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Images de 'Mars' médias trouvés, 104,759

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March: Iani Chaos - Mars: Iani Chaos - The region of Iani Chaos on Mars. Image obtained by the Mars Express probe. Iani Chaos on Mars, an area where Light Toned Deposits, or LTD, are known to be present. An analysis of data and images from Mars Express suggests that several LTD, some of the least understood structures on Mars, were formed when large amounts of groundwater burst on to the surface. Scientists propose that groundwater had a greater role in shaping the martian surface than previously believed, and may have sheltered primitive life forms as the planet started drying up. This image was obtained with the High Resolution Stereo Camera on board ESA's Mars Express spacecraft

March: Iani Chaos - Mars: Iani Chaos - The region of Iani Chaos on Mars. Image obtained by the Mars Express probe. Iani Chaos on Mars, an area where Light Toned Deposits, or LTD, are known to be present. An analysis of data and images from Mars Express suggests that several LTD, some of the least understood structures on Mars, were formed when large amounts of groundwater burst on to the surface. Scientists propose that groundwater had a greater role in shaping the martian surface than previously believed, and may have sheltered primitive life forms as the planet started drying up. This image was obtained with the High Resolution Stereo Camera on board ESA's Mars Express spacecraft

PIX4616054

Mars - Satellite Phobos - Martian moon Phobos - View of the satellite Phobos obtained by the Mars Express probe on July 23, 2008 at a distance of 97 km from the Martian moon. The resolution is 3.7 meters per pixel. On 23 July 2008, the High Resolution Stereo Camera on board the ESA's Mars Express took the highest - resolution full - disc image yet of the surface of the moon Phobos. The image data was acquired from a distance of 97 km with a spatial resolution of about 3.7 m/pixel in orbit 5851. These images have surpassed all previous images from other missions in continuous coverage of the illuminated surface at the highest spatial resolution of 3.7 m/pixel. This image is photometrically enhanced to bring out the features in the less illuminated part

Mars - Satellite Phobos - Martian moon Phobos - View of the satellite Phobos obtained by the Mars Express probe on July 23, 2008 at a distance of 97 km from the Martian moon. The resolution is 3.7 meters per pixel. On 23 July 2008, the High Resolution Stereo Camera on board the ESA's Mars Express took the highest - resolution full - disc image yet of the surface of the moon Phobos. The image data was acquired from a distance of 97 km with a spatial resolution of about 3.7 m/pixel in orbit 5851. These images have surpassed all previous images from other missions in continuous coverage of the illuminated surface at the highest spatial resolution of 3.7 m/pixel. This image is photometrically enhanced to bring out the features in the less illuminated part

PIX4616278

Mars - Phobos Satellite - Martian moon Phobos - View of the Phobos satellite obtained by the Mars Express probe on March 7, 2010. The resolution is 4.4 meters per pixel. Mars Express took this image of the surface of the moon Phobos on 7 March 2010. The resolution is about 4.4 m/pixel

Mars - Phobos Satellite - Martian moon Phobos - View of the Phobos satellite obtained by the Mars Express probe on March 7, 2010. The resolution is 4.4 meters per pixel. Mars Express took this image of the surface of the moon Phobos on 7 March 2010. The resolution is about 4.4 m/pixel

PIX4616280

Crater Bacolor on Mars - Bacolor Crater on planet Mars - View of the impact crater Bacolor obtained by the Mars Odyssey probe. It's an impact crater about 20 km in diameter. Bacolor Crater is a magnificent impact feature about 20 kilometers (12 miles) wide. The lines on the ejecta blanket surrounding the crater rim come from a surge of superheated gas and debris flying outward in the wake of the meteorite impact that made the crater. This view combines images taken during the period from September 2002 to October 2005 by the Thermal Emission Imaging System instrument on Nasa's Mars Odyssey orbiter. The pictured location on Mars is 33 degrees north latitude, 118.6 degrees east longitude

Crater Bacolor on Mars - Bacolor Crater on planet Mars - View of the impact crater Bacolor obtained by the Mars Odyssey probe. It's an impact crater about 20 km in diameter. Bacolor Crater is a magnificent impact feature about 20 kilometers (12 miles) wide. The lines on the ejecta blanket surrounding the crater rim come from a surge of superheated gas and debris flying outward in the wake of the meteorite impact that made the crater. This view combines images taken during the period from September 2002 to October 2005 by the Thermal Emission Imaging System instrument on Nasa's Mars Odyssey orbiter. The pictured location on Mars is 33 degrees north latitude, 118.6 degrees east longitude

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Mars - Gale Crater Region - Gale Crater area on planet Mars - View of the region of the impact crater Gale in which the Curiosity rover will be installed in 2012. This crater (in the top center of the picture) is 154 km in diameter. Image recomposed from data obtained by the Mars Global Surveyor probe. This computer - generated view depicts part of Mars at the boundary between darkness and daylight, with an area including Gale Crater beginning to catch morning light. Northward is to the left. Gale is the crater with a mound inside it near the center of the image. NASA has selected Gale as the landing site for the Mars Science Laboratory mission. The mission's rover will be placed on the ground in a northern portion of Gale crater in August 2012. Gale crater is 96 miles (154 kilometers) in diameter and holds a layered mountain rising about 3 miles (5 kilometers) above the crater floor. The intended landing site is at 4.5 degrees south latitude, 137.4 degrees east longitude. This view wa

Mars - Gale Crater Region - Gale Crater area on planet Mars - View of the region of the impact crater Gale in which the Curiosity rover will be installed in 2012. This crater (in the top center of the picture) is 154 km in diameter. Image recomposed from data obtained by the Mars Global Surveyor probe. This computer - generated view depicts part of Mars at the boundary between darkness and daylight, with an area including Gale Crater beginning to catch morning light. Northward is to the left. Gale is the crater with a mound inside it near the center of the image. NASA has selected Gale as the landing site for the Mars Science Laboratory mission. The mission's rover will be placed on the ground in a northern portion of Gale crater in August 2012. Gale crater is 96 miles (154 kilometers) in diameter and holds a layered mountain rising about 3 miles (5 kilometers) above the crater floor. The intended landing site is at 4.5 degrees south latitude, 137.4 degrees east longitude. This view wa

PIX4615396

Mars - Phobos Satellite - Martian moon Phobos - View of the Phobos satellite obtained by the Mars Express probe in March 2010. The north pole is indicated. Mars Express took this image of the surface of the moon Phobos in March 2010. The resolution is about 9 m/pixel

Mars - Phobos Satellite - Martian moon Phobos - View of the Phobos satellite obtained by the Mars Express probe in March 2010. The north pole is indicated. Mars Express took this image of the surface of the moon Phobos in March 2010. The resolution is about 9 m/pixel

PIX4616274

Mars - Satellite Phobos - Martian moon Phobos - View of the satellite Phobos obtained by the Mars Express probe on January 9, 2011, at a distance of 100 km from the satellite. The south pole is indicated. Mars Express took this image of the surface of the moon Phobos on January 9, 2011. Mars Express passed Mars' largest moon at a distance of 100 km. South pole is indicated

