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High Resolution Imaging Science Experiment (HiRISE) of Jet Propulsion Laboratory (JPL)
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Mars Reconnaissance Orbiter
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| title |
Mars Reconnaissance Orbiter Takes Its First Look |
| date |
03.24.2006 |
| description |
This view shows a full-resolution portion of the first image of Mars taken by the High Resolution Imaging Science Experiment camera (HiRISE) on NASA's Mars Reconnaissance Orbiter. The spacecraft, launched Aug. 12, 2005, began orbiting Mars on March 10, 2006. The image is of an area in Mars' mid-latitude southern highlands. HiRISE took this first test image from orbit on March 24, 2006, from an altitude of 2,489 kilometers (1,547 miles), achieving a resolution of 2.49 meters (98 inches) per pixel, or picture element. The smallest objects of discernable shape are about three pixels across. An image acquired at this latitude during the Mars Reconnaissance Orbiter's main science phase, beginning in fall 2006, would be taken from an altitude of about 280 kilometers (174 miles) and have a resolution of 28 centimeters (11 inches) per pixel. This view covers an area about 4.5 by 2.1 kilometers (1.6 by 1.3 miles), a subset of the broader image. The quality of this test image is spectacular, with no hint to the eye of any smear or blurring. A high signal-to-noise ratio reveals fine details even in the shadows. Image Credit: NASA/JPL/University of Arizona |
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Victoria Crater' at Meridian
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| title |
Victoria Crater' at Meridiani Planum |
| date |
10.06.2006 |
| description |
This image from the High Resolution Imaging Science Experiment on NASA's Mars Reconnaissance Orbiter shows "Victoria crater," an impact crater at Meridiani Planum, near the equator of Mars. The crater is approximately 800 meters (half a mile) in diameter. It has a distinctive scalloped shape to its rim, caused by erosion and downhill movement of crater wall material. Layered sedimentary rocks are exposed along the inner wall of the crater, and boulders that have fallen from the crater wall are visible on the crater floor. The floor of the crater is occupied by a striking field of sand dunes. Since January 2004, the Mars Exploration Rover Opportunity has been operating at Meridiani Planum. Five days before this image was taken, Opportunity arrived at the rim of Victoria crater, after a drive of more than 9 kilometers (over 5 miles). The rover can be seen in this image, at roughly the "ten o'clock" position along the rim of the crater. This view is a portion of an image taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard the Mars Reconnaissance Orbiter spacecraft on Oct. 3, 2006. The complete image is centered at minus7.8 degrees latitude, 279.5 degrees East longitude. The range to the target site was 297 kilometers (185.6 miles). At this distance the image scale is 29.7 centimeters (12 inches) per pixel (with 1 x 1 binning) so objects about 89 centimeters (35 inches) across are resolved. The image shown here has been map-projected to 25 centimeters (10 inches) per pixel and north is up. The image was taken at a local Mars time of 3:30 PM and the scene is illuminated from the west with a solar incidence angle of 59.7 degrees, thus the sun was about 30.3 degrees above the horizon. At a solar longitude of 113.6 degrees, the season on Mars is northern summer. This is an enhanced-color view generated from images acquired by the HiRISE camera using its red filter and blue-green filter. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mroor http://HiRISE.lpl.arizona.edu. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov. JPL, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace & Technologies Corporation and is operated by the University of Arizona. Image Credit: NASA/JPL/UA |
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Gullies with Characteristics
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Gullies with Characteristics of Water-Carved Channels |
| description |
False-color image of gully channels in a crater in the southern highlands of Mars, taken by the High Resolution Imaging Science Experiment (HiRISE) camera on the Mars Reconnaissance Orbiter. The gullies emanating from the rocky cliffs near the crater's rim (upper left) show meandering and braided patterns typical of water-carved channels. North is approximately up and illumination is from the left, scale, 26 centimeters per pixel. A link to the full HiRISE image that includes this view is online at http://hirise.lpl.arizona.edu/PSP_003583_1425 Credit: NASA/JPL/University of Arizona |
