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Mars Reconnaissance Orbiter …
Title Mars Reconnaissance Orbiter Aerobraking
Description December 10, 2003 NASA's Mars Reconnaissance Orbiter dips into the thin martian atmosphere to adjust its orbit in this artist's concept illustration. NASA plans to launch this multipurpose spacecraft in August 2005 for arrival at Mars in March 2006. The plans call for controlled use of atmospheric friction in a process called aerobraking for about six months after arrival to change the initial, very elongated orbit into a rounder shape optimal for science operations. Mars Reconnaissance Orbiter is designed to advance our understanding of Mars through detailed observation, to examine potential landing sites for future surface missions and to provide a high-data-rate communications relay for those missions. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Reconnaissance Orbiter Project for the NASA Office of Space Science, Washington. JPL's main industrial partner in the project, Lockheed Martin Space Systems, Denver, Colo., is building the spacecraft.
Date 12.10.2003
Mars Reconnaissance Orbiter …
Title Mars Reconnaissance Orbiter over Nilosyrtis
Description December 10, 2003 NASA's Mars Reconnaissance Orbiter passes above a portion of the planet called Nilosyrtis Mensae in this artist's concept illustration. NASA plans to launch this multipurpose spacecraft in August 2005 to advance our understanding of Mars through detailed observation, to examine potential landing sites for future surface missions and to provide a high-data-rate communications relay for those missions. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Reconnaissance Orbiter Project for the NASA Office of Space Science, Washington. JPL's main industrial partner in the project, Lockheed Martin Space Systems, Denver, Colo., is building the spacecraft.
Date 12.10.2003
Mars Reconnaissance Orbiter …
Title Mars Reconnaissance Orbiter over Pole
Description December 10, 2003 NASA's Mars Reconnaissance Orbiter passes over the planet's south polar region in this artist's concept illustration. NASA plans to launch this multipurpose spacecraft in August 2005 to advance our understanding of Mars through detailed observation, to examine potential landing sites for future surface missions and to provide a high-data-rate communications relay for those missions. The orbiter's shallow radar experiment, one of six science instruments on board, is designed to probe the internal structure of Mars' polar ice caps, as well as to gather information planet-wide about underground layers of ice, rock and, perhaps, liquid water that might be accessible from the surface. Phobos, one of Mars' two moons, appears in the upper left corner of the illustration NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Reconnaissance Orbiter Project for the NASA Office of Space Science, Washington. JPL's main industrial partner in the project, Lockheed Martin Space Systems, Denver, Colo., is building the spacecraft. The Italian Space Agency is providing the radar instrument.
Date 12.10.2003
Moriba Jah Awaits Navigation …
title Moriba Jah Awaits Navigation Information
Description Forty minutes after launch, the navigation team hits full throttle, locating the exact trajectory of the Mars Reconnaissance Orbiter. Moriba Jah awaits the most updated information from the Goldstone, California Deep Space Network tracking station while in the Navigation Operations room at Jet Propulsion Laboratory on August 12, 2005. Credit: NASA/JPL
Flight Engineering Team Memb …
title Flight Engineering Team Members Enjoy the Launch
Description For over five years, Flight Engineering Team members have dedicated tireless hours to creating the Mars Reconnaissance Orbiter. On August 12, 2005, Kyle Martin, Peter Xaypraseuth, and David Skulsky take five minutes to experience the thrill of watching their spacecraft launch from Kennedy Space Center in Florida via TV screens in the Mission Support Area at JPL in California. Credit: NASA/JPL
Mars Reconnaissance Orbiter …
title Mars Reconnaissance Orbiter Taking Shape
Description Lockheed Martin Space Systems engineer Terry Kampmann (left) and lead technician Jack Farmerie work on assembly and test of NASA's Mars Reconnaissance Orbiter spacecraft bus in a cleanroom at the company's Denver facility. In coming months, the orbiter's science instruments will be integrated and tested, followed by environmental testing of the completed spacecraft. Launch of Mars Reconnaissance Orbiter is scheduled for August 2005. The Mars Reconnaissance Orbiter project is managed for the NASA Science Mission Directorate, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, is prime contractor for the project. Credit: NASA/JPL/Lockheed Martin/Pat Corkery
Mars Reconnaissance Orbiter …
PIA04918
Title Mars Reconnaissance Orbiter over Pole
Original Caption Released with Image December 10, 2003 NASA's Mars Reconnaissance Orbiter passes over the planet's south polar region in this artist's concept illustration. NASA plans to launch this multipurpose spacecraft in August 2005 to advance our understanding of Mars through detailed observation, to examine potential landing sites for future surface missions and to provide a high-data-rate communications relay for those missions. The orbiter's shallow radar experiment, one of six science instruments on board, is designed to probe the internal structure of Mars' polar ice caps, as well as to gather information planet-wide about underground layers of ice, rock and, perhaps, liquid water that might be accessible from the surface. Phobos, one of Mars' two moons, appears in the upper left corner of the illustration NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Reconnaissance Orbiter Project for the NASA Office of Space Science, Washington. JPL's main industrial partner in the project, Lockheed Martin Space Systems, Denver, Colo., is building the spacecraft. The Italian Space Agency is providing the radar instrument.
Mars Reconnaissance Orbiter …
PIA04916
Title Mars Reconnaissance Orbiter over Nilosyrtis
Original Caption Released with Image December 10, 2003 NASA's Mars Reconnaissance Orbiter passes above a portion of the planet called Nilosyrtis Mensae in this artist's concept illustration. NASA plans to launch this multipurpose spacecraft in August 2005 to advance our understanding of Mars through detailed observation, to examine potential landing sites for future surface missions and to provide a high-data-rate communications relay for those missions. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Reconnaissance Orbiter Project for the NASA Office of Space Science, Washington. JPL's main industrial partner in the project, Lockheed Martin Space Systems, Denver, Colo., is building the spacecraft.
Mars Reconnaissance Orbiter …
PIA04917
Title Mars Reconnaissance Orbiter Aerobraking
Original Caption Released with Image December 10, 2003 NASA's Mars Reconnaissance Orbiter dips into the thin martian atmosphere to adjust its orbit in this artist's concept illustration. NASA plans to launch this multipurpose spacecraft in August 2005 for arrival at Mars in March 2006. The plans call for controlled use of atmospheric friction in a process called aerobraking for about six months after arrival to change the initial, very elongated orbit into a rounder shape optimal for science operations. Mars Reconnaissance Orbiter is designed to advance our understanding of Mars through detailed observation, to examine potential landing sites for future surface missions and to provide a high-data-rate communications relay for those missions. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Reconnaissance Orbiter Project for the NASA Office of Space Science, Washington. JPL's main industrial partner in the project, Lockheed Martin Space Systems, Denver, Colo., is building the spacecraft.