Mars - Satellite Phobos - Martian moon Phobos - View of the satellite Phobos obtained by the Mars Express probe on January 9, 2011, at a distance of 100 km from the satellite. The south pole is indicated. Mars Express took this image of the surface of the moon Phobos on January 9, 2011. Mars Express passed Mars' largest moon at a distance of 100 km. South pole is indicated

PIX4616339

Mars view of Phobos - Illustration - Mars from Phobos - Illustration - Mars view from Phobos satellite. A view of Mars from its moon Phobos

Mars view of Phobos - Illustration - Mars from Phobos - Illustration - Mars view from Phobos satellite. A view of Mars from its moon Phobos

PIX4616832

March: chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles and Sacra Fossae. To the north, the large impact crater is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The image shows an old 35 km - diameter impact crater in the north. The crater's southwestern rim is eroded strongly, mostly by flowing water. The source of the water was located in Etus Chasma, which lies about 850 km to the southwest. The crater floor and the northwestern part are remarkably flat, formed by sediments and basaltic lava fl

March: chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles and Sacra Fossae. To the north, the large impact crater is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The image shows an old 35 km - diameter impact crater in the north. The crater's southwestern rim is eroded strongly, mostly by flowing water. The source of the water was located in Etus Chasma, which lies about 850 km to the southwest. The crater floor and the northwestern part are remarkably flat, formed by sediments and basaltic lava fl

PIX4616176

March -Satellite Phobos - Martian moon Phobos: View of the Phobos satellite obtained by the ExoMars probe on November 26, 2016, at a distance of 7700 km from the satellite. Colour composite of Phobos taken with the ExoMars orbiter's Colour and Stereo Surface Imaging System (Cassis) on 26 November 2016. The observation was made at a distance of 7700 km and yields a resolution of 87 m/pixel

March -Satellite Phobos - Martian moon Phobos: View of the Phobos satellite obtained by the ExoMars probe on November 26, 2016, at a distance of 7700 km from the satellite. Colour composite of Phobos taken with the ExoMars orbiter's Colour and Stereo Surface Imaging System (Cassis) on 26 November 2016. The observation was made at a distance of 7700 km and yields a resolution of 87 m/pixel

PIX4616732

Mars eclipse the Sun - Illustration - Phobos Eclipse - Artwork - Eclipse of the Sun seen from Phobos, one of Mars's satellites. Solar eclipse seen from Phobos.

Mars eclipse the Sun - Illustration - Phobos Eclipse - Artwork - Eclipse of the Sun seen from Phobos, one of Mars's satellites. Solar eclipse seen from Phobos.

Miller, Ron (b.1947)

PIX4617121

Image made from altimetric data obtained by the Mars Global Surveyor probe. The northern polar cap is mostly made up of water ice. It measures about 1100 km - Altimetric image of north pole made from MOLA instrument observations on the Mars Global Surveyor spacecraft. This image is colored according to the relative height of the surface features: North Mars pole seen by Mars Global Surveyor - Mars north pole

Image made from altimetric data obtained by the Mars Global Surveyor probe. The northern polar cap is mostly made up of water ice. It measures about 1100 km - Altimetric image of north pole made from MOLA instrument observations on the Mars Global Surveyor spacecraft. This image is colored according to the relative height of the surface features: North Mars pole seen by Mars Global Surveyor - Mars north pole

PIX4615383

Mars and its satellites - Mars and its moons - Photomontage showing the planet Mars surrounded by its two satellites, Phobos (middle) and Deimos (right)

Mars and its satellites - Mars and its moons - Photomontage showing the planet Mars surrounded by its two satellites, Phobos (middle) and Deimos (right)

PIX4616921

Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater at the top of the picture is 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The surface is mostly smooth, and is covered by several small impact craters measuring 800 to 2800 m in diameter. Smaller craters are scattered across the entire region. A larger impact crater measuring 20 km in diameter is a prominent f

Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater at the top of the picture is 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The surface is mostly smooth, and is covered by several small impact craters measuring 800 to 2800 m in diameter. Smaller craters are scattered across the entire region. A larger impact crater measuring 20 km in diameter is a prominent f

PIX4616151

The probe Mars 96 - Artist view - Mars 96 spacecraft - Artist view - Artist view of the sovietic probe Mars 96 observing the planet Mars. Launched in 1996, the probe could not leave Earth orbit and disintegrate. Artwork showing the soviet March 96 spacecraft above planet Mars. Launched in 1996, a rocket failure happened and the probe was desintegrated in the Earth atmosphere

The probe Mars 96 - Artist view - Mars 96 spacecraft - Artist view - Artist view of the sovietic probe Mars 96 observing the planet Mars. Launched in 1996, the probe could not leave Earth orbit and disintegrate. Artwork showing the soviet March 96 spacecraft above planet Mars. Launched in 1996, a rocket failure happened and the probe was desintegrated in the Earth atmosphere

D. Ducros

PIX4606422

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

PIX4606652

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

D. Ducros

PIX4606610

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

D. Ducros

PIX4606614

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

D. Ducros

PIX4606616

Detail of the 1st color panorama of the Martian soil obtained by Spirit. The Rover Spirit landed on Mars in the area of the crater Gusev, July 4, 2004 - Detail of the first panorama taken by Spirit.: Surface de Mars: detail of the first panorama obtained by Spirit - The martian surface seen by Spirit. 07/2004

Detail of the 1st color panorama of the Martian soil obtained by Spirit. The Rover Spirit landed on Mars in the area of the crater Gusev, July 4, 2004 - Detail of the first panorama taken by Spirit.: Surface de Mars: detail of the first panorama obtained by Spirit - The martian surface seen by Spirit. 07/2004

PIX4615535

March: Hebes Chasma - Hebes Chasma is a basin of almost 8000 m deep located in the northern part of Valles Marineris, the great Martian canyon. At the centre of this depression is a stratified plateau that constitutes sedimentary deposits. Perspective image obtained by the Mars Express probe in 2005. Perspective view of Hebes Chasma obtained by the High Resolution Stereo Camera (HRSC) on ESA's Mars Express spacecraft. Hebes Chasma is an enclosed trough, almost 8000 m deep, in Valles Marineris, the Grand Canyon of Mars, where water is believed to have flowed. Hebes Chasma is located at approximately 1* south and 282* east. The HRSC obtained image data on 16 September 2005 with a ground resolution of approximately 15 m/pixel

March: Hebes Chasma - Hebes Chasma is a basin of almost 8000 m deep located in the northern part of Valles Marineris, the great Martian canyon. At the centre of this depression is a stratified plateau that constitutes sedimentary deposits. Perspective image obtained by the Mars Express probe in 2005. Perspective view of Hebes Chasma obtained by the High Resolution Stereo Camera (HRSC) on ESA's Mars Express spacecraft. Hebes Chasma is an enclosed trough, almost 8000 m deep, in Valles Marineris, the Grand Canyon of Mars, where water is believed to have flowed. Hebes Chasma is located at approximately 1* south and 282* east. The HRSC obtained image data on 16 September 2005 with a ground resolution of approximately 15 m/pixel