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Gullies in Sirenum Terra, Ma
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| title |
Gullies in Sirenum Terra, Mars |
| date |
10.03.2006 |
| description |
This enhanced-color view shows gullies in an unnamed crater in the Terra Sirenum region of Mars. It is a sub-image from a larger view imaged by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter on Oct. 3, 2006. This scene is about 254 meters (about 830 feet) wide. The upper and left regions of this scene are in shadow, yet color variations are still apparent. The high signal to noise ratio of the HiRISE camera allows for colors to be distinguished in shadows. This allows dark features to be identified as true albedo features versus topographical features. Image credit: NASA/JPL/Univ. of Arizona |
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Mars: The View from HiRISE
| Title |
Mars: The View from HiRISE |
| Explanation |
HiRISE [ http://hiroc.lpl.arizona.edu/HiROC/ ] - the High Resolution Imaging Science Experiment - rides on the Mars Reconnaissance Orbiter (MRO [ http://marsprogram.jpl.nasa.gov/mro/ ])spacecraft just arrived in Mars orbit on March 10. This sharp view of the martian [ http://www.google.com/mars/ ] surface from the HiRISE camera includes image data [ http://photojournal.jpl.nasa.gov/catalog/PIA08014 ] with a full resolution of about 2.5 meters per pixel - recorded from a range of 2,500 kilometers. In the coming months, MRO's [ http://marsprogram.jpl.nasa.gov/mro/mission/ rightnow.html ] orbit will be circularized through repeated passages into Mars' outer atmosphere, a process known as aerobraking [ http://marsprogram.jpl.nasa.gov/mro/mission/ tl_aerobraking.html ], shrinking its orbit to an altitude of only 280 kilometers. At that distance, the HiRISE experiment should be able to image the Red Planet's [ http://www.uapress.arizona.edu/onlinebks/mars/ contents.htm ] surface at a resolution of 28 centi [ http://lamar.colostate.edu/~hillger/ common.html ]meters (11 inches) per pixel. In this first color image [ http://hiroc.lpl.arizona.edu/first_images/all/ AEB_000001_0000.shtml ], the false colors represent HiRISE's visible and infrared imaging data combined. The picture is nearly 24 kilometers wide and covers an area in the Bosporos Planum region of southern Mars. |
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Mars Rover at Victoria Crate
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| Title |
Mars Rover at Victoria Crater Imaged from Orbit |
| Explanation |
An unusual spot has been found on Mars that scientists believe is not natural in origin. The spot appears mobile and is now hypothesized to be a robot [ http://en.wikipedia.org/wiki/Robot ] created by an intelligent species [ http://www.guardian.co.uk/life/feature/story/0,13026,989714,00.html ] alien to Mars. In fact, the spot appears to be NASA's robotic Opportunity rover currently rolling across Mars. The ability to see the Martian rover from orbit has recently been demonstrated by the High Resolution Imaging Science Experiment [ http://hirise.lpl.arizona.edu/ ] on NASA's Mars Reconnaissance Orbiter [ http://en.wikipedia.org/wiki/Mars_Reconnaissance_Orbiter ] (MRO). The new spacecraft achieved orbit around Mars in 2006 March. Last week, MRO imaged the location of Victoria Crater [ http://antwrp.gsfc.nasa.gov/apod/ap061002.html ] and the rover Opportunity [ http://antwrp.gsfc.nasa.gov/apod/ap051214.html ] that had just arrived there. In the above image [ http://photojournal.jpl.nasa.gov/catalog/PIA08816 ] at spectacularly high resolution [ http://antwrp.gsfc.nasa.gov/apod/ap060410.html ], objects about one meter in size are resolved, and this includes the rolling rover. Such images may help scientists better determine if any safe path exists for Opportunity to enter large crater. In the inset image [ http://photojournal.jpl.nasa.gov/catalog/PIA08813 ] on the upper left, the whole of Victoria Crater [ http://en.wikipedia.org/wiki/Victoria_crater ] was also imaged by MRO. |
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Spirit Rover on Mars Imaged
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Spirit Rover on Mars Imaged from Orbit |
| Explanation |
