Tag: space

  • NASA Hosts Kepler Spacecraft Status Teleconference Today

    NASA will host a news teleconference at 4 p.m. EDT, today, May 15, to discuss the status of the agency’s Kepler Space Telescope.

  • Kepler Mission Manager Update

    During a scheduled contact, engineers discovered Kepler was in a self-protective mode. The spacecraft returned to science data collection on May 6.

  • Kepler Mission Manager Update

    The team recently completed a monthly science data download, marking the successful completion of Quarter 16 flight operations.

  • NASA TV Briefing Discusses Alpha Magnetic Spectrometer Results

    NASA will hold a news conference at 1:30 p.m. EDT on Wednesday, April 3, to discuss the first results of the Alpha Magnetic Spectrometer (AMS) experiment. AMS is a state-of-the-art cosmic ray particle physics detector located on the exterior of the International Space Station.

  • Watch Live @ 9 pm ET: Slooh Earth Day Webcast

    The Slooh community observatory will be celebrating Earth Day on Saturday (April 22), with a webcast beginning at 9 a.m. EDT (1300 GMT). During the webcast, members of the public will share the things they’d miss most about Earth if they had to go to space, while two astronauts will name the things they did miss during their journeys to space. You can watch the Earth Day webcast live via Slooh.com, or in the window below, courtesy of Slooh. 

    From Slooh: 

    “On Saturday, 22nd April 2017 … Slooh will host a special live show for Earth Day, sponsored by the digital release of Sony Pictures’ Passengers.  

    “Over the last month, people from all over the world have sent in videos to Slooh answering one very important question: what would they would miss about our planet if they were to go into space? During the live show, Slooh will share a compilation of the best submissions and will explore what about the Earth inspires those who reach for the stars. The show will be anchored by live views of the Earth from space and with live feeds of various beautiful vistas around the world from Slooh’s observatory in the Canary Islands, as well as cameras around the globe.

    “Headlining the show are NASA astronauts Doctors Tracy Caldwell Dyson and Stan Love. They will be sharing what they missed about Earth when they were away in space, how their unique perspective deepened their appreciation of the planet, and what they will be doing to honor Earth this Earth Day.
     
    “Academy-award nominated production designer, Guy Hendrix Dyas, will also join the show to talk about why the concept of leaving Earth is so popular in science fiction, and his experience of capturing the contrast between outer space and Earth in his latest movie, Passengers. 

    “‘No matter who we are or where we live, we all share a common home — Earth,’ says Slooh Human Spirit Editor, Helen Avery. ‘In the day-to-day, we often forget that we are all connected, as too do we often forget just how wondrous our planet is. It is the most diverse of all those in our solar system, and — as far as we yet know — in the universe. Earth Day is a wonderful time to come together to remember and to appreciate the home we all share.’

    “Join with Slooh and people from around the world to celebrate the wonder of our planet, as we remind ourselves … there really is no place like home. 

    “Viewers can join in on the celebration on Twitter by sending questions and comments to @Slooh or using the hashtag #noplacelikehome. Viewers are also encouraged to join the rest of the Slooh Community in expressing on Twitter what they would miss most about Earth if they had to travel into space.”

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  • 2016 Moon Phases Calendar

    Thursday, Dec. 6, 2012, 10:31 a.m. EST. The last or third quarter moon rises around 11:30 p.m. and sets around 12:15 p.m. It is most easily seen just after sunrise in the southern sky.

    Some nights when we look up at the moon, it is full and bright; sometimes it is just a sliver of silvery light. These changes in appearance are the phases of the moon. As the moon orbits Earth, it cycles through eight distinct phases. The four primary phases occur about a week apart.

    Editor’s Note: The next full moon will be the Beaver Moon and will peak on Monday, Nov. 14 at 8:52 a.m. EST (1352 GMT).The November full moon will coincide with the moon’s arrival at perigee, the point at which it is closest to Earth in its monthly orbit. Such Perigee Full Moon are also sometimes called Supermoon Full Moons. Our Full Guide: Supermoon November 2016: When, Where & How to See It

    Here are the dates of the moon’s phases for 2016 (and for December 2015), according to NASA. Times and dates are in Universal Time. Subtract five hours to get Eastern U.S. time. 