Mars Reconnaissance Orbiter …
PIA06756
Title Mars Reconnaissance Orbiter Taking Shape
Original Caption Released with Image Lockheed Martin Space Systems engineer Terry Kampmann (left) and lead technician Jack Farmerie work on assembly and test of NASA's Mars Reconnaissance Orbiter spacecraft bus in a cleanroom at the company's Denver facility. In coming months, the orbiter's science instruments will be integrated and tested, followed by environmental testing of the completed spacecraft. Launch of Mars Reconnaissance Orbiter is scheduled for August 2005. The Mars Reconnaissance Orbiter project is managed for the NASA Science Mission Directorate, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, is prime contractor for the project.
New Impact Crater in Arabia …
PIA09022
Sol (our sun)
Mars Orbiter Camera
Title New Impact Crater in Arabia Terra
Original Caption Released with Image http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ]., The images of new martian impact craters reveal many details about the impact event that result from the manner in which the impact process interacted with the dusty surface and thin planetary atmosphere, these data are sure to keep scientists busy for years. Of the 20 new impact craters found on Mars by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 2006, the one shown here is perhaps the prettiest. The darkened "blast zone" around the crater exhibits considerable details about how the energy transferred from the impact to the surrounding atmosphere and dust-mantled surface interacted. Wispy dark rays and dark, annular (nearly-circular) zones surround the crater, while several chains of dark spots formed by secondary impact radiate away for hundreds of meters from the tiny crater. This impact site has a single crater of about 22.6 ± 1.7 meters (about 75 feet) in diameter. Compare this with the typical 100 yard U.S.-style football field: 75 feet is about 24.7 yards. The crater is located in Arabia Terra near 26.4°N, 336.5°W. This picture is a colorized view of the crater. The image is a sub-frame of MOC narrow angle camera image S16-01674, obtained on 20 March 2006. The color comes from a look-up table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Stereo Camera (HRSC) [ http://berlinadmin.dlr.de/Missions/express/indexeng.shtml ]. Figures A and B: These pictures are grayscale composites of portions of MOC images S16-01674, S17-00795, S17-02191, and S18-01407, showing the impact site and the extensive rays developed during the impact event. These data were acquired during March, April, and May 2006. Figure C: This picture shows how the age of the crater was constrained. The first (left) is a portion of MOC red wide angle camera image R12-00786, acquired on 8 December 2003. The white circle indicates the location of the impact site, but the impact had not yet occurred. The second picture (right) shows the same MOC red wide angle image, overlain by a portion of an image from the Mars Odyssey Thermal Emission Imaging System (THEMIS) [ http://themis.asu.edu/ ]. The THEMIS image is an infrared picture (I17523014, band 9, ~12.6 micrometers) acquired on 26 November 2005. In the infrared image, the impact site shows up as a bright spot because it is warmer than its surroundings during the day. These two pictures, thus, tell us that the impact occurred some time between 8 December 2003 and 26 November 2005. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see
New Impact Crater in Arabia …
PIA09022
Sol (our sun)
Mars Orbiter Camera
Title New Impact Crater in Arabia Terra
Original Caption Released with Image http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ]., The images of new martian impact craters reveal many details about the impact event that result from the manner in which the impact process interacted with the dusty surface and thin planetary atmosphere, these data are sure to keep scientists busy for years. Of the 20 new impact craters found on Mars by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 2006, the one shown here is perhaps the prettiest. The darkened "blast zone" around the crater exhibits considerable details about how the energy transferred from the impact to the surrounding atmosphere and dust-mantled surface interacted. Wispy dark rays and dark, annular (nearly-circular) zones surround the crater, while several chains of dark spots formed by secondary impact radiate away for hundreds of meters from the tiny crater. This impact site has a single crater of about 22.6 ± 1.7 meters (about 75 feet) in diameter. Compare this with the typical 100 yard U.S.-style football field: 75 feet is about 24.7 yards. The crater is located in Arabia Terra near 26.4°N, 336.5°W. This picture is a colorized view of the crater. The image is a sub-frame of MOC narrow angle camera image S16-01674, obtained on 20 March 2006. The color comes from a look-up table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Stereo Camera (HRSC) [ http://berlinadmin.dlr.de/Missions/express/indexeng.shtml ]. Figures A and B: These pictures are grayscale composites of portions of MOC images S16-01674, S17-00795, S17-02191, and S18-01407, showing the impact site and the extensive rays developed during the impact event. These data were acquired during March, April, and May 2006. Figure C: This picture shows how the age of the crater was constrained. The first (left) is a portion of MOC red wide angle camera image R12-00786, acquired on 8 December 2003. The white circle indicates the location of the impact site, but the impact had not yet occurred. The second picture (right) shows the same MOC red wide angle image, overlain by a portion of an image from the Mars Odyssey Thermal Emission Imaging System (THEMIS) [ http://themis.asu.edu/ ]. The THEMIS image is an infrared picture (I17523014, band 9, ~12.6 micrometers) acquired on 26 November 2005. In the infrared image, the impact site shows up as a bright spot because it is warmer than its surroundings during the day. These two pictures, thus, tell us that the impact occurred some time between 8 December 2003 and 26 November 2005. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see
New Impact Crater in Arabia …
PIA09022
Sol (our sun)
Mars Orbiter Camera
Title New Impact Crater in Arabia Terra
