. If this is the case, it could mean the vented water’s falling onto the surface of the moon, which would change the structure and chemistry of the surface grains and allow them to retain heat longer than the surrounding region. This location would be a great place to search for the ingredients of life and a possible entry point into an ocean of water beneath.

NASA’s Europa Clipper mission is being designed to fly by the icy Jovian moon multiple times and investigate whether it possesses the ingredients necessary for life.
Credits: NASA/JPL-Caltech/SETI Institute

These observations by the Hubble Space Telescope and future looks enable future space missions to Europa and other ocean worlds in the solar system. Specifically, laying the groundwork for NASA’s Europa Clipper mission, which is set for a launch sometime in the 2020s. 

James Green: Director of Planetary Science, NASA Headquarters. Credits: NASA

“If there are plumes on Europa, as we now strongly suspect, with the Europa Clipper we will be ready for them,” said Jim Green, Director of Planetary Science, at NASA Headquarters.

NASA has indicated they’re looking to identify a possible site with persistent, intermittent plume activity as a target location for a mission to Europa to explore using its powerful suite of science instruments. Another team’s currently at work on a powerful ultraviolet camera to add to the Europa Clipper that would offer data similar to that provided by the Hubble Space Telescope, while some members of the Cassini team are working on a very sensitive, next generation INMS instrument to put on the spacecraft. 

Water’s the story of life on Earth! Science has shown it played and plays the main part in the birth, evolution, and sustenance of life on Earth. 

NASA’s planning on taking the human journey to the beginning of space and time to the ocean worlds of the solar system during the decades ahead. To search for the ingredients of life and even possibly simple one-celled life forms, of an unknown type. We plan on going along for the ride to have a look for ourselves and we hope to see your name on the ship manifest. We’ll save a seat for you.

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Planetary scientists searching the Red Planet for signs of past and present water believe they have found evidence indicating Mars once was a lot wetter and a possible location for the evolution of life.

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Europa Spacecraft

Set to blast off sometime in the 2020s

This artist’s rendering shows NASA’s Europa mission spacecraft, which is being developed for a launch sometime in the 2020s. This view shows the spacecraft configuration, which could change before launch, as of early 2016.
The mission would place a spacecraft in orbit around Jupiter in order to perform a detailed investigation of the giant planet’s moon Europa — a world that shows strong evidence for an ocean of liquid water beneath its icy crust and which could host conditions favorable for life. The highly capable, radiation-tolerant spacecraft would enter into a long, looping orbit around Jupiter to perform repeated close flybys of Europa.
The concept image shows two large solar arrays extending from the sides of the spacecraft, to which the mission’s ice-penetrating radar antennas are attached. A saucer-shaped high-gain antenna is also side mounted, with a magnetometer boom placed next to it. On the forward end of the spacecraft (at left in this view) is a remote-sensing palette, which houses the rest of the science instrument payload.
The nominal mission would perform at least 45 flybys of Europa at altitudes varying from 1,700 miles to 16 miles (2,700 kilometers to 25 kilometers) above the surface.
This view takes artistic liberty with Jupiter’s position in the sky relative to Europa and the spacecraft. Credits: NASA/JPL/ESA

Space news (The search for life beyond Earth) – An artist’s rendition of the Europa spacecraft orbiting Jupiter

This 12-frame mosaic provides the highest resolution view ever obtained of the side of Jupiter’s moon Europa that faces the giant planet. It was obtained on Nov. 25, 1999 by the camera onboard the Galileo spacecraft, a past NASA mission to Jupiter and its moons which ended in 2003. NASA will announce today, Tuesday, May 26, the selection of science instruments for a mission to Europa, to investigate whether it could harbor conditions suitable for life. The Europa mission would conduct repeated close flybys of the small moon during a three-year period.
Numerous linear features in the center of this mosaic and toward the poles may have formed in response to tides strong enough to fracture Europa’s icy surface. Some of these features extend for over 1,500 kilometers (900 miles). Darker regions near the equator on the eastern (right) and western (left) limb may be vast areas of chaotic terrain. Bright white spots near the western limb are the ejecta blankets of young impact craters.
North is to the top of the picture and the sun illuminates the surface from the left. The image, centered at 0 latitude and 10 longitude, covers an area approximately 2,500 by 3,000 kilometers. The finest details that can discerned in this picture are about 2 kilometers across (about 1,550 by 1,860 miles). The images were taken by Galileo’s camera when the spacecraft was 94,000 kilometers (58,000 miles) from Europa.
Image Credit: NASA/JPL/University of Arizona