If you have the right equipment, you can see the Spirit rover currently rolling across Mars. The right equipment, however, is currently limited to the High Resolution Imaging Science Experiment [ http://hirise.lpl.arizona.edu/ ] onboard the Mars Reconnaissance Orbiter [ http://en.wikipedia.org/wiki/Mars_Reconnaissance_Orbiter ] (MRO). MRO arrived at Mars [ http://www.nineplanets.org/mars.html ] in March and just started science observations of the red planet last month. Visible in the above spectacularly high resolution image [ http://photojournal.jpl.nasa.gov/catalog/PIA01879 ] is the Spirit rover [ http://antwrp.gsfc.nasa.gov/apod/ap051214.html ] in the Columbia Hills [ http://antwrp.gsfc.nasa.gov/apod/ap040628.html ] of Mars. Objects as small as one meter are resolved. Also visible are the tracks made by the robot explorer and a large plateau of layered rock dubbed Home Plate [ http://www.marsdaily.com/reports/Home_Plate_Continues_To_Mystify_Mars_Rover_Team.html ]. MRO will continue to image the red planet [ http://antwrp.gsfc.nasa.gov/apod/ap980608.html ] in unprecedented detail, creating images that will likely be important in better understanding the geology and weather on Mars, as well as indicating good candidate landing sites for future missions [ http://mars.jpl.nasa.gov/missions/future/msl.html ] to Mars. |
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White Ridges on Mars
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White Ridges on Mars |
| Explanation |
What created these white ridges on Mars? The images [ http://photojournal.jpl.nasa.gov/catalog/PIA09189 ] showing the white ridges, including some of the highest resolution images ever taken from Martian orbit, were recorded last year by the Mars Reconnaissance Orbiter [ http://en.wikipedia.org/wiki/Mars_Reconnaissance_Orbiter ] (MRO). A current leading hypothesis [ http://www.jpl.nasa.gov/news/news.cfm?release=2007-017 ] is that the white ridges formed as water flowed through underground cracks and bleached [ http://en.wikipedia.org/wiki/Bleaching ] and hardened the edges of surrounding rocks. Over millions of years, surface winds eroded the darker rock leaving the raised white ridges. Such water-created light-colored markings are well known here on Earth [ http://antwrp.gsfc.nasa.gov/apod/ap050102.html ]. The hypothesis is particularly interesting as underground water could have helped to support microbial life [ http://www.microbeworld.org/microbes/ ] on the red world. The above image resolves surface features as small as one meter across in Candor Chasma [ http://antwrp.gsfc.nasa.gov/apod/ap030218.html ] region of huge Valles Marineris [ http://antwrp.gsfc.nasa.gov/apod/ap060730.html ] on Mars [ http://www.nineplanets.org/mars.html ]. |
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A Hole in Mars
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A Hole in Mars |
| Explanation |
Black spots have been discovered on Mars that are so dark that nothing inside can be seen. Quite possibly, the spots [ http://www.planetary.org/blog/article/00000984/ ] are entrances to deep underground caves capable of protecting Martian life [ http://mars.jpl.nasa.gov/life/ ], were it to exist. The unusual hole pictured above was found on the slopes of the giant Martian volcano Arsia Mons [ http://en.wikipedia.org/wiki/Arsia_Mons ]. The above image was captured three weeks ago by the HiRISE [ http://en.wikipedia.org/wiki/HiRISE ] instrument onboard the Mars Reconnaissance Orbiter [ http://mars.jpl.nasa.gov/mro/overview/ ] currently circling Mars [ http://antwrp.gsfc.nasa.gov/apod/ap050209.html ]. The holes were originally identified [ http://www.lpi.usra.edu/meetings/lpsc2007/pdf/1371.pdf ] on lower resolution images from the Mars Odyssey [ http://mars.jpl.nasa.gov/odyssey/overview/ ] spacecraft, The above hole is about the size of a football field [ http://en.wikipedia.org/wiki/Football_pitch ] and is so deep that it is completely unilluminated [ http://antwrp.gsfc.nasa.gov/apod/ap060409.html ] by the Sun. Such holes and underground caves [ http://en.wikipedia.org/wiki/Cave ] might be prime targets for future spacecraft [ http://mars.jpl.nasa.gov/missions/future/ ], robots [ http://www-robotics.jpl.nasa.gov/ ], and even the next generation of human interplanetary explorers [ http://en.wikipedia.org/wiki/The_Martian_Chronicles ]. |
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A Hole in Mars Close Up
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A Hole in Mars Close Up |
| Explanation |