Original Caption Released with Image http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ]., The images of new martian impact craters reveal many details about the impact event that result from the manner in which the impact process interacted with the dusty surface and thin planetary atmosphere, these data are sure to keep scientists busy for years. Of the 20 new impact craters found on Mars by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 2006, the one shown here is perhaps the prettiest. The darkened "blast zone" around the crater exhibits considerable details about how the energy transferred from the impact to the surrounding atmosphere and dust-mantled surface interacted. Wispy dark rays and dark, annular (nearly-circular) zones surround the crater, while several chains of dark spots formed by secondary impact radiate away for hundreds of meters from the tiny crater. This impact site has a single crater of about 22.6 ± 1.7 meters (about 75 feet) in diameter. Compare this with the typical 100 yard U.S.-style football field: 75 feet is about 24.7 yards. The crater is located in Arabia Terra near 26.4°N, 336.5°W. This picture is a colorized view of the crater. The image is a sub-frame of MOC narrow angle camera image S16-01674, obtained on 20 March 2006. The color comes from a look-up table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Stereo Camera (HRSC) [ http://berlinadmin.dlr.de/Missions/express/indexeng.shtml ]. Figures A and B: These pictures are grayscale composites of portions of MOC images S16-01674, S17-00795, S17-02191, and S18-01407, showing the impact site and the extensive rays developed during the impact event. These data were acquired during March, April, and May 2006. Figure C: This picture shows how the age of the crater was constrained. The first (left) is a portion of MOC red wide angle camera image R12-00786, acquired on 8 December 2003. The white circle indicates the location of the impact site, but the impact had not yet occurred. The second picture (right) shows the same MOC red wide angle image, overlain by a portion of an image from the Mars Odyssey Thermal Emission Imaging System (THEMIS) [ http://themis.asu.edu/ ]. The THEMIS image is an infrared picture (I17523014, band 9, ~12.6 micrometers) acquired on 26 November 2005. In the infrared image, the impact site shows up as a bright spot because it is warmer than its surroundings during the day. These two pictures, thus, tell us that the impact occurred some time between 8 December 2003 and 26 November 2005. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see
New Impact Crater in Arabia …
PIA09022
Sol (our sun)
Mars Orbiter Camera
Title New Impact Crater in Arabia Terra
Original Caption Released with Image http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ]., The images of new martian impact craters reveal many details about the impact event that result from the manner in which the impact process interacted with the dusty surface and thin planetary atmosphere, these data are sure to keep scientists busy for years. Of the 20 new impact craters found on Mars by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 2006, the one shown here is perhaps the prettiest. The darkened "blast zone" around the crater exhibits considerable details about how the energy transferred from the impact to the surrounding atmosphere and dust-mantled surface interacted. Wispy dark rays and dark, annular (nearly-circular) zones surround the crater, while several chains of dark spots formed by secondary impact radiate away for hundreds of meters from the tiny crater. This impact site has a single crater of about 22.6 ± 1.7 meters (about 75 feet) in diameter. Compare this with the typical 100 yard U.S.-style football field: 75 feet is about 24.7 yards. The crater is located in Arabia Terra near 26.4°N, 336.5°W. This picture is a colorized view of the crater. The image is a sub-frame of MOC narrow angle camera image S16-01674, obtained on 20 March 2006. The color comes from a look-up table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Stereo Camera (HRSC) [ http://berlinadmin.dlr.de/Missions/express/indexeng.shtml ]. Figures A and B: These pictures are grayscale composites of portions of MOC images S16-01674, S17-00795, S17-02191, and S18-01407, showing the impact site and the extensive rays developed during the impact event. These data were acquired during March, April, and May 2006. Figure C: This picture shows how the age of the crater was constrained. The first (left) is a portion of MOC red wide angle camera image R12-00786, acquired on 8 December 2003. The white circle indicates the location of the impact site, but the impact had not yet occurred. The second picture (right) shows the same MOC red wide angle image, overlain by a portion of an image from the Mars Odyssey Thermal Emission Imaging System (THEMIS) [ http://themis.asu.edu/ ]. The THEMIS image is an infrared picture (I17523014, band 9, ~12.6 micrometers) acquired on 26 November 2005. In the infrared image, the impact site shows up as a bright spot because it is warmer than its surroundings during the day. These two pictures, thus, tell us that the impact occurred some time between 8 December 2003 and 26 November 2005. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see
New Impact Crater in Arabia …
PIA09022
Sol (our sun)
Mars Orbiter Camera
Title New Impact Crater in Arabia Terra
Original Caption Released with Image http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ]., The images of new martian impact craters reveal many details about the impact event that result from the manner in which the impact process interacted with the dusty surface and thin planetary atmosphere, these data are sure to keep scientists busy for years. Of the 20 new impact craters found on Mars by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 2006, the one shown here is perhaps the prettiest. The darkened "blast zone" around the crater exhibits considerable details about how the energy transferred from the impact to the surrounding atmosphere and dust-mantled surface interacted. Wispy dark rays and dark, annular (nearly-circular) zones surround the crater, while several chains of dark spots formed by secondary impact radiate away for hundreds of meters from the tiny crater. This impact site has a single crater of about 22.6 ± 1.7 meters (about 75 feet) in diameter. Compare this with the typical 100 yard U.S.-style football field: 75 feet is about 24.7 yards. The crater is located in Arabia Terra near 26.4°N, 336.5°W. This picture is a colorized view of the crater. The image is a sub-frame of MOC narrow angle camera image S16-01674, obtained on 20 March 2006. The color comes from a look-up table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Stereo Camera (HRSC) [ http://berlinadmin.dlr.de/Missions/express/indexeng.shtml ]. Figures A and B: These pictures are grayscale composites of portions of MOC images S16-01674, S17-00795, S17-02191, and S18-01407, showing the impact site and the extensive rays developed during the impact event. These data were acquired during March, April, and May 2006. Figure C: This picture shows how the age of the crater was constrained. The first (left) is a portion of MOC red wide angle camera image R12-00786, acquired on 8 December 2003. The white circle indicates the location of the impact site, but the impact had not yet occurred. The second picture (right) shows the same MOC red wide angle image, overlain by a portion of an image from the Mars Odyssey Thermal Emission Imaging System (THEMIS) [ http://themis.asu.edu/ ]. The THEMIS image is an infrared picture (I17523014, band 9, ~12.6 micrometers) acquired on 26 November 2005. In the infrared image, the impact site shows up as a bright spot because it is warmer than its surroundings during the day. These two pictures, thus, tell us that the impact occurred some time between 8 December 2003 and 26 November 2005. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see
New Impact Crater in Arabia …
PIA09022
Sol (our sun)
Mars Orbiter Camera
Title New Impact Crater in Arabia Terra