NASA’s Jet Propulsion Laboratory released this artists rendering of the Europa spacecraft, which is set to head to Jupiter sometime in the 2020s. The Europa Mission spacecraft configuration in early 2016 is shown in this image. The final spacecraft configuration at launch could easily be different, so stay tuned here for more news. The position of Jupiter in the sky relative to Europa and the spacecraft are also off in this drawing

This is an artist’s concept of a plume of water vapor thought to be ejected off the frigid, icy surface of the Jovian moon Europa, located about 500 million miles (800 million kilometers) from the sun. Spectroscopic measurements from NASA’s Hubble Space Telescope led scientists to calculate that the plume rises to an altitude of 125 miles (201 kilometers) and then it probably rains frost back onto the moon’s surface. Previous findings already pointed to a subsurface ocean under Europa’s icy crust.
Image credit: NASA/ESA/K. Retherford/SWRI

Two large solar arrays are shown extending from the sides of the Europa spacecraft to which the ice-penetrating radar antennas are attached in this artist’s rendition. On the side of the craft, a saucer-shaped high gain antenna is depicted next to a magnetometer boom. On the forward section is a remote-sensing palette with the remaining science instruments.

Jupiter’s moon Europa has a crust made up of blocks, which are thought to have broken apart and ‘rafted’ into new positions, as shown in the image on the left. These features are the best geologic evidence to date that Europa may have had a subsurface ocean at some time in its past.
Combined with the geologic data, the presence of a magnetic field leads scientists to believe an ocean is most likely present at Europa today. In this false color image, reddish-brown areas represent non-ice material resulting from geologic activity. White areas are rays of material ejected during the formation of the Pwyll impact crater. Icy plains are shown in blue tones to distinguish possibly coarse-grained ice (dark blue) from fine-grained ice (light blue). Long, dark lines are ridges and fractures in the crust, some of which are more than 1,850 miles long. These images were obtained by NASA’s Galileo spacecraft during Sept. 7, 1996, Dec. 1996 and Feb. 1997 at a distance of 417,489 miles.
Image Credit: NASA/JPL/University of Arizona

The Europa Mission profile has a very capable, radiation-resistant spacecraft traveling to Jupiter, where it enters into a long, looping orbit of the giant planet in order to perform at least 45 repeated flybys of Europa at altitudes ranging from 1700 miles to 16 miles (2700 kilometers to 25 kilometers) above its surface. Planetary scientists want to take a closer look at the evidence for an ocean of liquid water beneath its icy shell. An ocean of liquid water that could be the habitat of alien lifeforms we want to get to know better. 

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Travel into the heart of a cosmic storm over 200,000 light-years away in one of many large satellite galaxies orbiting the Milky Way, the Large Magellanic Cloud.