PIX4616076

Our Near Neighbour, Mars (engraving)

Our Near Neighbour, Mars (engraving)

English School, (19th century)

LIP1627909

Mars: Valles Marineris - Mosaic of 20 images obtained by the European probe Mars Express. This image shows the eastern part of Valles Marineris, a canyon about 4500 km long and 8 km deep. This mosaic image of eastern part of Valles Marineris - colored to resemble the martian surface - comes from Esa's Mars Express spacecraft, which repeatedly crosses the Martian equator from north to south or south to north. The High Resolution Stereo Camera (HRSC) on board Mars Express, has been taking image strips of the valley system since 2004 as it passes overhead. The individual HRSC image strips are each between 50 and 200 kilometers wide, depending on Mars Express' orbit, so this view of Valles Marineris has only been made possible by creating a mosaic using 20 separate images. To improve the presentation here, the altitudes have been exaggerated fourfold, so that the slopes and mountainsides appear steeper than they are in reality. The colours in this image are slightly false as well. By incre

Mars: Valles Marineris - Mosaic of 20 images obtained by the European probe Mars Express. This image shows the eastern part of Valles Marineris, a canyon about 4500 km long and 8 km deep. This mosaic image of eastern part of Valles Marineris - colored to resemble the martian surface - comes from Esa's Mars Express spacecraft, which repeatedly crosses the Martian equator from north to south or south to north. The High Resolution Stereo Camera (HRSC) on board Mars Express, has been taking image strips of the valley system since 2004 as it passes overhead. The individual HRSC image strips are each between 50 and 200 kilometers wide, depending on Mars Express' orbit, so this view of Valles Marineris has only been made possible by creating a mosaic using 20 separate images. To improve the presentation here, the altitudes have been exaggerated fourfold, so that the slopes and mountainsides appear steeper than they are in reality. The colours in this image are slightly false as well. By incre

PIX4616253

Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater on the left of the image measures 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The surface is mostly smooth, and is covered by several small impact craters measuring 800 to 2800 m in diameter. Smaller craters are scattered across the entire region. The left side of the image shows a large impact crater measuri

Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater on the left of the image measures 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The surface is mostly smooth, and is covered by several small impact craters measuring 800 to 2800 m in diameter. Smaller craters are scattered across the entire region. The left side of the image shows a large impact crater measuri

PIX4616156

Mission habitee vers Mars-View d'artiste - Manned mission to Mars - Artist vie

Mission habitee vers Mars-View d'artiste - Manned mission to Mars - Artist vie

S. Numazawa

PIX4639464

Mars surface seen by the rover Curiosity 03/2014: The formation “” Kimberley “” seen by Curiosity on March 25, 2014. The strata indicate a flow of water towards Mount Sharp (in the background). A view from the “” Kimberley”” formation on Mars taken by Nasa's Curiosity rover. The strata in the foreground dip towards the base of Mount Sharp, indicating flow of water toward a basin that existed before the larger bulk of the mountain formed. The colors are adjusted so that rocks look approximately as they would if they were on Earth, to help geologists interpret the rocks. This “” white balancing”” to adjust for the lighting on Mars overly compensates for the absence of blue on Mars, making the sky appear light blue and sometimes giving dark, black rocks a blue cast.

Mars surface seen by the rover Curiosity 03/2014: The formation “” Kimberley “” seen by Curiosity on March 25, 2014. The strata indicate a flow of water towards Mount Sharp (in the background). A view from the “” Kimberley”” formation on Mars taken by Nasa's Curiosity rover. The strata in the foreground dip towards the base of Mount Sharp, indicating flow of water toward a basin that existed before the larger bulk of the mountain formed. The colors are adjusted so that rocks look approximately as they would if they were on Earth, to help geologists interpret the rocks. This “” white balancing”” to adjust for the lighting on Mars overly compensates for the absence of blue on Mars, making the sky appear light blue and sometimes giving dark, black rocks a blue cast.

PIX4616687

March: Spherule seen by Opportunity - Mars: hematite - rich berry seen by Opportunity - Spherule of a few millimetres in diameter, rich in hematite, seen on the surface of a Martian rock by the microscope camera of the rover Opportunity on March 4, 2004. Recolorized image. Opportunity micrograph of Martian soil taken on Sol 39 (march 4 2004), showing the blueberries of hematite, indicators of evidence of past water activity. Recolorized picture

March: Spherule seen by Opportunity - Mars: hematite - rich berry seen by Opportunity - Spherule of a few millimetres in diameter, rich in hematite, seen on the surface of a Martian rock by the microscope camera of the rover Opportunity on March 4, 2004. Recolorized image. Opportunity micrograph of Martian soil taken on Sol 39 (march 4 2004), showing the blueberries of hematite, indicators of evidence of past water activity. Recolorized picture

Steven Hobbs

PIX4615783

Mars Polar Lander - Artist view - Mars Polar Lander spaceprobe - Artist view - The American Mars Polar Lander probe, launched on January 3, 1999, was scheduled to land in December 1999 near the southern polar cap of Mars. Contact with the probe was interrupted on 3 December 1999, when it entered the Martian atmosphere. The Mars Polar Lander is shown on the surface of Mars. The spacecraft was launched in january 1999 to Mars to land near the southern polar cap in December 1999 and carry out a three - month mission to search for traces of subsurface water in this frozen, layered terrain. The contact with the spacecraft was lost on December 9, 1999, shortly after it entered the Martian atmosphere

Mars Polar Lander - Artist view - Mars Polar Lander spaceprobe - Artist view - The American Mars Polar Lander probe, launched on January 3, 1999, was scheduled to land in December 1999 near the southern polar cap of Mars. Contact with the probe was interrupted on 3 December 1999, when it entered the Martian atmosphere. The Mars Polar Lander is shown on the surface of Mars. The spacecraft was launched in january 1999 to Mars to land near the southern polar cap in December 1999 and carry out a three - month mission to search for traces of subsurface water in this frozen, layered terrain. The contact with the spacecraft was lost on December 9, 1999, shortly after it entered the Martian atmosphere

PIX4606673

Mars Science Laboratory - Artist View - Mars Science Laboratory - Artist view - Mars Science Laboratory (MSL), named Curiosity, is a NASA rover that will explore the surface of Mars from 2012 onwards. In this artist's view, Curiosity analyses the chemical composition of a Martian rock using the ChECAM instrument. This artist's concept depicts the rover Curiosity, of Nasa's Mars Science Laboratory mission, as it uses its Chemistry and Camera (ChemCam) instrument to investigate the composition of a rock surface. ChemCam fires laser pulses at a target and views the resulting spark with a telescope and spectrometers to identify chemical elements. The laser is actually in an invisible infrared wavelength, but is shown here as visible red light for purposes of illustration