Original Caption Released with Image http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ]., The images of new martian impact craters reveal many details about the impact event that result from the manner in which the impact process interacted with the dusty surface and thin planetary atmosphere, these data are sure to keep scientists busy for years. Of the 20 new impact craters found on Mars by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) in 2006, the one shown here is perhaps the prettiest. The darkened "blast zone" around the crater exhibits considerable details about how the energy transferred from the impact to the surrounding atmosphere and dust-mantled surface interacted. Wispy dark rays and dark, annular (nearly-circular) zones surround the crater, while several chains of dark spots formed by secondary impact radiate away for hundreds of meters from the tiny crater. This impact site has a single crater of about 22.6 ± 1.7 meters (about 75 feet) in diameter. Compare this with the typical 100 yard U.S.-style football field: 75 feet is about 24.7 yards. The crater is located in Arabia Terra near 26.4°N, 336.5°W. This picture is a colorized view of the crater. The image is a sub-frame of MOC narrow angle camera image S16-01674, obtained on 20 March 2006. The color comes from a look-up table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Stereo Camera (HRSC) [ http://berlinadmin.dlr.de/Missions/express/indexeng.shtml ]. Figures A and B: These pictures are grayscale composites of portions of MOC images S16-01674, S17-00795, S17-02191, and S18-01407, showing the impact site and the extensive rays developed during the impact event. These data were acquired during March, April, and May 2006. Figure C: This picture shows how the age of the crater was constrained. The first (left) is a portion of MOC red wide angle camera image R12-00786, acquired on 8 December 2003. The white circle indicates the location of the impact site, but the impact had not yet occurred. The second picture (right) shows the same MOC red wide angle image, overlain by a portion of an image from the Mars Odyssey Thermal Emission Imaging System (THEMIS) [ http://themis.asu.edu/ ]. The THEMIS image is an infrared picture (I17523014, band 9, ~12.6 micrometers) acquired on 26 November 2005. In the infrared image, the impact site shows up as a bright spot because it is warmer than its surroundings during the day. These two pictures, thus, tell us that the impact occurred some time between 8 December 2003 and 26 November 2005. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by the Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see
New Gully Deposit in a Crate …
PIA09028
Sol (our sun)
Mars Orbiter Camera
Title New Gully Deposit in a Crater in the Centauri Montes Region
Original Caption Released with Image ). The second case, in an unnamed crater in the Centauri Montes region, east of the Hellas Basin, is described here. Gullies were first described by Mars Orbiter Camera scientists in June 2000, and many examples were presented in our June 2000 web releases and in a paper published in the journal Science. Additional examples of these middle and high-latitude landforms can be seen among the other more than 1,600 web releases. The new gully deposit in an unnamed crater in the Centauri Montes region is located near 38.7 degrees south latitude, 263.3 degrees west longitude. Like the new gully deposit in Terra Sirenum, this one has a light tone relative to its surroundings. It is on an equator-facing slope on which numerous narrow gully channels occur. As this slope is always in sunlight during the afternoons when Mars Global Surveyor passes overhead, the gullies always appear somewhat "washed out," just as craters on a full Moon do when viewed from Earth with a telescope. The new, light-toned flow was first noticed by the Mars Orbiter Camera science operations team in an image acquired on Sept. 10, 2005. Re-examination of other images of this crater showed that the new deposit had actually been present on Feb. 21, 2004, when the distal (down-slope) end of the deposit was captured in other images. In February 2004, the deposit had gone unnoticed because only a small portion of it was imaged. This location was first imaged by the Mars Orbiter Camera on Aug. 30, 1999. The deposit was not present at that time. Thus, it formed between Aug. 30, 1999 and Feb. 21, 2004. Roughly 20 percent brighter than the surface as it appeared before the flow occurred, the new deposit exhibits characteristics consistent with transport and deposition of a fluid that behaved like liquid water and likely transported some fine-grained sediment along with it. The distal end of the flow broke into several branches, or digits, and the material diverted and flowed around low obstacles. As with the example in Terra Sirenum, the depth of the flow is too thin to be measured in 1.5-meter-per-pixel (1.7-yard-per-pixel) images, so a very small volume of liquid and sediment was involved. While the material flowed and easily budded into several branches, it also must have moved slow enough to not topple over some of the low obstacles in its path. This picture is a colorized view of the light-toned gully deposit, draped over a topographic image derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment. Figure A: This figure shows the southeast wall of the unnamed crater in the Centauri Montes region, as it appeared in August 1999, and later in September 2005. No light-toned deposit was present in August 1999, but appeared by February 2004. The 300-meter scale bar represents 328 yards. Figure B: The second figure is a, Two Martian southern mid-latitude craters have new light-toned deposits that formed in gully settings during the course of the Mars Global Surveyor mission. Images from the Mars Orbiter Camera documented one case in an unnamed crater in Terra Sirenum, described in an accompanying release (see PIA09027 [ http://photojournal.jpl.nasa.gov/catalog/PIA09027 ] or MOC2-1618 [ http://www.msss.com/mars_images/moc/2006/12/06/gullies/sirenum_crater/index.html ], mosaic of several Mars Global Surveyor images, colorized using a table derived from Mars Reconnaissance Orbiter camera color data and overlain on a sub-frame of a Mars Odyssey Thermal Emission Imaging System image. The 1-kilometer scale bar represents about 0.62 miles. Figure C: The third figure is a colorized view of the light-toned gully deposit as viewed from an oblique perspective, draped over topography derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter camera. The new light-toned flow, by itself, does not prove that liquid water was involved in its genesis. However, this observation and the similar light-toned flow in Terra Sirenum together show that some gully sites are indeed changing today, providing tantalizing evidence there might be sources of liquid water beneath the surface of Mars right now. In both cases, these new flows may be indicating the locations of aquifers (subsurface rocks saturated with water) that could be detected by orbiting, ground-penetrating radar systems such as the Mars Express Mars Advanced Radar for Subsurface and Ionosphere Sounding or the Mars Reconnaissance Orbiter's Mars Shallow Subsurface Radar. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by NASA's Jet Propulsion Laboratory, Pasadena, Calif., a division of the California Institute of Technology, also in Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ].