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Travel into the Heart of a Cosmic Storm

This shot from the NASA/ESA Hubble Space Telescope shows a maelstrom of glowing gas and dark dust within one of the Milky Way’s satellite galaxies, the Large Magellanic Cloud (LMC). This stormy scene shows a stellar nursery known as N159, an HII region over 150 light-years across. N159 contains many hot young stars. These stars are emitting intense ultraviolet light, which causes nearby hydrogen gas to glow, and torrential stellar winds, which are carving out ridges, arcs, and filaments from the surrounding material. At the heart of this cosmic cloud lies the Papillon Nebula, a butterfly-shaped region of nebulosity. This small, dense object is classified as a High-Excitation Blob, and is thought to be tightly linked to the early stages of massive star formation. N159 is located over 160 000 light-years away. It resides just south of the Tarantula Nebula (heic1402), another massive star-forming complex within the LMC. It was previously imaged by Hubble’s Wide Field Planetary Camera 2, which also resolved the Papillon Nebula for the first time.
Electric-blue wisps of gas and young stars in early stages of star birth startle the senses in this stunning Hubble Space Telescope image. Credits: NASA/Hubble/ESA

Space news (astrophysics: stellar nurseries; HII region N159) – 180,000 light-years from Earth deep within the Large Magellanic Cloud (LMC) –

Nearly 200 000 light-years from Earth, the Large Magellanic Cloud, a satellite galaxy of the Milky Way, floats in space, in a long and slow dance around our galaxy. As the Milky Way’s gravity gently tugs on its neighbour’s gas clouds, they collapse to form new stars. In turn, these light up the gas clouds in a kaleidoscope of colours, visible in this image from the NASA/ESA Hubble Space Telescope.
Nearly 200 000 light-years from Earth, the Large Magellanic Cloud, a satellite galaxy of the Milky Way, floats in space, in a long and slow dance around our galaxy. As the Milky Way’s gravity gently tugs on its neighbour’s gas clouds, they collapse to form new stars. In turn, these light up the gas clouds in a kaleidoscope of colours, visible in this image from the NASA/ESA Hubble Space Telescope.

The stunning Hubble Space Telescope image seen above shows the heart of a cosmic maelstrom, glowing gas, and dark dust deep within the Large Magellanic Cloud (LMC), one of many satellite galaxies of the Milky Way. This stormy region of space contains stellar nursery N159, an HII region over 150 light-years across with many hot young suns emitting intense ultraviolet radiation. Ultraviolet light causing nearby hydrogen gas to glow and torrential stellar winds carving ridges, arcs, and filaments out of surrounding gas and dust. 

papillon_hst_big
The Papillon Nebula is seen in the inset image in  the top right of the main image of the Large Magellanic Cloud. Credit: M. Heydari-Malayeri(Paris Observatory) et al, WFPC2, HST, ESA, NASA

Early stages of star birth

Near the heart of this cosmic maelstrom lies the butterfly-shaped Papillon Nebula, a small, dense stellar object astronomers refer to as a High-Excitation Blob, they have linked to the early stages of the formation of a massive star. This region of space was first detected using Hubble Space Telescope’s Wide Field Planetary Camera 2 (WFPC2).

Image Credit & Copyright: Processing - Robert Gendler, Roberto Colombari Data - Hubble Tarantula Treasury, European Southern Observatory
The Tarantula Nebula Image Credit & Copyright: Processing – Robert Gendler, Roberto Colombari Data – Hubble Tarantula Treasury, European Southern Observatory

Nebula N159’s just south of the Tarantula Nebula (heic 1402), a star-forming region also imaged by Hubble’s WFPC2. Hidden within this region of space astronomers found several massive stars they’re currently studying looking for clues to the growth and evolution of the most massive stars in the galaxy. The image seen here was taken using the Hubble Space Telescope’s Advanced Camera for Surveys. 

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NASA Engineers Test Prototype Robotic Asteroid Capture System 

In order to better understand intricate operations and detailed planning needed to capture multi-ton boulder from asteroid surface