In a close-up [ http://hirise.lpl.arizona.edu/PSP_004847_1745 ] from the HiRISE [ http://hirise.lpl.arizona.edu/index.php ] instrument onboard the Mars Reconnaissance Orbiter, this mysterious dark pit, about 150 meters across, lies on the north slope of ancient martian [ http://www.lukew.com/marsgeo/index.html ] volcano Arsia Mons [ http://photojournal.jpl.nasa.gov/catalog/PIA02337 ]. Lacking raised rims and other impact crater characteristics, this pit and others like it [ http://mars.jpl.nasa.gov/odyssey/newsroom/pressreleases/ 20070921a.html ] were originally identified in visible light and infrared images from the Mars Odyssey and Mars Global Surveyor spacecraft. While the visible light images showed only darkness within [ http://antwrp.gsfc.nasa.gov/apod/ap070528.html ], infrared thermal signatures [ http://www.nasa.gov/mission_pages/odyssey/images/ cave4.html ] indicated that the openings penetrated deep under the martian surface and perhaps were skylights to underground caverns. In this later image, the pit wall is partially illuminated by sunlight and seen to be nearly vertical, though the bottom, at least 78 meters below, is still not visible. The dark martian pits are thought to be related to collapse pits [ http://hvo.wr.usgs.gov/gallery/kilauea/erz/ devilsthroat.html ] in the lava flow, similar [ http://hvo.wr.usgs.gov/gallery/kilauea/erz/ upper/30424305-044_large.jpg ] to Hawaiian volcano pit craters [ http://volcanoes.usgs.gov/Products/Pglossary/ PitCrater.html ]. |
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Mars Rover Races to Survive
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Mars Rover Races to Survive |
| Explanation |
The Martian rover Spirit is now in the race of its life. The rolling robot [ http://antwrp.gsfc.nasa.gov/apod/ap051214.html ] is trying to reach an outpost to spend the winter, but it keeps getting bogged down [ http://space.newscientist.com/article/dn13001-mars-rover-spirit-escapes-from-sandy-dungeon.html ] in soft sand on Mars [ http://www.nasa.gov/vision/earth/technologies/31jan_sandsofmars.html ]. Earth scientists hope that Spirit [ http://en.wikipedia.org/wiki/Spirit_rover ] can reach [ http://space.newscientist.com/article/dn12884-mars-rover-spirit-to-head-north-for-the-winter.html ] a slope on the northern edge of the unusual feature dubbed Home Plate [ http://en.wikipedia.org/wiki/Home_Plate_%28Mars%29 ], before the end of this month when northern winter [ http://antwrp.gsfc.nasa.gov/apod/ap041130.html ] will be phasing in on Mars [ http://en.wikipedia.org/wiki/Mars ]. Reaching this slope will likely allow the rover [ http://antwrp.gsfc.nasa.gov/apod/ap040127.html ] to tilt enough toward the Sun to create a needed increase [ http://antwrp.gsfc.nasa.gov/apod/ap060406.html ] in the efficiency of its energy-absorbing solar panels [ http://www.wisegeek.com/how-do-solar-panels-work.htm ]. This map [ http://marsrovers.jpl.nasa.gov/gallery/press/spirit/20071129a.html ] shows the path of Spirit from July 2004 until just last month. |
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Terrain Type for Phoenix Lan
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| title |
Terrain Type for Phoenix Landing |
| Description |
This view shows the texture of the ground in the area favored as a landing site for NASA's Phoenix Mars Lander mission. The pattern resembles permafrost terrain on Earth, where cycles of thawing and freezing cause cracking into polygon shapes. This is a subframe, covering a patch of ground about 700 meters (2,300 feet) across, from a larger image taken by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter on Nov. 11, 2006. The full image, catalogued as PSP_001418_2495 [ http://hirise.lpl.arizona.edu/PSP_001418_2495 ], shows an area of far-northern Mars centered at 69.2 degrees north latitude, 234.2 degrees east longitude. |
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Mars Reconnaissance Orbiter
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Mars Reconnaissance Orbiter Adjusts Angle of Orbit |
| Description |
This artist's concept of NASA's Mars Reconnaissance Orbiter features the spacecraft's main bus facing down, toward the red planet. The large silver circular feature above the spacecraft bus is the high-gain antenna, the spacecraft's main means of communicating with Earth. The long, thin pole behind the bus is the antenna for the Shallow Subsurface Radar instrument (SHARAD). Seeking liquid or frozen water, this instrument will probe the subsurface using radar waves at frequencies of 15 to 25 megahertz, "seeing" in the first few hundred feet (up to 1 kilometer) of Mars' crust. The large instrument covered in black thermal blanketing in the center is the High Resolution Imaging Science Experiment camera (HiRISE). It will provide the highest-resolution images ever taken from Mars orbit. The Electra telecommunications package is the gold-colored instrument directly left of the high-resolution camera. It will act as a communications relay and navigation aid for Mars spacecraft. To the right of the high-resolution camera is the Context Imager (CTX). Credit: NASA/JPL |