    New Moon 1st Quarter Full Moon Last Quarter
                Dec. 3 07:40
    Dec. 11 10:29 Dec. 18 15:14 Dec. 25 11:11 Jan. 2 05:30
    Jan. 10 01:30 Jan. 16 23:26 Jan. 24 01:46 Feb. 1 03:28
    Feb. 8 14:39 Feb. 15 07:46 Feb. 22 18:20 Mar. 1 23:11
    Mar. 9 01:54 Mar. 15 17:03 Mar. 23 12:01 Mar. 31 15:17
    Apr. 7 11:24 Apr. 14 03:59 Apr. 22 05:24 Apr. 30 03:29
    May 6 19:30 May 13 17:02 May 21 21:15 May 29 12:12
    Jun. 5 03:00 Jun. 12 08:10 Jun. 20 11:02 Jun. 27 18:19
    Jul. 4 11:01 Jul. 12 00:52 Jul. 19 22:57 Jul. 26 23:00
    Aug. 2 20:45 Aug. 10 18:21 Aug. 18 09:27 Aug. 25 03:41
    Sep. 1 09:03 Sep. 9 11:49 Sep. 16 19:05 Sep. 23 09:56
    Oct. 1 00:12 Oct. 9 04:33 Oct. 16 04:23 Oct. 22 19:14
    Oct. 30 17:38 Nov. 7 19:51 Nov. 14 13:52 Nov. 21 08:33
    Nov. 29 12:18 Dec. 7 09:03 Dec. 14 00:05 Dec. 21 01:56
    Dec. 29 06:53            

    The moon, like Earth, is a sphere, and it is always half-illuminated by the sun. However, as the moon travels around Earth, we see more or less of the illuminated half. The moon’s phases describe how much of the moon’s disk is illuminated from our perspective.

    New moon: The moon is between Earth and the sun, and the side of the moon facing toward us receives no direct sunlight; it is lit only by dim sunlight reflected from Earth.

    Waxing crescent: As the moon moves around Earth, the side we can see gradually becomes more illuminated by direct sunlight.

    First quarter: The moon is 90 degrees away from the sun in the sky and is half-illuminated from our point of view. We call it “first quarter” because the moon has traveled about a quarter of the way around Earth since the new moon.

    <img class=”pure-img lazy” big-src=”http://www.space.com/images/i/000/000/398/original/moon-phases-101111-02.jpg?1289850911″ data-src=”http://www.space.com/images/i/000/000/398/i01/moon-phases-101111-02.jpg?1289850911?interpolation=lanczos-none&downsize=192:*” alt=”See the moon phases, and the difference between a waxing and waning crescent or gibbous moon, in this Space.com infographic about the lunar cycle each month. See the full infographic. ” data-options-closecontrol=”true” data-options-fullsize=”true”/>
    See the moon phases, and the difference between a waxing and waning crescent or gibbous moon, in this Space.com infographic about the lunar cycle each month. See the full infographic.

    Credit: Karl Tate, SPACE.com

    Waxing gibbous: The area of illumination continues to increase. More than half of the moon’s face appears to be getting sunlight.

    Full moon: The moon is 180 degrees away from the sun and is as close as it can be to being fully illuminated by the sun from our perspective. The sun, Earth and the moon are aligned, but because the moon’s orbit is not exactly in the same plane as Earth’s orbit around the sun, they rarely form a perfect line. When they do, we have a lunar eclipse as Earth’s shadow crosses the moon’s face.

    Waning gibbous: More than half of the moon’s face appears to be getting sunlight, but the amount is decreasing.

    Last quarter: The moon has moved another quarter of the way around Earth, to the third quarter position. The sun’s light is now shining on the other half of the visible face of the moon.

    Waning crescent: Less than half of the moon’s face appears to be getting sunlight, and the amount is decreasing.

    Finally, the moon is back to its new moon starting position. Now, the moon is between Earth and the sun. Usually the moon passes above or below the sun from our vantage point, but occasionally it passes right in front of the sun, and we get a solar eclipse. [Infographic: How Moon Phases Work]

    NASA’s Sky Events Calendar

  • Amazing Mars Photos by NASA's Curiosity Rover (Latest Images)

    This illustration provides a comparison for how big the moons of Mars appear to be, as seen from the surface of Mars, in relation to the size that Earth’s moon appears to be when seen from the surface of Earth. Deimos, at far left, and Phobos, beside it, are shown together as they actually were photographed by the Mast Camera (Mastcam) NASA’s Mars rover Curiosity on Aug. 1, 2013. [Read the Full Story]

  • Watch Live! Now: 2017 Astronaut Class Interviews, Later: NASA Budget Hearing

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    NASA’s newest astronauts are meeting the press in a series of televised interviews today through 1 p.m. EDT (1700 GMT). Space.com’s Hanneke Weitering will interview astronaut candidate Robb Kulin, formerly of SpaceX, at 11:20 a.m. EDT (1520 GMT). Tune in!