A prototype of the Asteroid Redirect Mission (ARM) robotic capture module system is tested with a mock asteroid boulder in its clutches at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. The robotic portion of ARM is targeted for launch in 2021. Located in the center’s Robotic Operations Center, the mockup helps engineers understand the intricate operations required to collect a multi-ton boulder from an asteroid’s surface. The hardware involved here includes three space frame legs with foot pads, two seven degrees of freedom arms that have with microspine gripper “hands” to grasp onto the boulder. NASA and students from West Virginia University built the asteroid mockup from rock, styrofoam, plywood and an aluminum endoskeleton. The mock boulder arrived in four pieces and was assembled inside the ROC to help visualize the engagement between the prototype system and a potential capture target. Inside the ROC, engineers can use industrial robots, a motion-based platform, and customized algorithms to create simulations of space operations for robotic spacecraft. The ROC also allows engineers to simulate robotic satellite servicing operations, fine tuning systems and controllers and optimizing performance factors for future missions when a robotic spacecraft might be deployed to repair or refuel a satellite in orbit. Image Credit: NASA
A prototype of the Asteroid Redirect Mission (ARM) robotic capture module system is tested with a mock asteroid boulder in its clutches at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. The robotic portion of ARM is targeted for launch in 2021.
Located in the center’s Robotic Operations Center, the mockup helps engineers understand the intricate operations required to collect a multi-ton boulder from an asteroid’s surface. The hardware involved here includes three space frame legs with footpads, two seven degrees of freedom arms that have with microspine gripper “hands” to grasp onto the boulder.
NASA and students from West Virginia University built the asteroid mockup from rock, styrofoam, plywood and an aluminum endoskeleton. The mock boulder arrived in four pieces and was assembled inside the ROC to help visualize the engagement between the prototype system and a potential capture target.
Inside the ROC, engineers can use industrial robots, a motion-based platform, and customized algorithms to create simulations of space operations for robotic spacecraft. The ROC also allows engineers to simulate robotic satellite-servicing operations, fine-tuning systems and controllers and optimizing performance factors for future missions when a robotic spacecraft might be deployed to repair or refuel a satellite in orbit.
Image Credit: NASA

Space news (Asteroid Redirect Mission: testing of prototype of robotic capture module system) – The Robotic Operations Center of NASA’s Goddard Space Flight Center

NASA's Asteroid Redirect Missions. Credits: NASA/Goddard
A new report provides expert findings from a special action team on how elements of the Asteroid Redirect Mission (ARM) can address decadal science objectives and help close Strategic Knowledge Gaps (SKGs) for future human missions in deep space. Credits: NASA/Goddard

Inside the Robotic Operations Center (ROC) of NASA’s Goddard Space Flight Center engineers are at work preparing the robotic section of the Asteroid Redirect Mission (ARM). The most recent work involved testing a prototype of the asteroid capture system with a mock boulder built by NASA and students from West Virginia University. This work will help engineers learn more about the intricate operations needed to capture a multi-ton boulder from the surface of an asteroid. The robotic section of ARM is targeted for a 2021 launch window.

The capability built into the ROC allows engineers to create a simulation of the capture of a boulder from the surface of an asteroid. Here they can also simulate servicing of the satellite, fine tuning of systems and controllers, and even optimize all performance factors for future repairs and refueling. An important capability when building spacecraft worth hundreds of millions of dollars and even more. One that saves money and time.

The Asteroid Redirect Mission is expected to offer benefits that should teach us more about operating in space and enable future space missions. You can read a report here on some of the expected benefits.

The report reflects the findings of a two-month study conducted by members of the Small Bodies Assessment Group (SBAG). It explains many of ARM’s potential contributions to the future of the human journey to the beginning of space and time.

“This report is an important step in identifying ways that ARM will be more scientifically relevant as we continue mission formulation for the robotic and the crew segments,” said Gates. “We’re currently in the process of selecting hosted instruments and payloads for the robotic segment, and hope to receive an updated analysis from the SBAG after we announce those selections in spring 2017.”

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Discover and learn more about the ferocious winds near the biggest magnets discovered during the human journey to the beginning of space and time, magnetars.

Read about NASA’s latest additions to its plans to send manned missions to Mars.

Discover and learn about the feedback mechanisms of supermassive black holes.

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

Read about NASA’s Asteroid Redirect Mission.

Discover NASA’s Goddard Space Flight Center.

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.”

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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. 

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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. 

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