New Gully Deposit in a Crate …
PIA09028
Sol (our sun)
Mars Orbiter Camera
Title New Gully Deposit in a Crater in the Centauri Montes Region
Original Caption Released with Image ). The second case, in an unnamed crater in the Centauri Montes region, east of the Hellas Basin, is described here. Gullies were first described by Mars Orbiter Camera scientists in June 2000, and many examples were presented in our June 2000 web releases and in a paper published in the journal Science. Additional examples of these middle and high-latitude landforms can be seen among the other more than 1,600 web releases. The new gully deposit in an unnamed crater in the Centauri Montes region is located near 38.7 degrees south latitude, 263.3 degrees west longitude. Like the new gully deposit in Terra Sirenum, this one has a light tone relative to its surroundings. It is on an equator-facing slope on which numerous narrow gully channels occur. As this slope is always in sunlight during the afternoons when Mars Global Surveyor passes overhead, the gullies always appear somewhat "washed out," just as craters on a full Moon do when viewed from Earth with a telescope. The new, light-toned flow was first noticed by the Mars Orbiter Camera science operations team in an image acquired on Sept. 10, 2005. Re-examination of other images of this crater showed that the new deposit had actually been present on Feb. 21, 2004, when the distal (down-slope) end of the deposit was captured in other images. In February 2004, the deposit had gone unnoticed because only a small portion of it was imaged. This location was first imaged by the Mars Orbiter Camera on Aug. 30, 1999. The deposit was not present at that time. Thus, it formed between Aug. 30, 1999 and Feb. 21, 2004. Roughly 20 percent brighter than the surface as it appeared before the flow occurred, the new deposit exhibits characteristics consistent with transport and deposition of a fluid that behaved like liquid water and likely transported some fine-grained sediment along with it. The distal end of the flow broke into several branches, or digits, and the material diverted and flowed around low obstacles. As with the example in Terra Sirenum, the depth of the flow is too thin to be measured in 1.5-meter-per-pixel (1.7-yard-per-pixel) images, so a very small volume of liquid and sediment was involved. While the material flowed and easily budded into several branches, it also must have moved slow enough to not topple over some of the low obstacles in its path. This picture is a colorized view of the light-toned gully deposit, draped over a topographic image derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment. Figure A: This figure shows the southeast wall of the unnamed crater in the Centauri Montes region, as it appeared in August 1999, and later in September 2005. No light-toned deposit was present in August 1999, but appeared by February 2004. The 300-meter scale bar represents 328 yards. Figure B: The second figure is a, Two Martian southern mid-latitude craters have new light-toned deposits that formed in gully settings during the course of the Mars Global Surveyor mission. Images from the Mars Orbiter Camera documented one case in an unnamed crater in Terra Sirenum, described in an accompanying release (see PIA09027 [ http://photojournal.jpl.nasa.gov/catalog/PIA09027 ] or MOC2-1618 [ http://www.msss.com/mars_images/moc/2006/12/06/gullies/sirenum_crater/index.html ], mosaic of several Mars Global Surveyor images, colorized using a table derived from Mars Reconnaissance Orbiter camera color data and overlain on a sub-frame of a Mars Odyssey Thermal Emission Imaging System image. The 1-kilometer scale bar represents about 0.62 miles. Figure C: The third figure is a colorized view of the light-toned gully deposit as viewed from an oblique perspective, draped over topography derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter camera. The new light-toned flow, by itself, does not prove that liquid water was involved in its genesis. However, this observation and the similar light-toned flow in Terra Sirenum together show that some gully sites are indeed changing today, providing tantalizing evidence there might be sources of liquid water beneath the surface of Mars right now. In both cases, these new flows may be indicating the locations of aquifers (subsurface rocks saturated with water) that could be detected by orbiting, ground-penetrating radar systems such as the Mars Express Mars Advanced Radar for Subsurface and Ionosphere Sounding or the Mars Reconnaissance Orbiter's Mars Shallow Subsurface Radar. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by NASA's Jet Propulsion Laboratory, Pasadena, Calif., a division of the California Institute of Technology, also in Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ].
New Gully Deposit in a Crate …
PIA09028
Sol (our sun)
Mars Orbiter Camera
Title New Gully Deposit in a Crater in the Centauri Montes Region
Original Caption Released with Image ). The second case, in an unnamed crater in the Centauri Montes region, east of the Hellas Basin, is described here. Gullies were first described by Mars Orbiter Camera scientists in June 2000, and many examples were presented in our June 2000 web releases and in a paper published in the journal Science. Additional examples of these middle and high-latitude landforms can be seen among the other more than 1,600 web releases. The new gully deposit in an unnamed crater in the Centauri Montes region is located near 38.7 degrees south latitude, 263.3 degrees west longitude. Like the new gully deposit in Terra Sirenum, this one has a light tone relative to its surroundings. It is on an equator-facing slope on which numerous narrow gully channels occur. As this slope is always in sunlight during the afternoons when Mars Global Surveyor passes overhead, the gullies always appear somewhat "washed out," just as craters on a full Moon do when viewed from Earth with a telescope. The new, light-toned flow was first noticed by the Mars Orbiter Camera science operations team in an image acquired on Sept. 10, 2005. Re-examination of other images of this crater showed that the new deposit had actually been present on Feb. 21, 2004, when the distal (down-slope) end of the deposit was captured in other images. In February 2004, the deposit had gone unnoticed because only a small portion of it was imaged. This location was first imaged by the Mars Orbiter Camera on Aug. 30, 1999. The deposit was not present at that time. Thus, it formed between Aug. 30, 1999 and Feb. 21, 2004. Roughly 20 percent brighter than the surface as it appeared before the flow occurred, the new deposit exhibits characteristics consistent with transport and deposition of a fluid that behaved like liquid water and likely transported some fine-grained sediment along with it. The distal end of the flow broke into several branches, or digits, and the material diverted and flowed around low obstacles. As with the example in Terra Sirenum, the depth of the flow is too thin to be measured in 1.5-meter-per-pixel (1.7-yard-per-pixel) images, so a very small volume of liquid and sediment was involved. While the material flowed and easily budded into several branches, it also must have moved slow enough to not topple over some of the low obstacles in its path. This picture is a colorized view of the light-toned gully deposit, draped over a topographic image derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment. Figure A: This figure shows the southeast wall of the unnamed crater in the Centauri Montes region, as it appeared in August 1999, and later in September 2005. No light-toned deposit was present in August 1999, but appeared by February 2004. The 300-meter scale bar represents 328 yards. Figure B: The second figure is a, Two Martian southern mid-latitude craters have new light-toned deposits that formed in gully settings during the course of the Mars Global Surveyor mission. Images from the Mars Orbiter Camera documented one case in an unnamed crater in Terra Sirenum, described in an accompanying release (see PIA09027 [ http://photojournal.jpl.nasa.gov/catalog/PIA09027 ] or MOC2-1618 [ http://www.msss.com/mars_images/moc/2006/12/06/gullies/sirenum_crater/index.html ], mosaic of several Mars Global Surveyor images, colorized using a table derived from Mars Reconnaissance Orbiter camera color data and overlain on a sub-frame of a Mars Odyssey Thermal Emission Imaging System image. The 1-kilometer scale bar represents about 0.62 miles. Figure C: The third figure is a colorized view of the light-toned gully deposit as viewed from an oblique perspective, draped over topography derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter camera. The new light-toned flow, by itself, does not prove that liquid water was involved in its genesis. However, this observation and the similar light-toned flow in Terra Sirenum together show that some gully sites are indeed changing today, providing tantalizing evidence there might be sources of liquid water beneath the surface of Mars right now. In both cases, these new flows may be indicating the locations of aquifers (subsurface rocks saturated with water) that could be detected by orbiting, ground-penetrating radar systems such as the Mars Express Mars Advanced Radar for Subsurface and Ionosphere Sounding or the Mars Reconnaissance Orbiter's Mars Shallow Subsurface Radar. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by NASA's Jet Propulsion Laboratory, Pasadena, Calif., a division of the California Institute of Technology, also in Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ].