    Main Story: NASA Reveals 12 New Astronauts for Earth Orbit, Deep Space Missions

    What’s Next for NASA’s New Astronaut Class?

    Vice President Welcomes NASA’s ‘Newest Heroes’ to Astronaut Corps

    Astronauts Record Awesome Welcome Video for NASA’s 2017 Recruits

    What It’s Like to Become a NASA Astronaut: 10 Surprising Facts

    NASA announced the 2017 astronaut class Wednesday, June 7, at the Johnson Space Center in Houston. The astronaut candidates will be presented by acting NASA Administrator Robert Lightfoot, JSC director Ellen Ochoa and Flight Operations Director Brian Kelly. Vice President Mike Pence welcomed the new astronauts to NASA and toured the agency’s Mission Control Center. He also received briefings on the agency’s current human spaceflight operations. 

    Live @ 2 p.m. EDT: NASA Budget Overview with House Appropriations Committee

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    At 2 p.m. EDT (1800 GMT) today, acting NASA chiefe Robert Lightfoot will give testimony before the House Appropriations Committee during a hearing on the agency’s proposed 2018 budget. The meeting follows a 10 a.m. EDT (1400 GMT) hearing on the same subject, where Lightfoot is also appearing as a witness, by the Space Subcommittee of the House Committee on Space, Science and Technology. 

  • Exoplanets: Worlds Beyond Our Solar System

    The youngest exoplanet yet discovered is less than 1 million years old.
    The youngest exoplanet yet discovered is less than 1 million years old and orbits Coku Tau 4, a star 420 light-years away. Astronomers inferred the planet’s presence from an enormous hole in the dusty disk that girdles the star. The hole is 10 times the size of Earth’s orbit around the Sun and probably caused by the planet clearing a space in the dust as it orbits the star.
    Credit: NASA

    Exoplanets are planets beyond our own solar system. Thousands have been discovered in the past two decades, mostly with NASA’s Kepler space telescope. 

    These worlds come in a huge variety of sizes and orbits. Some are gigantic planets hugging close to their parent stars; others are icy, some rocky. NASA and other agencies are looking for a special kind of planet: one that’s the same size as Earth, orbiting a sun-like star in the habitable zone.

    The habitable zone is the range of distances from a star where a planet’s temperature allows liquid water oceans, critical for life on Earth. The earliest definition of the zone was based on simple thermal equilibrium, but current calculations of the habitable zone include many other factors, including the greenhouse effect of a planet’s atmosphere. This makes the boundaries of a habitable zone “fuzzy.”  

    Early discoveries

    While exoplanets were not confirmed until the 1990s, for years beforehand astronomers were convinced they were out there. That wasn’t just wishful thinking, but because of how slowly our own sun and other stars like it spin, University of British Columbia astrophysicist Jaymie Matthews told Space.com. Matthews, the mission scientist of occasional exoplanet telescope observer MOST (Microvariability and Oscillations of STars), was involved in some of the early exoplanet discoveries.

    Astronomers had an origin story for our solar system. Simply put, a spinning cloud of gas and dust (called the protosolar nebula) collapsed under its own gravity and formed the sun and planets.  As the cloud collapsed, conservation of angular momentum meant the soon-to-be-sun should have spun faster and faster. But, while the sun contains 99.8 percent of the solar system’s mass, the planets have 96 percent of the angular momentum. Astronomers asked themselves why the sun rotates so slowly.

    The young sun would have had a very strong magnetic field, whose lines of force reached out into the disk of swirling gas from which the planets would form. These field lines connected with the charged particles in the gas, and acted like anchors, slowing down the spin of the forming sun and spinning up the gas that would eventually turn into the planets. Most stars like the sun rotate slowly, so astronomers inferred that the same “magnetic braking” occurred for them, meaning that planet formation must have occurred for them. The implication: Planets must be common around sun-like stars.