Mars Science Laboratory - Artist View - Mars Science Laboratory - Artist view - Mars Science Laboratory (MSL), named Curiosity, is a NASA rover that will explore the surface of Mars from 2012 onwards. In this artist's view, Curiosity analyses the chemical composition of a Martian rock using the ChECAM instrument. This artist's concept depicts the rover Curiosity, of Nasa's Mars Science Laboratory mission, as it uses its Chemistry and Camera (ChemCam) instrument to investigate the composition of a rock surface. ChemCam fires laser pulses at a target and views the resulting spark with a telescope and spectrometers to identify chemical elements. The laser is actually in an invisible infrared wavelength, but is shown here as visible red light for purposes of illustration

PIX4606775

Rover Curiosity on Mars - Curiosity Mars rover selfie - Mars Science Laboratory (MSL), named Curiosity, is a NASA rover exploring the surface of Mars. This self-portrait is a composite of images taken by the robot on August 5, 2015. This low-angle self-portrait of Nasa's Curiosity Mars rover shows the vehicle at the site from which it reached down to drill into a rock target called “” Buckskin”” on lower Mount Sharp. The selfie combines several component images taken by Curiosity's Mars Hand Lens Imager (MAHLI) on Aug. 5, 2015, during the 1,065th Martian day, or sol, of the rover's work on Mars. For scale, the rover's wheels are 20 inches (50 centimeters) in diameter and about 16 inches (40 centimeters) wide

Rover Curiosity on Mars - Curiosity Mars rover selfie - Mars Science Laboratory (MSL), named Curiosity, is a NASA rover exploring the surface of Mars. This self-portrait is a composite of images taken by the robot on August 5, 2015. This low-angle self-portrait of Nasa's Curiosity Mars rover shows the vehicle at the site from which it reached down to drill into a rock target called “” Buckskin”” on lower Mount Sharp. The selfie combines several component images taken by Curiosity's Mars Hand Lens Imager (MAHLI) on Aug. 5, 2015, during the 1,065th Martian day, or sol, of the rover's work on Mars. For scale, the rover's wheels are 20 inches (50 centimeters) in diameter and about 16 inches (40 centimeters) wide

PIX4643615

Mars: crateres and canals in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater on the left is 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. This image covering an area of approximately 150 km exhibits a large impact crater measuring 20 kilometers in diameter. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region

Mars: crateres and canals in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. The large impact crater on the left is 20 km in diameter. The image covering an area of about 150 square km was obtained by the Mars Express probe on 28 December 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. This image covering an area of approximately 150 km exhibits a large impact crater measuring 20 kilometers in diameter. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region

PIX4616155

March: chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles and Sacra Fossae. The large impact crater is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The image shows an old 35 km - diameter impact crater in the north. The crater's southwestern rim is eroded strongly, mostly by flowing water. The source of the water was located in Echo Chasma, which lies about 850 km to the southwest

March: chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles and Sacra Fossae. The large impact crater is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The image shows an old 35 km - diameter impact crater in the north. The crater's southwestern rim is eroded strongly, mostly by flowing water. The source of the water was located in Echo Chasma, which lies about 850 km to the southwest

PIX4616171

Mars Exploration Rover - Mars Exploration Rover is a Martian exploration mission composed of two probes housing two identical rovers, Spirit and Opportunity MER - A, the Spirit robot launched on June 10, 2003, landed on January 3, 2004 in the crater Gusev. MER - B, the Opportunity robot launched on July 8, 2003, landed on January 24, 2004 on Meridiani Planum. The sun rises behind one of the Mars Exploration Rovers as it prepares to analyse a rock with its RAT tool. Mars Exploration Rover (MER) is a robotic mission which aims to explore the Martian surface and geology. The mission began with the sending of two twin rovers: MER - A (Spirit), launched on June 10 2003 and landed on January 03 2004 in Gusev crater; MER - B (Opportunity) launched on July 08 2003 and landed on January 24 2004 at Meridiani Planum

Mars Exploration Rover - Mars Exploration Rover is a Martian exploration mission composed of two probes housing two identical rovers, Spirit and Opportunity MER - A, the Spirit robot launched on June 10, 2003, landed on January 3, 2004 in the crater Gusev. MER - B, the Opportunity robot launched on July 8, 2003, landed on January 24, 2004 on Meridiani Planum. The sun rises behind one of the Mars Exploration Rovers as it prepares to analyse a rock with its RAT tool. Mars Exploration Rover (MER) is a robotic mission which aims to explore the Martian surface and geology. The mission began with the sending of two twin rovers: MER - A (Spirit), launched on June 10 2003 and landed on January 03 2004 in Gusev crater; MER - B (Opportunity) launched on July 08 2003 and landed on January 24 2004 at Meridiani Planum

Steven Hobbs

PIX4606584

Mars and its satellites - Mars and its moons - Photomontage showing the planet Mars surrounded by its two satellites, Phobos (middle) and Deimos (right)

Mars and its satellites - Mars and its moons - Photomontage showing the planet Mars surrounded by its two satellites, Phobos (middle) and Deimos (right)

PIX4616910

Mars and its satellites - Mars and its moons - Photomontage showing the planet Mars surrounded by its two satellites, Phobos (middle) and Deimos (left)

Mars and its satellites - Mars and its moons - Photomontage showing the planet Mars surrounded by its two satellites, Phobos (middle) and Deimos (left)

PIX4616933

Terraformation de Mars-Illustration - Terraforming of Mars - Illustration - In 1000 years, the inhabitants of the cites under the dome of Phobos will be able to contemplate the Martian oceans from their balconies. The terraforming of a planet, moon or other body, is the hypothetical process of deliberately modifying its atmosphere, temperature, or ecology to be similar to those of Earth in order to make it habitable by humans. Inhabitants of Phobos would gaze martian oceans in the next thousand years

Terraformation de Mars-Illustration - Terraforming of Mars - Illustration - In 1000 years, the inhabitants of the cites under the dome of Phobos will be able to contemplate the Martian oceans from their balconies. The terraforming of a planet, moon or other body, is the hypothetical process of deliberately modifying its atmosphere, temperature, or ecology to be similar to those of Earth in order to make it habitable by humans. Inhabitants of Phobos would gaze martian oceans in the next thousand years

P. Carril

PIX4639658

The Mars Express and Beagle 2 probe - Artist view - Mars Express and Beagle 2 - Separation of the Beagle 2 module. The Beagle 2 landing gear that was supposed to perform analysis on the surface of Mars did not work. The European Mars Express probe was launched on 2 June 2003 and began its observations in early 2004. Illustration showing the separation of Beagle 2 from Mars Express. Beagle 2 was lost but the european spaceprobe Mars Express began its March observations in 2004

The Mars Express and Beagle 2 probe - Artist view - Mars Express and Beagle 2 - Separation of the Beagle 2 module. The Beagle 2 landing gear that was supposed to perform analysis on the surface of Mars did not work. The European Mars Express probe was launched on 2 June 2003 and began its observations in early 2004. Illustration showing the separation of Beagle 2 from Mars Express. Beagle 2 was lost but the european spaceprobe Mars Express began its March observations in 2004

