The US space agency NASA has recently pieced together a panoramic view from the camera on NASA's Mars Exploration Rover Opportunity, calling it the "next best thing to being" on the Red Planet.
A full-circle scene combining
817 images taken by the panoramic camera (Pancam) on NASA's Mars
Exploration Rover Opportunity. The US space agency NASA is calling it
the "next best thing to being" on the Red Planet.
A TextureCam analysis of a Mars image is able to distinguish rocks from soil.
A Martian dust devil roughly 12
miles (20 kilometers) high was captured winding its way along the
Amazonis Planitia region of northern Mars on March 14, 2012 by NASA's
Mars Reconnaissance Orbiter.
This image mosaic taken by the
Mars Exploration Rover Spirit's panoramic camera shows a new slice of
martian real estate southwest of the rover's landing site. The landscape
shows little variation in local topography, though a narrow peak only
seven to eight kilometres away is visible on the horizon. A circular
depression, similar to the one dubbed Sleepy Hollow, can be seen in the
foreground. Compared to the Viking and Pathfinder landing sites, the
terrain at Gusev Crater, Spirit's landing site, is flat and speckled
with a sparse array of rocks. The picture was released by the Jet
Propulsion Laboratory in Pasadena, California Janaury 10, 2004.
A view of Eberswalde crater
containing a rare case of a martian delta, with well preserved channels
which fed the lake in the crater, located in the southern highlands of
Mars, seen in this handout photograph acquired by Mars Express at
approximately 25S / 326E during orbit 7208 on August 15, 2009 and
released September 2, 2011. The delta deposits and channels together
provide a clear indication of liquid surface water during the early
history of Mars. The images have a ground resolution of about 22 m per
pixel. Reuters
A close-up of the sunset on Sol
24 as seen by the Imager for Mars Pathfinder was released by the Jet
Propulsion Labratory August 27. The red sky in the background and the
blue around the Sun are approximately as they would appear to the human
eye but the color of the Sun itself is not correct -- the Sun was
overexposed in each of the 3 color images that were used to make the
picture. The true color of the Sun itself may be near white or slightly
bluish.
Mars' Victoria Crater at
Meridiani Planum is seen in this image taken by NASA's High Resolution
Imaging Science Experiment (HiRISE) camera in this picture released
October 6, 2006. NASA officials gave conflicting views during a meeting
of space scientists on December 13, 2006, on whether the construction
of a moon base will mark a great leap in planning for a manned mission
to Mars or prove a wasteful diversion of funds.
A portion of the west rim of
Endeavour crater sweeps southward in this color view from NASA's Mars
Exploration Rover Opportunity released by NASA August 10, 2011. This
crater has a diameter of about 14 miles (22 km). This view combines
exposures taken by Opportunity's panoramic camera (Pancam) of the
rover's work on Mars August 6, 2011. Opportunity arrived at the rim
during its next drive on August 9, 2011. Endeavour crater has been the
rover team's destination for Opportunity since the rover finished
exploring Victoria crater in August 2008. Endeavour offers access to
older geological deposits than any Opportunity has seen before. The
lighter-toned rocks closer to the rover in this view are similar to the
rocks Opportunity has driven over for most of the mission. However, the
darker-toned and rougher rocks just beyond that might be a different
type for Opportunity to investigate. The ground in the foreground is
covered with iron-rich spherules, nicknamed "blueberries," which
Opportunity has observed frequently since the first days after landing.
They are about 0.2 inch (5 millimeters) or more in diameter.
A handout of the European Space
Agency ESA shows a visualisation of Mars, created from spacecraft
imagery. ESA's first mission to the Red Planet is Mars Express. It
comprises an orbiter carrying seven scientific instruments to probe the
planet's atmosphere, structure and geology, including a search for
evidence of hidden water. The main spacecraft will also release the UK's
small Beagle 2 lander to gather and test rock and soil samples on the
surface. British space probe Beagle 2 failed to broadcast a signal on
December 25, 2003, to confirm it had landed on Mars, but scientists said
they were waiting for a second contact opportunity later on Thursday.
In
this image released January 19, 2005, NASA's Mars Exploration Rover
"Opportunity": has found an iron meteorite on Mars, the first meteorite
of any type ever identified on another planet. The pitted,
basketball-size object is mostly made of iron and nickel. This composite
combines images taken through the panoramic camera's 600-nanometer
(red), 530-nanometer (green), and 480-nanometer (blue) filters.
A cliff, up to 4,000 m high,
located in the eastern part of Echus Chasma, one of the largest water
source regions on Mars, is seen in this image taken by the
High-Resolution Stereo Camera (HRSC) on board ESAĆs Mars Express and
made available July 14, 2008. Echus Chasma is the source region of Kasei
Valles which extends 3,000 km to the north.
The High-Resolution Stereo
Camera (HRSC) on board ESA?s Mars Express has returned images of Echus
Chasma in this image made available on July 14, 2008. Echus Chasma is an
approximately 100 km long and 10 km wide incision in the Lunae Planum
high plateau north of Valles Marineris, the ?Grand Canyon? of Mars.
One of the first colour images
from the Phoenix Mars Lander shows the surface of Mars after the Phoenix
Mars Lander spacecraft landed successfully in the first-ever touchdown
near Mars' north pole
An
artist's conception shows what NASA's Mars Reconnaissance Orbiter has
revealed, vast Martian glaciers of water ice under protective blankets
of rocky debris at much lower latitudes than any ice previously
identified on the Red Planet. Scientists analyzed data from the
spacecraft's ground-penetrating radar and report in the November 21,
2008 issue of the journal Science that buried glaciers extend for dozens
of miles from edges of mountains or cliffs.