    For this reason and others, astronomers at first restricted their search for exoplanets to stars similar to the sun, but the first two discoveries were around a pulsar (rapidly spinning corpse of a star that died as a supernova) called PSR 1257+12, in 1992. The first confirmed discovery of a world orbiting a sun-like star, in 1995, was 51 Pegasi b — a Jupiter-mass planet 20 times closer to its sun than we are to ours. That was a surprise. But another oddity popped up seven years earlier that hinted at the wealth of exoplanets to come.

    A Canadian team discovered a Jupiter-size planet around Gamma Cephei in 1988, but because its orbit was much smaller than Jupiter’s, the scientists did not claim a definitive planet detection. “We weren’t expecting planets like that. It was different enough from a planet in our own solar system that they were cautious,” Matthews said.  

    Alien Worlds Infographic Poster

    Alien Worlds Infographic 20″x60″ Poster. Buy Here
    Credit: Space.com Store

    Explosion of data

    Most of the first exoplanet discoveries were huge Jupiter-size (or larger) gas giants orbiting close to their parent stars. That’s because astronomers were relying on the radial velocity technique, which measures how much a star “wobbles” when a planet or planets orbit it. These large planets close in produce a correspondingly big effect on their parent star, causing an easier-to-detect wobble.

    Before the era of exoplanet discoveries, instruments could only measure stellar motions down to a kilometer per second, too imprecise to detect a wobble due to a planet. Now, some instruments can measure velocities as low as a centimeter per second, according to Matthews. “Partly due to better instrumentation, but also because astronomers are now more experienced in teasing subtle signals out of the data.”

    Today, there are more than 1,000 confirmed exoplanets discovered by a single telescope: the Kepler space telescope, which reached orbit in 2009 and hunted for habitable planets for four years. Kepler uses a technique called the “transit” method, measuring how much a star’s light dims when a planet passes in front of it.

    Kepler has revealed a cornucopia of different types of planets. Besides gas giants and terrestrial planets, it has helped define a whole new class known as “super-Earths”: planets that are between the size of Earth and Neptune. Some of these are in the habitable zones of their stars, but astrobiologists are going back to the drawing board to consider how life might develop on such worlds.

    In 2014, Kepler astronomers (including Matthews’ former student Jason Rowe) unveiled a “verification by multiplicity” method that should increase the rate at which astronomers promote candidate planets to confirmed planets. The technique is based on orbital stability — many transits of a star occurring with short periods can only be due to planets in small orbits, since multiply eclipsing stars that might mimic would gravitationally eject each other from the system in just a few million years.

    While the Kepler (and French CoRoT) planet-hunting satellites have ended their original missions, scientists are still mining the data for discoveries, and there are more to come. MOST is still operating, and the NASA TESS (Transiting Exoplanet Survey Satellite), Swiss CHEOPS (Characterizing ExOPlanets Satellite) and ESA’s PLATO missions will soon pick up the transit search from space.  From the ground, the HARPS spectrograph on the European Southern Observatory’s La Silla 3.6-meter telescope in Chile is leading the Doppler wobble search, but there are many other telescopes in the hunt. 

    One too-neglected example, Matthews said, is NASA’s Spitzer Space Telescope. Because it is sensitive in the infrared, it can sense the temperature profile of an exoplanet and give insights into its atmosphere.

    A diagram showing the relative sizes of the new alien planets discovered by Kepler, compared to Earth and Jupiter.

    A diagram showing the relative sizes of the new alien planets discovered by Kepler, compared to Earth and Jupiter.
    Credit: NASA/Tim Pyle

    Notable exoplanets

    With almost 2,000 to choose from, it’s hard to narrow down a few. Small solid planets in the habitable zone are automatically standouts, but Matthews singled out five other exoplanets that have expanded our perspective on how planets form and evolve:

    • 51 Pegasi b: As mentioned earlier, this was the first planet to be confirmed around a sun-like star. Half the mass of Jupiter, it orbits around its sun at roughly the distance of Mercury from our Sun. 51 Pegasi b is so close to its parent star that it is likely tidally locked, meaning one side always faces the star.
    • HD 209458 b: This was the first planet found (in 1999) to transit its star (although it was discovered by the Doppler wobble technique) and in subsequent years more discoveries piled up. It was the first planet outside the solar system for which we could determine aspects of its atmosphere, including temperature profile and the lack of clouds. (Matthews participated in some of the observations using MOST.)
    • 55 Cancri e: This super-Earth orbits a star that is bright enough to see by eye, meaning astronomers can study the system in more detail than almost any other.  Its “year” is only 17 hours and 41 minutes long (recognized when MOST gazed at the system for two weeks in 2011). Theorists speculate that the planet may be carbon-rich, with a diamond core.
    • HD 80606 b: At the time of its discovery in 2001, it held the record as the most eccentric exoplanet ever discovered. It is possible that its odd orbit (which is similar to Halley’s Comet around the sun) may be due to the influence of another star. Its extreme orbit would make the planet’s environment extremely variable.
    • WASP-33b: This planet was discovered in 2011 and has a sort of “sunscreen” layer — a stratosphere — that absorbs some of the visible and ultraviolet light from its parent star. Not only does this planet orbit its star “backward,” but it also triggers vibrations in the star, seen by the MOST satellite. 
  • Water on Mars: Exploration & Evidence

    Liquid water may still flow on Mars, but that doesn’t mean it’s easy to spot. The search for water on the Red Planet has taken more than 15 years to turn up definitive signs that liquid flows on the surface today. In the past, however, rivers and oceans may have covered the land. Where did all of the liquid water go? Why? How much of it still remains?

    Observations of the Red Planet indicate that rivers and oceans may have been prominent features in its early history. Billions of years ago, Mars was a warm and wet world that could have supported microbial life in some regions. But the planet is smaller than Earth, with less gravity and a thinner atmosphere. Over time, as liquid water evaporated, more and more of it escaped into space, allowing less to fall back to the surface of the planet.

    Where is the water today?

    Liquid water appears to flow from some steep, relatively warm slopes on the Martian surface. First identified in 2011, features known as recurring slope lineae (RSL) were confirmed to be signs of salty water running on the surface of the planet today. The dark streaks appear seasonally on Martian slopes were found in images taken by the High Resolution Imaging Science Experiment (HiRISE) camera aboard the Mars Reconnaissance Orbiter (MRO) Spectral analysis of RSL lead scientists to conclude they are caused by salty liquid water. [Related: Salty Water Flows on Mars Today, Boosting Odds for Life]

    “The detection of hydrated salts on these slopes means that water plays a vital role in the formation of these streaks,” the study’s lead author, Lujendra Ojha, of the Georgia Institute of Technology in Atlanta, said in a statement.

    Vast deposits of water appear to be trapped within the ice caps at the north and south poles of the planet. Each summer, as temperatures increase, the caps shrink slightly as their contents skip straight from solid to gas form, but in the winter, cooler temperatures cause them to grow to latitudes as low as 45 degrees, or halfway to the equator. The caps are an average of 2 miles (3 kilometers) thick and, if completely melted, could cover the Martian surface with about 18 feet (5.6 meters) of water. 

    Frozen water also lies beneath the surface. Scientists discovered a slab of ice as large as California and Texas combined in the region between the equator and north pole of the Red Planet. The presence of subsurface water has long been suspected but required the appearance of strange layered craters to confirm. Other regions of the planet may contain frozen water, as well. Some high-latitude regions seem to boast patterned ground-shapes that may have formed as permafrost in the soil freezes and thaws over time. 

    The European Space Agency’s Mars Express spacecraft captured images of sheets of ice in the cooler, shadowed bottoms of craters, which suggests that liquid water can pool under appropriate conditions. Other craters identified by NASA’s Mars Reconnaissance Orbiter show similar pooling.

    Evidence for water on Mars first came to light in 2000, with the appearance of gullies that suggested a liquid origin. Their formation has been hotly debated over the ensuing years.