D. Ducros

PIX4606641

The Mars Express and Beagle 2 probe - Artist view - Mars Express and Beagle 2 - Separation of the Beagle 2 module. The Beagle 2 landing gear that was supposed to perform analysis on the surface of Mars did not work. The European Mars Express probe was launched on 2 June 2003 and began its observations in early 2004. Illustration showing the separation of Beagle 2 from Mars Express. Beagle 2 was lost but the european spaceprobe Mars Express began its March observations in 2004

The Mars Express and Beagle 2 probe - Artist view - Mars Express and Beagle 2 - Separation of the Beagle 2 module. The Beagle 2 landing gear that was supposed to perform analysis on the surface of Mars did not work. The European Mars Express probe was launched on 2 June 2003 and began its observations in early 2004. Illustration showing the separation of Beagle 2 from Mars Express. Beagle 2 was lost but the european spaceprobe Mars Express began its March observations in 2004

D. Ducros

PIX4606646

Glaciers under Martian crateres - Buried glaciers on Mars - Computer reconstructed views of three Martian crateres in the Hellas region that house glaciers. The images show the crateres as they appear today with a layer of Martian soil covering the ice with water and, on the right, the glaciers updated according to radar measurements obtained by the Mars Reconnaissance Orbiter probe (MRO). These glaciers would have a thickness of 250 to 450 meters. Each image covers 20 km wide. This computer graphic image shows three craters in the eastern Hellas region of Mars containing concealed glaciers detected by radar. The images shows how the surface looks today with the ice covered with a layer of Martian soil and what the ice may look like underneath. The image was created using image data from the Context Camera on the Mars Reconnaissance Orbiter (MRO) spacecraft combined with results from the SHARAD radar sounder on MRO and HRSC digital elevation map from the Mars Express spacecraft. The co

Glaciers under Martian crateres - Buried glaciers on Mars - Computer reconstructed views of three Martian crateres in the Hellas region that house glaciers. The images show the crateres as they appear today with a layer of Martian soil covering the ice with water and, on the right, the glaciers updated according to radar measurements obtained by the Mars Reconnaissance Orbiter probe (MRO). These glaciers would have a thickness of 250 to 450 meters. Each image covers 20 km wide. This computer graphic image shows three craters in the eastern Hellas region of Mars containing concealed glaciers detected by radar. The images shows how the surface looks today with the ice covered with a layer of Martian soil and what the ice may look like underneath. The image was created using image data from the Context Camera on the Mars Reconnaissance Orbiter (MRO) spacecraft combined with results from the SHARAD radar sounder on MRO and HRSC digital elevation map from the Mars Express spacecraft. The co

PIX4616544

Mars - Noctis Labyrinthus - Image reconstructed from images taken by the 2001 Mars Odyssey probe.

Mars - Noctis Labyrinthus - Image reconstructed from images taken by the 2001 Mars Odyssey probe.

PIX4616427

Mars and its satellites seen with an amateur telescope - Mars with its moons through an amateur telescope - Composite image of the planet Mars accompanied by its two moving satellites, Phobos (left) and Deimos (right). Image taken with a C14 and a webcam on August 28, 2003 in Namibia. Composite image of planet Mars with its moons. Image taken on August 28 2003 from Namibia with a C14 telescope and a webcam. Phobos is moving on the left of the image, Deimos at right

Mars and its satellites seen with an amateur telescope - Mars with its moons through an amateur telescope - Composite image of the planet Mars accompanied by its two moving satellites, Phobos (left) and Deimos (right). Image taken with a C14 and a webcam on August 28, 2003 in Namibia. Composite image of planet Mars with its moons. Image taken on August 28 2003 from Namibia with a C14 telescope and a webcam. Phobos is moving on the left of the image, Deimos at right

Sebastian Voltmer

PIX4614913

Mars - View of the north pole - Mars north pole - Image based on altimetric data obtained by the Mars Global Surveyor probe. The northern polar cap is mostly made up of water ice. It's about 1100 km long. The ice - rich north polar cap (the quasi - circular white area at center) is approximately 1,000 kilometers (621 miles) across. The white cap is riven with dark, spiral - shaped bands. These are deep troughs that are in shadow. They do not reflect sunlight as well or have more internal layers exposed. To the right of center, a large canyon, Chasma Boreale, almost bisects the ice cap. Chasma Boreale is about the length of the United States' famous Grand Canyon and up to 2 kilometers (1.2 miles) deep. The image synthesizes topographic data from Mars Orbiter Laser Altimeter (MOLA) and images from the Mars Orbiter Camera (MOC)

Mars - View of the north pole - Mars north pole - Image based on altimetric data obtained by the Mars Global Surveyor probe. The northern polar cap is mostly made up of water ice. It's about 1100 km long. The ice - rich north polar cap (the quasi - circular white area at center) is approximately 1,000 kilometers (621 miles) across. The white cap is riven with dark, spiral - shaped bands. These are deep troughs that are in shadow. They do not reflect sunlight as well or have more internal layers exposed. To the right of center, a large canyon, Chasma Boreale, almost bisects the ice cap. Chasma Boreale is about the length of the United States' famous Grand Canyon and up to 2 kilometers (1.2 miles) deep. The image synthesizes topographic data from Mars Orbiter Laser Altimeter (MOLA) and images from the Mars Orbiter Camera (MOC)

PIX4615389

Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. Close-up of a large impact crater measuring 20 km in diameter. The image was obtained by the Mars Express probe on December 28, 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The image shows a large impact crater measuring 20 km in diameter. It shows a blanket of ejecta with flow forms surrounding the rim

Mars: craters and channels in Hephaestus Fossae - Mars: craters and channels in Hephaestus Fossae - Impact crateres and channel system in Hephaestus Fossae, a region on Mars located on the western flank of Elysium Mons. Close-up of a large impact crater measuring 20 km in diameter. The image was obtained by the Mars Express probe on December 28, 2007. This image of Hephaestus Fossae was obtained by Esa's Mars Express orbiter on 28 December 2007. The region is dotted with craters and channel systems and lies at about 21* North and 126* East on the Red Planet. Named after the Greek god of fire, Hephaestus Fossae extends for more than 600 km on the western flank of Elysium Mons in the Utopia Planitia region. The image shows a large impact crater measuring 20 km in diameter. It shows a blanket of ejecta with flow forms surrounding the rim

PIX4616168

Mars - View of the south pole - Mars South pole - Image of part of the southern polar cap of Mars obtained by the Mars Express probe on December 17, 2012. The bright white region of this image shows the icy cap that covers Mars' south pole, composed of frozen water and carbon dioxide. While it looks smooth in this image, at close quarters the cap is a layered mix of peaks, troughs and flat plains, and has been likened in appearance to swiss cheese. The southern cap reaches some 3 km thick in places, and is around 350 km in diameter. This icy region is permanent; in the martian winter another, thinner ice cap forms over the top of it, stretching further out across the planet and disappearing again when the weather warms up. The cap is around 150 km north of Mars' geographical south pole and Mars Express has shed light on why this ice cap is displaced. Deep impact craters - notably the Hellas Basin, the largest impact structure on the entire planet at 7 km deep and 2300 km across - funne

