Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment (HiRISE) camera snapped this shot of Phoenix hanging from its parachute during its descent to the Martian surface....[More]
LOOK OUT BELOW:
Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment (HiRISE) camera snapped this shot of Phoenix hanging from its parachute during its descent to the Martian surface. In the background is a crater measuring 10 kilometers (six miles) in diameter. Although it appears that Phoenix is descending into the crater, informally known as "Heimdall," the falling probe is actually about 20 kilometers (12 miles) in front of it.
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona
GOTCHA: This color image from Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment (HiRISE) camera shows the Phoenix lander with its solar panels deployed on the Mars surface. [Link to this slide] NASA/JPL-Caltech/University of Arizona
BIOBARRIER:
In one of the few glitches so far for NASA's Phoenix Mars Lander mission, a shiny, protective film failed to completely unwrap from around the elbow joint of the craft's 7.7-foot robotic arm, shown here in its stowed configuration on days one [ left ] and two [ right ] of the mission....[More]
BIOBARRIER:
In one of the few glitches so far for NASA's Phoenix Mars Lander mission, a shiny, protective film failed to completely unwrap from around the elbow joint of the craft's 7.7-foot robotic arm, shown here in its stowed configuration on days one [left] and two [right] of the mission. The image shows the gradual peeling away of the protective biobarrier, put in place to prevent Earthly bacteria from contaminating the arm during the final stages before launch.
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona
SOFT LANDING: NASA's Phoenix Mars Lander slid a short distance when it alighted on the pebbly arctic terrain of Mars this Sunday, as seen in this close-up image of the probe's footpad. [Link to this slide] NASA/JPL-Caltech/University of Arizona/Texas A&M University
CRACKING UP:
A polygonal pattern in the ground near Phoenix Mars Lander, shown here in approximate color based on violet and infrared light, suggests that subsurface ice has recently undergone seasonal thawing and refreezing....[More]
CRACKING UP:
A polygonal pattern in the ground near Phoenix Mars Lander, shown here in approximate color based on violet and infrared light, suggests that subsurface ice has recently undergone seasonal thawing and refreezing.
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona/Texas A&M University
MARTIAN COLOR WHEEL:
Three color targets—similar to what you might use in selecting a paint color for your walls—used to add hues to images [ bottom ] sent back by the Surface Stereo Imager (SSI) aboard NASA's Phoenix Mars Lander....[More]
MARTIAN COLOR WHEEL:
Three color targets—similar to what you might use in selecting a paint color for your walls—used to add hues to images [bottom] sent back by the Surface Stereo Imager (SSI) aboard NASA's Phoenix Mars Lander. Visible in two of the images [top] are sand grains two to three millimeters in size that were likely lifted to the Phoenix deck during landing. Each of the large color chips contains a strong magnet to protect the interior material from Mars' magnetic dust.
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona/Texas A&M University
MARS TIME CAPSULE:
An American flag and a mini-DVD on the deck of Phoenix Mars Lander. The mini-DVD from the Planetary Society contains a message to future Martian explorers, science fiction stories and art inspired by the Red Planet as well as the names of more than a quarter-million earthlings....[More]
MARS TIME CAPSULE:
An American flag and a mini-DVD on the deck of Phoenix Mars Lander. The mini-DVD from the Planetary Society contains a message to future Martian explorers, science fiction stories and art inspired by the Red Planet as well as the names of more than a quarter-million earthlings. No social security numbers, we hope.
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona
FISH-EYE VIEW:
This mosaic, forming a 360-degree polar projection of the terrain surrounding the Phoenix Mars Lander, was generated from images collected by the probe's Surface Stereo Imager (SSI) instrument during the first three days of the mission....[More]
FISH-EYE VIEW:
This mosaic, forming a 360-degree polar projection of the terrain surrounding the Phoenix Mars Lander, was generated from images collected by the probe's Surface Stereo Imager (SSI) instrument during the first three days of the mission. (Note the changing daylight.) Clockwise from 12 o'clock (due north) are a pair of solar collectors (4 and 8 o'clock) and a mast sporting three temperature sensors (7:30 o'clock). [Updated 5/30]
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona/Texas A&M University
PHOENIX "WORKSPACE":
This terrain model showing the workspace, or area accessible by, Phoenix's Robotic Arm has been color coded by depth (red = low; blue = high) with a model of the lander for context....[More]
PHOENIX "WORKSPACE":
This terrain model showing the workspace, or area accessible by, Phoenix's Robotic Arm has been color coded by depth (red = low; blue = high) with a model of the lander for context. Color-coding was derived from the depth perception feature on the craft's Surface Stereo Imager (SSI).
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona/Texas A&M University/NASA Ames
VERTICAL HORIZON:
This approximate-color view of the terrain northwest of Phoenix Mars Lander, obtained by the craft's Surface Stereo Imager (SSI), shows polygonal cracking thought to represent seasonal thawing and freezing of subsurface ice....[More]
VERTICAL HORIZON:
This approximate-color view of the terrain northwest of Phoenix Mars Lander, obtained by the craft's Surface Stereo Imager (SSI), shows polygonal cracking thought to represent seasonal thawing and freezing of subsurface ice.
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona/Texas A&M University
FIRST THINGS FIRST:
This image—one of the first captured by NASA's Phoenix Mars Lander—shows the vast plains of the northern polar region of Mars. NASA researchers believe the network of polygon-shaped cracks, seen widely in Martian high latitudes and also observed in Earthly permafrost terrains, results from seasonal contraction and expansion of surface ice....[More]
FIRST THINGS FIRST:
This image—one of the first captured by NASA's Phoenix Mars Lander—shows the vast plains of the northern polar region of Mars. NASA researchers believe the network of polygon-shaped cracks, seen widely in Martian high latitudes and also observed in Earthly permafrost terrains, results from seasonal contraction and expansion of surface ice.
[Less]
[Link to this slide]
NASA/JPL-Caltech/University of Arizona/Texas A&M University
YES! Send me a free issue of Scientific American with no obligation to continue the subscription. If I like it, I will be billed for the one-year subscription.
Comments
Add Comment