    Young Mars Crater Contains Water Ice, Photo Shows

    At the center of this view of an area of mid-latitude northern Mars, a fresh crater about 6 meters (20 feet) in diameter holds an exposure of bright material, blue in this false-color image.
    Credit: NASA/JPL-Caltech/University of Arizona [Full Story]

    Searching for an oasis

    When Mariner 9 became the first craft to orbit another planet in 1971, the photographs it returned of dry river beds and canyons seemed to indicate that water had once existed on the Martian surface. Images from the Viking orbiters only strengthened the idea that many of the landforms may have been created by running water. Data from the Viking landers pointed to the presence of water beneath the surface, but the experiments were deemed inconclusive. [Mars Explored: Landers and Rovers Since 1971 (Infographic)]

    The early ’90s kicked off a slew of Mars missions. Scientists were flooded with a wealth of information about Mars. Three NASA orbiters and one sent by the European Space Agency studied the planet from above, mapping the surface and analyzing the minerals below. Some detected the presence of minerals, indicating the presence of water. Other data measured enough subsurface ice to fill Lake Michigan twice. They found evidence for the presence of hot springs on the surface and sustained precipitation at some areas. And they found patches of ice within some of the deeper craters.

    Impact craters offer a view of the interior of the red planet. Using the ESA’s Mars Express and NASA’s Mars Reconnaissance Orbiter, scientists were able to study rocks ejected from the planet’s interior, finding minerals that suggested the presence of water.

    “Water circulation occurred several kilometers deep in the crust some 3.7 billion years ago,” Nicolas Mangold, of the University of Nantes in France, said in a statement.

    But orbiters weren’t the only objects launched toward Mars. NASA’s Curiosity rover is the fifth robot to land on the surface of the Red Planet in the last 15 years. Pathfinder, Phoenix, Spirit and Opportunity all took detailed measurements of the planet; all but Phoenix traveled across the surface collecting a treasure trove of information.

    Phoenix Mars Lander Found Liquid Water, Some Scientists Think

    Images of one of Phoenix’s struts taken by the lander’s robotic arm camera on Sols (or Martian days) 8, 31 and 44 of th emission. The two spheroids enclosed by the circle appear to merge with each other, which some Phoenix scientists argue is a sign that the globs are liquid water.
    Credit: Renno, et al., NASA

    The probes dug into the ground, examining rocks and performing experiments. In 2008, Phoenix turned up small chunks of bright material that disappeared after four days, leading scientists to surmise that they were pieces of water ice. The lander went on to detect water vapor in a sample it collected and analyzed, confirming the presence of frozen water on the red planet.

    Spirit and Opportunity, the twin rovers, found traces of water enclosed in rock. In a shining example of a problem becoming a solution, a broken wheel on Spirit scraped into the top of the Martian surface, revealing a layer beneath rich in silica that had most likely formed in the presence of water.

    Curiosity has found yet more evidence of water flowing on ancient Mars. The 1-ton rover rolled through an ancient stream bed shortly after touching down in August 2012, and it has examined a number of rocks that were exposed to liquid water billions of years ago. 

    Mars missions aren’t the only way to search for water on Mars. Scientists studying rocks ejected from the Red Planet found signs that water lay beneath the surface in the past.

    “While robotic missions to Mars continue to shed light on the planet’s history, the only samples from Mars available for study on Earth are Martian meteorites,” lead author Lauren White, of the JPL, said in a statement.

    “On Earth, we can utilize multiple analytical techniques to take a more in-depth look at meteorites and shed light on the history of Mars.”

    Historical landforms

    In addition to examining the relatively recent (geologically speaking) presence of water, the various missions have also studied the surface of the planet in a historical context. The river beds of Mars don’t run wet today, but scientists can study them to learn more about the evolution of the planet. [Photos: The Search for Water on Mars]

    The flatter northern plains of Mars may once have hosted an ocean, or possibly, as the planet cycled through dry periods, two. The more recent body of water would likely have only been temporary, seeping into the ground, evaporating, or freezing in less than a million years, scientists say.

    Riverbeds and gullies indicate that water ran, at least briefly, across the surface of Mars. A hundred times more water may have flowed annually through a large channel system known as Marte Vallis than passes through the Mississippi River each year, according to estimates. The gullies themselves are smaller, likely forming during brief torrential rainstorms when fast-moving water could have carved them across the land.

    Curiosity found indications that at least one region of Mars, Mount Sharp, was built by sediments deposited in a lake bed millions of years ago, suggesting large pools existed on the planet for significant time periods.

    “If our hypothesis for Mount Sharp holds up, it challenges the notion that warm and wet conditions were transient, local, or only underground on Mars,” Curiosity deputy project scientist Ashwin Vasavada of NASA’s Jet Propulsion Laboratory (JPL) said in a statement.