Mars - View of the south pole - Mars South pole - Image of part of the southern polar cap of Mars obtained by the Mars Express probe on December 17, 2012. The bright white region of this image shows the icy cap that covers Mars' south pole, composed of frozen water and carbon dioxide. While it looks smooth in this image, at close quarters the cap is a layered mix of peaks, troughs and flat plains, and has been likened in appearance to swiss cheese. The southern cap reaches some 3 km thick in places, and is around 350 km in diameter. This icy region is permanent; in the martian winter another, thinner ice cap forms over the top of it, stretching further out across the planet and disappearing again when the weather warms up. The cap is around 150 km north of Mars' geographical south pole and Mars Express has shed light on why this ice cap is displaced. Deep impact craters - notably the Hellas Basin, the largest impact structure on the entire planet at 7 km deep and 2300 km across - funne

PIX4616189

Mars surface seen by the rover Curiosity 09/2015 - Martian surface seen from the rover Curiosity 09/2015: Panorama of the surface of Mars on Mount Sharp. Mosaic of images obtained by the rover Curiosity on September 9, 2015. This composite image looking toward the higher regions of Mount Sharp was taken on September 9, 2015, by Nasa's Curiosity rover. In the foreground - about 2 miles (3 kilometers) from the rover - is a long ridge teeming with hematite, an iron oxide. Just beyond is an undulating plain rich in clay minerals. And just beyond that are a multitude of rounded buttes, all high in sulfate minerals. The changing mineralogy in these layers of Mount Sharp suggests a changing environment in early Mars, though all involve exposure to water billions of years ago. Further back in the image are striking, light-toned cliffs in rock that may have formed in drier times and now is heavily eroded by winds. The colors are adjusted so that rocks look approximately as they would if they we

Mars surface seen by the rover Curiosity 09/2015 - Martian surface seen from the rover Curiosity 09/2015: Panorama of the surface of Mars on Mount Sharp. Mosaic of images obtained by the rover Curiosity on September 9, 2015. This composite image looking toward the higher regions of Mount Sharp was taken on September 9, 2015, by Nasa's Curiosity rover. In the foreground - about 2 miles (3 kilometers) from the rover - is a long ridge teeming with hematite, an iron oxide. Just beyond is an undulating plain rich in clay minerals. And just beyond that are a multitude of rounded buttes, all high in sulfate minerals. The changing mineralogy in these layers of Mount Sharp suggests a changing environment in early Mars, though all involve exposure to water billions of years ago. Further back in the image are striking, light-toned cliffs in rock that may have formed in drier times and now is heavily eroded by winds. The colors are adjusted so that rocks look approximately as they would if they we

PIX4616695

March -View of the south pole - Mars South Pole: Image of the southern polar cap of Mars obtained by the Mars Express probe on December 17, 2012. The bright white region of this image shows the icy cap that covers Mars' south pole, composed of frozen water and carbon dioxide. The southern cap reaches some 3 km thick in places, and is around 350 km in diameter. This icy region is permanent; in the martian winter another, thinner ice cap forms over the top of it, stretching further out across the planet and disappearing again when the weather warms up. Mars Express imaged this area of March on 17 December 2012, in infrared, green and blue light, using its High Resolution Stereo Camera.

March -View of the south pole - Mars South Pole: Image of the southern polar cap of Mars obtained by the Mars Express probe on December 17, 2012. The bright white region of this image shows the icy cap that covers Mars' south pole, composed of frozen water and carbon dioxide. The southern cap reaches some 3 km thick in places, and is around 350 km in diameter. This icy region is permanent; in the martian winter another, thinner ice cap forms over the top of it, stretching further out across the planet and disappearing again when the weather warms up. Mars Express imaged this area of March on 17 December 2012, in infrared, green and blue light, using its High Resolution Stereo Camera.

PIX4616213

Rover Curiosity on Mars - Curiosity Mars rover selfie: Mars Science Laboratory (MSL), named Curiosity, is a NASA rover exploring the surface of Mars. This self-portrait is a composite of 57 images taken by the robot on January 19, 2016. This self-portrait of Nasa's Curiosity Mars rover shows the vehicle at “” Namib Dune,””” where the rover's activities included scuffing into the dune with a wheel and scooping samples of sand for laboratory analysis. The scene combines 57 images taken on Jan. 19, 2016, during the 1,228th Martian day, or sol, of Curiosity's work on Mars. The camera used for this is the Mars Hand Lens Imager (MAHLI) at the end of the rover's robotic arm. The view does not include the rover's arm. Wrist motions and turret rotations on the arm allowed MAHLI to acquire the mosaic's component images. The arm was positioned out of the shot in the images, or portions of images, that were used in this mosaic. For scale, the rover's wheels are 20 inches (50 centimeters) in diamet

Rover Curiosity on Mars - Curiosity Mars rover selfie: Mars Science Laboratory (MSL), named Curiosity, is a NASA rover exploring the surface of Mars. This self-portrait is a composite of 57 images taken by the robot on January 19, 2016. This self-portrait of Nasa's Curiosity Mars rover shows the vehicle at “” Namib Dune,””” where the rover's activities included scuffing into the dune with a wheel and scooping samples of sand for laboratory analysis. The scene combines 57 images taken on Jan. 19, 2016, during the 1,228th Martian day, or sol, of Curiosity's work on Mars. The camera used for this is the Mars Hand Lens Imager (MAHLI) at the end of the rover's robotic arm. The view does not include the rover's arm. Wrist motions and turret rotations on the arm allowed MAHLI to acquire the mosaic's component images. The arm was positioned out of the shot in the images, or portions of images, that were used in this mosaic. For scale, the rover's wheels are 20 inches (50 centimeters) in diamet

PIX4643637

Mars and Phobos - Illustration - Mars and Phobos - Illustration - Mars seen from its nearest satellite, Phobos. A view of Mars from its nearest moon, Phobo

Mars and Phobos - Illustration - Mars and Phobos - Illustration - Mars seen from its nearest satellite, Phobos. A view of Mars from its nearest moon, Phobo

Steven Hobbs

PIX4616806

March: Chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles (top) and Sacra Fossae (bottom). Kasei Valles is one of the largest Martian canal systems. The large impact crater on the right is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The upper portion of the image swath shows the eastern margin of Kasei Valles and the western margin of the Lunae Planum plateau and the adjoining Sacra Fossae. Kasei Valles is one of the largest outflow channels on Mars, spanning 3000 km, from the Chryse Planitia basi