New Gully Deposit in a Crate …
PIA09028
Sol (our sun)
Mars Orbiter Camera
Title New Gully Deposit in a Crater in the Centauri Montes Region
Original Caption Released with Image ). The second case, in an unnamed crater in the Centauri Montes region, east of the Hellas Basin, is described here. Gullies were first described by Mars Orbiter Camera scientists in June 2000, and many examples were presented in our June 2000 web releases and in a paper published in the journal Science. Additional examples of these middle and high-latitude landforms can be seen among the other more than 1,600 web releases. The new gully deposit in an unnamed crater in the Centauri Montes region is located near 38.7 degrees south latitude, 263.3 degrees west longitude. Like the new gully deposit in Terra Sirenum, this one has a light tone relative to its surroundings. It is on an equator-facing slope on which numerous narrow gully channels occur. As this slope is always in sunlight during the afternoons when Mars Global Surveyor passes overhead, the gullies always appear somewhat "washed out," just as craters on a full Moon do when viewed from Earth with a telescope. The new, light-toned flow was first noticed by the Mars Orbiter Camera science operations team in an image acquired on Sept. 10, 2005. Re-examination of other images of this crater showed that the new deposit had actually been present on Feb. 21, 2004, when the distal (down-slope) end of the deposit was captured in other images. In February 2004, the deposit had gone unnoticed because only a small portion of it was imaged. This location was first imaged by the Mars Orbiter Camera on Aug. 30, 1999. The deposit was not present at that time. Thus, it formed between Aug. 30, 1999 and Feb. 21, 2004. Roughly 20 percent brighter than the surface as it appeared before the flow occurred, the new deposit exhibits characteristics consistent with transport and deposition of a fluid that behaved like liquid water and likely transported some fine-grained sediment along with it. The distal end of the flow broke into several branches, or digits, and the material diverted and flowed around low obstacles. As with the example in Terra Sirenum, the depth of the flow is too thin to be measured in 1.5-meter-per-pixel (1.7-yard-per-pixel) images, so a very small volume of liquid and sediment was involved. While the material flowed and easily budded into several branches, it also must have moved slow enough to not topple over some of the low obstacles in its path. This picture is a colorized view of the light-toned gully deposit, draped over a topographic image derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment. Figure A: This figure shows the southeast wall of the unnamed crater in the Centauri Montes region, as it appeared in August 1999, and later in September 2005. No light-toned deposit was present in August 1999, but appeared by February 2004. The 300-meter scale bar represents 328 yards. Figure B: The second figure is a, Two Martian southern mid-latitude craters have new light-toned deposits that formed in gully settings during the course of the Mars Global Surveyor mission. Images from the Mars Orbiter Camera documented one case in an unnamed crater in Terra Sirenum, described in an accompanying release (see PIA09027 [ http://photojournal.jpl.nasa.gov/catalog/PIA09027 ] or MOC2-1618 [ http://www.msss.com/mars_images/moc/2006/12/06/gullies/sirenum_crater/index.html ], mosaic of several Mars Global Surveyor images, colorized using a table derived from Mars Reconnaissance Orbiter camera color data and overlain on a sub-frame of a Mars Odyssey Thermal Emission Imaging System image. The 1-kilometer scale bar represents about 0.62 miles. Figure C: The third figure is a colorized view of the light-toned gully deposit as viewed from an oblique perspective, draped over topography derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter camera. The new light-toned flow, by itself, does not prove that liquid water was involved in its genesis. However, this observation and the similar light-toned flow in Terra Sirenum together show that some gully sites are indeed changing today, providing tantalizing evidence there might be sources of liquid water beneath the surface of Mars right now. In both cases, these new flows may be indicating the locations of aquifers (subsurface rocks saturated with water) that could be detected by orbiting, ground-penetrating radar systems such as the Mars Express Mars Advanced Radar for Subsurface and Ionosphere Sounding or the Mars Reconnaissance Orbiter's Mars Shallow Subsurface Radar. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by NASA's Jet Propulsion Laboratory, Pasadena, Calif., a division of the California Institute of Technology, also in Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ].
New Gully Deposit in a Crate …
PIA09028
Sol (our sun)
Mars Orbiter Camera
Title New Gully Deposit in a Crater in the Centauri Montes Region
Original Caption Released with Image ). The second case, in an unnamed crater in the Centauri Montes region, east of the Hellas Basin, is described here. Gullies were first described by Mars Orbiter Camera scientists in June 2000, and many examples were presented in our June 2000 web releases and in a paper published in the journal Science. Additional examples of these middle and high-latitude landforms can be seen among the other more than 1,600 web releases. The new gully deposit in an unnamed crater in the Centauri Montes region is located near 38.7 degrees south latitude, 263.3 degrees west longitude. Like the new gully deposit in Terra Sirenum, this one has a light tone relative to its surroundings. It is on an equator-facing slope on which numerous narrow gully channels occur. As this slope is always in sunlight during the afternoons when Mars Global Surveyor passes overhead, the gullies always appear somewhat "washed out," just as craters on a full Moon do when viewed from Earth with a telescope. The new, light-toned flow was first noticed by the Mars Orbiter Camera science operations team in an image acquired on Sept. 10, 2005. Re-examination of other images of this crater showed that the new deposit had actually been present on Feb. 21, 2004, when the distal (down-slope) end of the deposit was captured in other images. In February 2004, the deposit had gone unnoticed because only a small portion of it was imaged. This location was first imaged by the Mars Orbiter Camera on Aug. 30, 1999. The deposit was not present at that time. Thus, it formed between Aug. 30, 1999 and Feb. 21, 2004. Roughly 20 percent brighter than the surface as it appeared before the flow occurred, the new deposit exhibits characteristics consistent with transport and deposition of a fluid that behaved like liquid water and likely transported some fine-grained sediment along with it. The distal end of the flow broke into several branches, or digits, and the material diverted and flowed around low obstacles. As with the example in Terra Sirenum, the depth of the flow is too thin to be measured in 1.5-meter-per-pixel (1.7-yard-per-pixel) images, so a very small volume of liquid and sediment was involved. While the material flowed and easily budded into several branches, it also must have moved slow enough to not topple over some of the low obstacles in its path. This picture is a colorized view of the light-toned gully deposit, draped over a topographic image derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment. Figure A: This figure shows the southeast wall of the unnamed crater in the Centauri Montes region, as it appeared in August 1999, and later in September 2005. No light-toned deposit was present in August 1999, but appeared by February 2004. The 300-meter scale bar represents 328 yards. Figure B: The second figure is a, Two Martian southern mid-latitude craters have new light-toned deposits that formed in gully settings during the course of the Mars Global Surveyor mission. Images from the Mars Orbiter Camera documented one case in an unnamed crater in Terra Sirenum, described in an accompanying release (see PIA09027 [ http://photojournal.jpl.nasa.gov/catalog/PIA09027 ] or MOC2-1618 [ http://www.msss.com/mars_images/moc/2006/12/06/gullies/sirenum_crater/index.html ], mosaic of several Mars Global Surveyor images, colorized using a table derived from Mars Reconnaissance Orbiter camera color data and overlain on a sub-frame of a Mars Odyssey Thermal Emission Imaging System image. The 1-kilometer scale bar represents about 0.62 miles. Figure C: The third figure is a colorized view of the light-toned gully deposit as viewed from an oblique perspective, draped over topography derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter camera. The new light-toned flow, by itself, does not prove that liquid water was involved in its genesis. However, this observation and the similar light-toned flow in Terra Sirenum together show that some gully sites are indeed changing today, providing tantalizing evidence there might be sources of liquid water beneath the surface of Mars right now. In both cases, these new flows may be indicating the locations of aquifers (subsurface rocks saturated with water) that could be detected by orbiting, ground-penetrating radar systems such as the Mars Express Mars Advanced Radar for Subsurface and Ionosphere Sounding or the Mars Reconnaissance Orbiter's Mars Shallow Subsurface Radar. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by NASA's Jet Propulsion Laboratory, Pasadena, Calif., a division of the California Institute of Technology, also in Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ].
New Gully Deposit in a Crate …
PIA09028
Sol (our sun)
Mars Orbiter Camera
Title New Gully Deposit in a Crater in the Centauri Montes Region
Original Caption Released with Image ). The second case, in an unnamed crater in the Centauri Montes region, east of the Hellas Basin, is described here. Gullies were first described by Mars Orbiter Camera scientists in June 2000, and many examples were presented in our June 2000 web releases and in a paper published in the journal Science. Additional examples of these middle and high-latitude landforms can be seen among the other more than 1,600 web releases. The new gully deposit in an unnamed crater in the Centauri Montes region is located near 38.7 degrees south latitude, 263.3 degrees west longitude. Like the new gully deposit in Terra Sirenum, this one has a light tone relative to its surroundings. It is on an equator-facing slope on which numerous narrow gully channels occur. As this slope is always in sunlight during the afternoons when Mars Global Surveyor passes overhead, the gullies always appear somewhat "washed out," just as craters on a full Moon do when viewed from Earth with a telescope. The new, light-toned flow was first noticed by the Mars Orbiter Camera science operations team in an image acquired on Sept. 10, 2005. Re-examination of other images of this crater showed that the new deposit had actually been present on Feb. 21, 2004, when the distal (down-slope) end of the deposit was captured in other images. In February 2004, the deposit had gone unnoticed because only a small portion of it was imaged. This location was first imaged by the Mars Orbiter Camera on Aug. 30, 1999. The deposit was not present at that time. Thus, it formed between Aug. 30, 1999 and Feb. 21, 2004. Roughly 20 percent brighter than the surface as it appeared before the flow occurred, the new deposit exhibits characteristics consistent with transport and deposition of a fluid that behaved like liquid water and likely transported some fine-grained sediment along with it. The distal end of the flow broke into several branches, or digits, and the material diverted and flowed around low obstacles. As with the example in Terra Sirenum, the depth of the flow is too thin to be measured in 1.5-meter-per-pixel (1.7-yard-per-pixel) images, so a very small volume of liquid and sediment was involved. While the material flowed and easily budded into several branches, it also must have moved slow enough to not topple over some of the low obstacles in its path. This picture is a colorized view of the light-toned gully deposit, draped over a topographic image derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment. Figure A: This figure shows the southeast wall of the unnamed crater in the Centauri Montes region, as it appeared in August 1999, and later in September 2005. No light-toned deposit was present in August 1999, but appeared by February 2004. The 300-meter scale bar represents 328 yards. Figure B: The second figure is a, Two Martian southern mid-latitude craters have new light-toned deposits that formed in gully settings during the course of the Mars Global Surveyor mission. Images from the Mars Orbiter Camera documented one case in an unnamed crater in Terra Sirenum, described in an accompanying release (see PIA09027 [ http://photojournal.jpl.nasa.gov/catalog/PIA09027 ] or MOC2-1618 [ http://www.msss.com/mars_images/moc/2006/12/06/gullies/sirenum_crater/index.html ], mosaic of several Mars Global Surveyor images, colorized using a table derived from Mars Reconnaissance Orbiter camera color data and overlain on a sub-frame of a Mars Odyssey Thermal Emission Imaging System image. The 1-kilometer scale bar represents about 0.62 miles. Figure C: The third figure is a colorized view of the light-toned gully deposit as viewed from an oblique perspective, draped over topography derived from Mars Global Surveyor's Mars Orbiter Laser Altimeter data. The color comes from a table derived from the colors of Mars as seen by the Mars Reconnaissance Orbiter camera. The new light-toned flow, by itself, does not prove that liquid water was involved in its genesis. However, this observation and the similar light-toned flow in Terra Sirenum together show that some gully sites are indeed changing today, providing tantalizing evidence there might be sources of liquid water beneath the surface of Mars right now. In both cases, these new flows may be indicating the locations of aquifers (subsurface rocks saturated with water) that could be detected by orbiting, ground-penetrating radar systems such as the Mars Express Mars Advanced Radar for Subsurface and Ionosphere Sounding or the Mars Reconnaissance Orbiter's Mars Shallow Subsurface Radar. The Mars Global Surveyor mission is managed for NASA's Office of Space Science, Washington, by NASA's Jet Propulsion Laboratory, Pasadena, Calif., a division of the California Institute of Technology, also in Pasadena. Lockheed Martin Space Systems, Denver, developed and operates the spacecraft. Malin Space Science Systems, San Diego, Calif., built and operates the Mars Orbiter Camera. For more information about images from the Mars Orbiter Camera, see http://www.msss.com/mgs/moc/index.html [ http://www.msss.com/mgs/moc/index.html ].