    On Earth, the land around rivers and lakes is wetter, made up of mud and clays. Such deposits exist on Mars as well, trapping water and indicating where larger bodies may have once existed.

    Liquid gold

    Water may seem like a very common element to those of us stuck on Earth, but it has great value. In addition to understanding how Mars may have changed and developed over time, scientists hope that finding water will help them to find something even more valuable — life, either past or present.

    Only Earth is known to host life, and life on our planet requires water. Though life could conceivably evolve without relying on this precious liquid, scientists can only work with what they know. Thus they hope that locating water on celestial bodies such as Mars will lead to finding evidence for life.

    With this in mind, NASA developed a strategy for exploring the Red Planet that takes as its mantra “follow the water.” Recent orbiters, landers and rovers sent to Mars were designed to search for water, rather than life, in the hopes of finding environments where life could have thrived.

    That has changed, however, with the flood of evidence these robots have returned. Curiosity determined that Mars could indeed have supported microbial life in the ancient past, and the next NASA rover — a car-size robot based heavily on Curiosity’s basic design — will blast off in 2020 to look for evidence of past Red Planet life.

    Additional resources

    EDITOR’S RECOMMENDATIONS

  • Destination Pluto: NASA's New Horizons Mission in Pictures

    New Horizons space probe provides the highest resolution image of Pluto ever seen as presented in a NASA press conference on July 15, 2015, at the Johns Hopkins University Applied Physics Laboratory, Laurel, Maryland. This region near Pluto’s equator surprisingly contains a range of youthful mountains rising to heights of 11,000 feet (3,500 m) above the surface. [See a video of the flyby.]

  • Astronomers Discover Planetary Odd Couple

    Astronomers have discovered a pair of neighboring planets with dissimilar densities orbiting very close to each other.

  • Kuiper Belt Objects: Facts about the Kuiper Belt & KBOs

    This artist's impression shows the distant dwarf planet Eris in the distance with its moon Dysmonia in the foreground. New observations have shown that Eris is smaller than previously thought and almost exactly the same size as Pluto. Eris is extremely re
    This artist’s impression shows the distant dwarf planet Eris in the distance with its moon Dysmonia in the foreground. New observations have shown that Eris is smaller than previously thought and almost exactly the same size as Pluto. Eris is extremely reflective and its surface is probably covered in frost formed from the frozen remains of its atmosphere. Dysnomia appears to be a darker and less reflective body.
    Credit: ESO/L. Calçada

    Beyond the gas giant Neptune lies a region of space filled with icy bodies. Known as the Kuiper Belt, this chilly expanse holds trillions of objects, remnants of the early solar system. Dutch astronomer Jan Oort first proposed in 1950 that some comets might come from the the solar system’s far suburbs. That reservoir later became known as the Oort cloud. Earlier, in 1943, astronomer Kenneth Edgeworth had suggested comets and larger bodies might exist beyond Neptune. In 1951, astronomer Gerard Kuiper predicted the existence of a belt of icy objects that now bears his name. Some astronomers refer to it as the Edgeworth-Kuiper Belt.

    Astronomers are now hunting for a planet in the Kuiper Belt, a true ninth planet, after evidence of its existence was unveiled on Jan. 20, 2016. The so-called “Planet Nine,” as scientists are calling it, is about 10 times the mass of Earth and 5,000 times the mass of Pluto. 

    Let’s take a closer look at this distant section of the solar system and the small worlds most commonly known as Kupier Belt Objects (KBOs) and, in recent years, dwarf planets.

    Kuiper Belt Oort Cloud

    Artists rendering of the Kuiper Belt and Oort Cloud.
    Credit: NASA

    Kuiper Belt facts

    Haumea and its 2 Satellites

    Artist’s concept of the dwarf planet Haumea and its two satellites (Hi’iaka and Namaka).
    Credit: SINC/José Antonio Peñas

    The Kuiper Belt is an elliptical plane in space spanning from 30 to 50 times Earth’s distance from the sun, or 2.5 to 4.5 billion miles (4.5 to 7.4 billion kilometers). The belt is similar to the asteroid belt found between Mars and Jupiter, although the objects in the Kuiper Belt tend more to be icy rather than rocky.

    Scientists estimate that thousands of bodies more than 62 miles (100 km) in diameter travel around the sun within this belt, along with trillions of smaller objects, many of which are short-period comets. The region also contains several dwarf planets, round worlds too large to be considered asteroids and yet not qualifying as planets because they’re too small, on an odd orbit, and don’t clear out the space around them the way the 8 planets do.