March: Chaotic terrain between Kasei Valles and Sacra Fossae - Mars: Chaotic terrain between Kasei Valles and Sacra Fossae - Region bordering Kasei Valles (top) and Sacra Fossae (bottom). Kasei Valles is one of the largest Martian canal systems. The large impact crater on the right is 35 km in diameter. The image covering an area of 225 km by 95 km was obtained by the Mars Express probe. Mars Express flew over the boundary between Kasei Valles and Sacra Fossae and imaged the region, acquiring spectacular views of the chaotic terrain in the area. The images are centred at 12* N/285* E and have a ground resolution of about 21 m/pixel. They cover 225 x 95 km or 21.375 sq km, an area roughly half the size of the Netherlands. The upper portion of the image swath shows the eastern margin of Kasei Valles and the western margin of the Lunae Planum plateau and the adjoining Sacra Fossae. Kasei Valles is one of the largest outflow channels on Mars, spanning 3000 km, from the Chryse Planitia basi

PIX4616154

Sedimentary depots on Mars seen by Curiosity 02/2013 - Martian surface seen from the rover Curiosity 02/2013 - Sedimentary depots in the crater Gale sur Mars. Mosaic of images obtained by the rover Curiosity is his Mastcam camera on February 14, 2013. This mosaic of images from the Mast Camera (Mastcam) instrument on Nasa's Curiosity Mars rover shows a series of sedimentary deposits in the Glenelg area of Gale Crater, from a perspective in Yellowknife Bay looking toward west - northwest. Mastcam took the images for this mosaic during the 188th Martian day, or sol, of Curiosity's work on Mars (Feb. 14, 2013). The image has been white - balanced to show what the rocks would look like if ther were on Earth

Sedimentary depots on Mars seen by Curiosity 02/2013 - Martian surface seen from the rover Curiosity 02/2013 - Sedimentary depots in the crater Gale sur Mars. Mosaic of images obtained by the rover Curiosity is his Mastcam camera on February 14, 2013. This mosaic of images from the Mast Camera (Mastcam) instrument on Nasa's Curiosity Mars rover shows a series of sedimentary deposits in the Glenelg area of Gale Crater, from a perspective in Yellowknife Bay looking toward west - northwest. Mastcam took the images for this mosaic during the 188th Martian day, or sol, of Curiosity's work on Mars (Feb. 14, 2013). The image has been white - balanced to show what the rocks would look like if ther were on Earth

PIX4616681

Phobos and Mars - Illustration - Phobos and Mars - Illustration - Artist's view of Phobos, the largest of Mars's two satellites. This is how Mars and its tiny satellite Phobos might appear from a distance of about 100 miles from Phobos' surface. Phobos is over the low martian plains of Syrtis Major. Below the plains extending down to Mars' terminator and beyond is the heavily cratered Terra Sabaea. Clouds of water - ice crystals are forming at the terminator between light and dark. Looking more like a common potato than a celestial body, Phobos is actually the larger of Mars' two satellites, with a length of about 16 miles and about 11 miles across its smallest dimension. Phobos does not have enough mass for gravity to pull it into a uniform sphere like the larger satellites and planets in the Solar System. Phobos may be an asteroid long ago captured by Mars' gravity, orbiting a mere 5,800 miles above Mars' surface, making it the closest satellite to its host planet in the Solar System

Phobos and Mars - Illustration - Phobos and Mars - Illustration - Artist's view of Phobos, the largest of Mars's two satellites. This is how Mars and its tiny satellite Phobos might appear from a distance of about 100 miles from Phobos' surface. Phobos is over the low martian plains of Syrtis Major. Below the plains extending down to Mars' terminator and beyond is the heavily cratered Terra Sabaea. Clouds of water - ice crystals are forming at the terminator between light and dark. Looking more like a common potato than a celestial body, Phobos is actually the larger of Mars' two satellites, with a length of about 16 miles and about 11 miles across its smallest dimension. Phobos does not have enough mass for gravity to pull it into a uniform sphere like the larger satellites and planets in the Solar System. Phobos may be an asteroid long ago captured by Mars' gravity, orbiting a mere 5,800 miles above Mars' surface, making it the closest satellite to its host planet in the Solar System

Walter B Myers

PIX4616778

Image made from altimetric data obtained by the Mars Global Surveyor probe. The northern polar cap is mostly made up of water ice. It measures about 1100 km - Altimetric image of north pole made from MOLA instrument observations on the Mars Global Surveyor spacecraft. This image is colored according to the relative height of the surface features: North Mars pole seen by Mars Global Surveyor - Mars north pole

Image made from altimetric data obtained by the Mars Global Surveyor probe. The northern polar cap is mostly made up of water ice. It measures about 1100 km - Altimetric image of north pole made from MOLA instrument observations on the Mars Global Surveyor spacecraft. This image is colored according to the relative height of the surface features: North Mars pole seen by Mars Global Surveyor - Mars north pole

PIX4615388

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

Mars Express - Artist's View - Mars Express artist's view - The European Mars Express probe was launched on June 2, 2003 and began its observations in March early 2004. Mars Express left Earth for Mars on 2 June 2003 when the positions of the two planets made for the shortest possible route, a condition that occurs once every twenty - six months. The european spaceprobe began its March observations in 2004

D. Ducros

PIX4606649

Permanent station project between Mars and the Earth - Artist view - Mars Cycler - Artist view - Artist view of the Mars Cycler project, a space station placed in cylindrical orbit between Mars and Earth; this project defended by Edwin Aldrin would make a permanent connection between the two planets. A Mars cycler is a permanently orbiting vehicle with a path that alternately brings it near Earth and Mars. Once a cycler has been accelerated into orbit it continues on its own momentum, going back and forth between the two planets, only requiring propellant for occasional course adjustments. A one-way trip between Earth and Mars involves six to eight months of space travel, therefore a large and well-equipped Mars cycler would offer space explorers, and possibly even space tourists, better accommodations for these long journeys. Smaller spacecraft would ferry travelers between the planets and the cycler. A Mars cycler is a permanently orbiting vehicle with a path that alternately brings

Permanent station project between Mars and the Earth - Artist view - Mars Cycler - Artist view - Artist view of the Mars Cycler project, a space station placed in cylindrical orbit between Mars and Earth; this project defended by Edwin Aldrin would make a permanent connection between the two planets. A Mars cycler is a permanently orbiting vehicle with a path that alternately brings it near Earth and Mars. Once a cycler has been accelerated into orbit it continues on its own momentum, going back and forth between the two planets, only requiring propellant for occasional course adjustments. A one-way trip between Earth and Mars involves six to eight months of space travel, therefore a large and well-equipped Mars cycler would offer space explorers, and possibly even space tourists, better accommodations for these long journeys. Smaller spacecraft would ferry travelers between the planets and the cycler. A Mars cycler is a permanently orbiting vehicle with a path that alternately brings

Walter B Myers

PIX4639516

Permanent station project between Mars and the Earth-Vue d'artiste - Mars Cycler - Artist view - Artist view of the Mars Cycler project, four space stations placed in cylindrical orbit between Mars and the Earth; this project defended by Edwin Aldrin will make it possible to make a permanent link between the two planets. Artist's concept of the Buzz Aldrin Mars Cycler. A Mars cycler is a space station project that is on a permanent orbit between the Mars and Earth