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - At Kennedy Space Center?s Shuttle Landing Facility, one of two containers with the Mars Reconnaissance Orbiter (MRO) equipment is rolled toward the ramp of the Air Force C-17 cargo plane. The MRO is being moved to the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - At Kennedy Space Center?s Shuttle Landing Facility, the second of two containers with the Mars Reconnaissance Orbiter (MRO) equipment is lifted onto a flatbed truck for transport to the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - Workers roll one of two containers with the Mars Reconnaissance Orbiter (MRO) equipment into the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - Workers at Kennedy Space Center?s Shuttle Landing Facility roll one of two containers with the Mars Reconnaissance Orbiter (MRO) equipment away from the Air Force C-17 cargo plane that delivered it. The MRO is being moved to the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - Workers at Kennedy Space Center?s Shuttle Landing Facility roll the second of two containers with the Mars Reconnaissance Orbiter (MRO) equipment away from the Air Force C-17 cargo plane that delivered it. The MRO is being moved to the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - A forklift moves into place behind the Air Force C-17 cargo plane delivering the Mars Reconnaissance Orbiter (MRO) equipment to Kennedy Space Center?s Shuttle Landing Facility. The MRO is being moved to the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - A forklift lowers one of two containers with the Mars Reconnaissance Orbiter (MRO) equipment onto the ground in front of the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - Workers at Kennedy Space Center?s Shuttle Landing Facility roll one of two containers with the Mars Reconnaissance Orbiter (MRO) equipment away from the Air Force C-17 cargo plane that delivered it. The MRO is being moved to the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - One of two containers with the Mars Reconnaissance Orbiter (MRO) equipment arrives at the Payload Hazardous Servicing Facility. The MRO was built by Lockheed-Martin for NASA?s Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO carries six primary instruments: the High Resolution Imaging Science Experiment, Context Camera, Mars Color Imager, Compact Reconnaissance Imaging Spectrometer for Mars, Mars Climate Sounder and Shallow Radar. By 2007, the MRO will begin a series of global mapping, regional survey and targeted observations from a near-polar, low-altitude Mars orbit. It will observe the atmosphere and surface of Mars while probing its shallow subsurface as part of a ?follow the water? strategy.
Release Date 04/30/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility at NASA?s Kennedy Space Center, workers from Lockheed Martin help raise the high-gain antenna vertically for installation on the Mars Reconnaissance Orbiter (MRO). After solar array installation, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/25/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, workers from Lockheed Martin deploy the newly installed solar array on the Mars Reconnaissance Orbiter (MRO). After solar array testing, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/28/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility at NASA?s Kennedy Space Center, workers from Lockheed Martin prepare the high-gain antenna to be moved toward the Mars Reconnaissance Orbiter (MRO) for installation. After solar array installation, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/25/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility at NASA?s Kennedy Space Center, workers from Lockheed Martin test the installation of the high-gain antenna on the Mars Reconnaissance Orbiter (MRO). After solar array installation, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/25/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility at NASA?s Kennedy Space Center, workers from Lockheed Martin prepare the high-gain antenna for installation on the Mars Reconnaissance Orbiter (MRO), in the background. After solar array installation, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/25/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility at NASA?s Kennedy Space Center, workers from Lockheed Martin help guide the high-gain antenna toward the Mars Reconnaissance Orbiter (MRO) for installation. After solar array installation, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/25/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility at NASA?s Kennedy Space Center, workers from Lockheed Martin prepare the high-gain antenna for installation on the Mars Reconnaissance Orbiter (MRO). After solar array installation, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/25/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility at NASA?s Kennedy Space Center, workers from Lockheed Martin begin installing the high-gain antenna on the Mars Reconnaissance Orbiter (MRO). After solar array installation, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/25/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, workers from Lockheed Martin prepare to deploy the solar array on the Mars Reconnaissance Orbiter (MRO). After solar array testing, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/28/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, workers from Lockheed Martin begin deploying the solar array on the Mars Reconnaissance Orbiter (MRO). After solar array testing, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/28/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, workers from Lockheed Martin deploy the newly installed solar array on the Mars Reconnaissance Orbiter (MRO). After solar array testing, the MRO will be transported to the Vertical Installation Facility in late July. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 06/28/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, the Mars Reconnaissance Orbiter (MRO) has been lifted off the rotation stand and is being transferred to a Mars Orbit Insertion Thruster assembly stand for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/05/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -In the Payload Hazardous Servicing Facility, workers from Lockheed Martin help guide the Mars Reconnaissance Orbiter (MRO) onto a Mars Orbit Insertion Thruster assembly stand for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/05/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, the Mars Reconnaissance Orbiter (MRO) has been lifted off the rotation stand and is being moved toward a Mars Orbit Insertion Thruster assembly stand for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/05/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, workers from Lockheed Martin install the Mars Reconnaissance Orbiter (MRO) onto a Mars Orbit Insertion Thruster assembly stand for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/05/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, workers from Lockheed Martin prepare the Mars Reconnaissance Orbiter (MRO) to be lifted from the rotation stand. It is being transferred to a Mars Orbit Insertion Thruster assembly stand for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/05/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. - In the Payload Hazardous Servicing Facility, the Mars Reconnaissance Orbiter (MRO) is lowered toward a Mars Orbit Insertion Thruster assembly stand for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/05/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -- In the Payload Hazardous Servicing Facility, workers from Lockheed Martin begin securing the Mars Reconnaissance Orbiter (MRO) onto the spin balance machine for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/09/2005
KENNEDY SPACE CENTER, FLA. - …
Description KENNEDY SPACE CENTER, FLA. -- In the Payload Hazardous Servicing Facility, workers from Lockheed Martin stand nearby as the suspended Mars Reconnaissance Orbiter (MRO) is lowered toward the spin balance machine for testing. In late July, the MRO will be transported to the Vertical Installation Facility. It will join the Atlas V for the final phase of launch preparations. The spacecraft is then scheduled to undergo a functional test, and a final week of integrated testing and closeouts. The MRO was built by Lockheed Martin for the Jet Propulsion Laboratory in California. It is the next major step in Mars exploration and scheduled for launch from Cape Canaveral Air Force Station in a window opening Aug. 10. The MRO is an important next step in fulfilling NASA?s vision of space exploration and ultimately sending human explorers to Mars and beyond.
Release Date 07/09/2005
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