    Kuiper Belt formation

    When the solar system formed, much of the gas, dust and rocks pulled together to form the sun and planets. The planets then swept most of the remaining debris into the sun or out of the solar system. But bodies farther out remained safe from gravitational tugs of planets like Jupiter, and so managed to stay safe as they slowly orbited the sun. The Kuiper Belt and its compatriot, the more distant and spherical Oort Cloud, contain the leftover remnants from the beginning of the solar system and can provide valuable insights into its birth.

    The classical Kuiper Belt — the most crowded section — lies between 42 and 48 times Earth’s distance from the sun. The orbit of objects in this region remain stable for the most part, although some objects occasionally have their course changed slightly when they drift too close to Neptune.

    Kuiper Belt Objects

    This artist’s impression shows the distant dwarf planet Eris. New observations have shown that Eris is smaller than previously thought and almost exactly the same size as Pluto. Eris is extremely reflective and its surface is probably covered in frost for

    This artist’s impression shows the distant dwarf planet Eris. New observations have shown that Eris is smaller than previously thought and almost exactly the same size as Pluto. Eris is extremely reflective and its surface is probably covered in frost formed from the frozen remains of its atmosphere. The distant Sun appears to the upper right and both Eris and its moon Dysnomia (center) appear as crescents.
    Credit: ESO/L. Calçada

    Pluto was the first true Kuiper Belt Object to be seen, although scientists at the time didn’t recognize it as such. The existence of the belt wasn’t realized until scientists discovered a slow moving, small world in the outer solar system in 1992 (David Jewitt and Jane Luu found the KBO, 1992QB1.). Other objects soon followed, and astronomers quickly saw that the region beyond Neptune teemed with icy rocks and tiny worlds.

    Sedna (sed’nah), about three-fourths the size of Pluto, was discovered in 2004. It is so far out from the sun it takes about 10,500 years to make a single orbit. Sedna is about 1,100 miles (1,770 km) wide and circles the sun on an eccentric orbit that ranges between 8 billion miles (12.9 billion km) and 84 billion miles (135 billion km).

    In July 2005, astronomers announced the discovery of an object in the Kuiper Belt thought to be larger than Pluto, though subsequent observations revealed it was slightly smaller. Known as Eris, it orbits the sun approximately once every 580 years, traveling almost one hundred times farther from the sun than Earth does. Eris’ discovery revealed to some astronomers the problem of terming Pluto a full-scale planet, and in 2006, Pluto, Eris, and the largest asteroid Ceres were reclassified as dwarf planets. Two more dwarf planets, Haumea and Makemake, were discovered in the Kuiper Belt in 2008.

    Planet Nine

    Planet Nine orbits the sun at a distance that is 20 times farther out than the orbit of Neptune. (The orbit of Neptune is 2.7 billion miles from the sun at its closest point.)  The strange world’s orbit is about 600 times farther from the sun than the Earth’s orbit is from the star.

    [The Evidence for ‘Planet Nine’ in Our Solar System (Gallery)]

    Scientists have not actually seen Planet Nine directly. Its existence was inferred by its gravitational effects on other objects in the Kuiper Belt.

    [‘Planet Nine’: Facts About the Mysterious Solar System World (Infographic)]

    Scientists Mike Brown and Konstantin Batygin at the California Institute of Technology in Pasadena described the evidence for Planet Nine in a study published in the Astronomical Journal. The research is based on mathematical models and computer simulations using observations of six other smaller Kuiper Belt Objects with orbits that aligned in a similar matter.

    Exploration

    Because of their small size and distant location, Kuiper Belt Objects are a challenge to spot from Earth. Infrared measurements from NASA’s space-based telescope, Spitzer, have helped to nail down sizes for the largest objects.

    In order to catch a better glimpse of these remote leftovers from the birth of the solar system, NASA launched the New Horizons mission. The spacecraft reached Pluto in 2015 and continued on with an aim to examine multiple KBOs.

    See more about Discoveries and Discoverers of KBOs & Dwarf Planets.

    Kuiper Belt

    The Kuiper Belt is shown beyond the orbit of Neptune. One of its inhabitants is Eris, on a highly tilted and elipical orbit.
    Credit: NASA

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