Permanent station project between Mars and the Earth-Vue d'artiste - Mars Cycler - Artist view - Artist view of the Mars Cycler project, four space stations placed in cylindrical orbit between Mars and the Earth; this project defended by Edwin Aldrin will make it possible to make a permanent link between the two planets. Artist's concept of the Buzz Aldrin Mars Cycler. A Mars cycler is a space station project that is on a permanent orbit between the Mars and Earth

Dixon, Don (b.1951)

PIX4639479

Mars - View of the north pole - Mars north pole - Image of a portion of the northern polar cap of Mars obtained by the Mars Express probe on May 17, 2010. This image was acquired by the Mars Express High - Resolution Stereo Camera on 17 May 2010 and shows a part of the northern polar region of Mars at the northern hemisphere summer solstice. The polar ice deposits follow the seasonal cycles. Studies made by Mars Express's OMEGA instrument shows that the cap is covered by frozen water and carbon dioxide ice in winter and spring but by this point in the martian year all of the carbon dioxide ice has warmed and evaporated into the planet's atmosphere. Only water ice is left behind, which shows up as bright white areas in this picture. From these layers, large bursts of water vapour are occasionally released into the atmosphere. In winter, part of the atmosphere recondenses as frost and snow on the northern cap. These seasonal deposits can extend as far south as 45* N latitude and be up to

Mars - View of the north pole - Mars north pole - Image of a portion of the northern polar cap of Mars obtained by the Mars Express probe on May 17, 2010. This image was acquired by the Mars Express High - Resolution Stereo Camera on 17 May 2010 and shows a part of the northern polar region of Mars at the northern hemisphere summer solstice. The polar ice deposits follow the seasonal cycles. Studies made by Mars Express's OMEGA instrument shows that the cap is covered by frozen water and carbon dioxide ice in winter and spring but by this point in the martian year all of the carbon dioxide ice has warmed and evaporated into the planet's atmosphere. Only water ice is left behind, which shows up as bright white areas in this picture. From these layers, large bursts of water vapour are occasionally released into the atmosphere. In winter, part of the atmosphere recondenses as frost and snow on the northern cap. These seasonal deposits can extend as far south as 45* N latitude and be up to

PIX4616313

The probe Mars 96 - Artist view - Mars 96 spacecraft - Artist view - Scenario of the mission of the sovietic probe Mars 96. In addition to its observations in Martian orbit, this probe was to launch two stations and two penetrators on Martian soil. Launched in 1996, the probe could not leave Earth orbit and disintegrate. Artwork showing the mission sequence of soviet March 96 spacecraft. Two surface stations and two penetrators should be deployed on the martian surface. Launched in 1996, a rocket failure happened and the probe was desintegrated in the Earth atmosphere

The probe Mars 96 - Artist view - Mars 96 spacecraft - Artist view - Scenario of the mission of the sovietic probe Mars 96. In addition to its observations in Martian orbit, this probe was to launch two stations and two penetrators on Martian soil. Launched in 1996, the probe could not leave Earth orbit and disintegrate. Artwork showing the mission sequence of soviet March 96 spacecraft. Two surface stations and two penetrators should be deployed on the martian surface. Launched in 1996, a rocket failure happened and the probe was desintegrated in the Earth atmosphere

D. Ducros

PIX4606457

Permanent station between Mars and Earth - Artist view - Mars lander departs cycler - Artist view - A landing ship (top left) leaves the Mars Cycler to land on the red planet. Mars Cycler is a space station placed in orbit between Mars and Earth whose trajectory would alternate between Mars and Earth. Once positioned in orbit, this gravitational assistance vessel would use very little fuel. This project would make a permanent link between the two planets. A manned Mars lander/return vehicle, upper left, disembarks from a Mars cycler for the surface of Mars. A Mars cycler is a permanently orbiting vehicle with a path that alternately brings it near Earth and Mars. Once a cycler has been accelerated into orbit it continues on its own momentum, going back and forth between the two planets, only requiring propellant for occasional course adjustments. A one-way trip between Earth and Mars involves six to eight months of space travel, therefore a large and well-equipped Mars cycler would off

Permanent station between Mars and Earth - Artist view - Mars lander departs cycler - Artist view - A landing ship (top left) leaves the Mars Cycler to land on the red planet. Mars Cycler is a space station placed in orbit between Mars and Earth whose trajectory would alternate between Mars and Earth. Once positioned in orbit, this gravitational assistance vessel would use very little fuel. This project would make a permanent link between the two planets. A manned Mars lander/return vehicle, upper left, disembarks from a Mars cycler for the surface of Mars. A Mars cycler is a permanently orbiting vehicle with a path that alternately brings it near Earth and Mars. Once a cycler has been accelerated into orbit it continues on its own momentum, going back and forth between the two planets, only requiring propellant for occasional course adjustments. A one-way trip between Earth and Mars involves six to eight months of space travel, therefore a large and well-equipped Mars cycler would off

Walter B Myers

PIX4639544

The probe Mars 96 - Artist view - Mars 96 spacecraft - Artist view - Sequence of landing of a penetrator. In addition to its observations in Martian orbit, this probe was to launch two stations and two penetrators on Martian soil. Launched in 1996, the probe could not leave Earth orbit and disintegrate. Penetrator landing sequence. Artwork showing the mission sequence of soviet March 96 spacecraft. Two surface stations and two penetrators should be deployed on the martian surface. Launched in 1996, a rocket failure happened and the probe was desintegrated in the Earth atmosphere

The probe Mars 96 - Artist view - Mars 96 spacecraft - Artist view - Sequence of landing of a penetrator. In addition to its observations in Martian orbit, this probe was to launch two stations and two penetrators on Martian soil. Launched in 1996, the probe could not leave Earth orbit and disintegrate. Penetrator landing sequence. Artwork showing the mission sequence of soviet March 96 spacecraft. Two surface stations and two penetrators should be deployed on the martian surface. Launched in 1996, a rocket failure happened and the probe was desintegrated in the Earth atmosphere

D. Ducros

PIX4606471

March: Volcano Olympus Mons - False colors - Mars: volcano Olympus Mons - Altimetric data obtained by the Mars Express probe. The Olympus Mons volcano is 600 km in diameter and 26 km above the plains. This is a mosaic of Olympus Mons, the highest volcano on Mars, which towers 26 km above the surrounding plains. The image covers an area of approximately 600,000 sq km and is color - coded according to height

March: Volcano Olympus Mons - False colors - Mars: volcano Olympus Mons - Altimetric data obtained by the Mars Express probe. The Olympus Mons volcano is 600 km in diameter and 26 km above the plains. This is a mosaic of Olympus Mons, the highest volcano on Mars, which towers 26 km above the surrounding plains. The image covers an area of approximately 600,000 sq km and is color - coded according to height

PIX4615892

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