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First Context Camera Image o
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First Context Camera Image of Mars |
| Description |
), the second image obtained by the Context Camera, is much longer than the first: 260 kilometers (162 miles) at its widest point and about 122 kilometers (76 miles) at its narrowest, some 1,590 kilometers (988 miles) to the south. It covers an area of about 40,000 square kilometers (about 15,400 square miles). The change in width reflects a change in altitude of the Mars Reconnaissance Orbiter as it descended southward toward the orbit's closest point to the planet. The picture is shown here at one-third its original scale because the file size is large. Figure 4: image below ( Full Res GIF 7 MB ) contains the northernmost portion of the second Context Camera image, reproduced at one-half its original scale (because of its large file size). The white box [ http://photojournal.jpl.nasa.gov/catalog/PIA08060 ] outlines the location of the first image from the orbiter's High Resolution Imaging Science Experiment. The Context Camera image and the High Resolution Imaging Science Experiment image were acquired simultaneously. As with the Context Camera, the first image from the High Resolution Imaging Science Experiment was of a much lower resolution than will be obtained during the primary science phase of the Mars Reconnaissance Orbiter mission, owing to the higher altitude during this test. This figure illustrates one of the key roles that Context Camera will play during the mission -- acquiring context images for the other science instruments aboard the Mars Reconnaissance Orbiter. Credit: NASA/JPL/MSSS, This is the first image of Mars taken by the Context Camera on NASA's Mars Reconnaissance Orbiter. The spacecraft began orbiting the red planet on March 10, 2006. During its 10th close approach to Mars, on March 24, it turned its cameras to view the planet's surface. Although the images acquired were about 10 times lower in resolution than will ultimately be obtained when the spacecraft has finished reshaping its orbit for the mission's primary science phase, these test images provide important confirmation of the performance of the cameras and the spacecraft. This first image by the Context Camera includes some chaotic terrain at the east end of Mars' Valles Marineris, seen along the top (northern) edge of the image. The image has a scale of about 87 meters (285 feet) per pixel, which is 14.5 times lower resolution than will be acquired during the primary science phase. Typical images from the Context Camera acquired during that phase of the mission will have a resolution of 6 meters (20 feet) per pixel, and will cover an area about 30 kilometers (18.6 miles) wide. Note that, because these are initial, test images, there is some linear striping in the images. This results from incomplete removal of pixel-to-pixel variations in the Context Camera detector by the present calibration software. One use of the test imaging is an opportunity to fine-tune the calibrations before the primary science phase begins. Figure 1: image above ( Full Res GIF 1.9 MB ) is a comparison of a wide-angle, red-filter image from the Mars Orbiter Camera on NASA's Mars Global Surveyor (left) with the first Mars image from the Context Camera. The image from the Mars Orbiter Camera was taken the same day, but about 6.2 hours after the image from the Context Camera, at a local solar time of 1:42 p.m. The Context Camera image was taken at roughly 7:32 a.m., local solar time. Figure 2: image above ( Full Res JPEG 944 kB ) shows a color view cropped from a Mars Orbiter Camera daily global map acquired on the same day as the first two Mars images by the Context Camera. The map shows the planet as if every part could be imaged at some time between 1 p.m. and 3 p.m., that is, with early afternoon illumination. The cameras on Mars Reconnaissance Orbiter, conversely, imaged the planet during morning hours. The Mars Orbiter Camera view was obtained about four hours later in the day than the Context Camera data. Inserted into the daily global map are two grayscale views from the Context Camera. This shows that the Context Camera began imaging when it was over the southernmost portion of the chaotic terrain at the east end of the Valles Marineris. A second image was acquired several minutes later, as Mars Reconnaissance Orbiter flew southward towards the west side of the large Argyre impact basin. The tops of the two Context Camera images were obtained about 13 minutes apart. Figure 3: image to right ( Full Res GIF 2.1 MB |
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Mars Reconnaissance Orbiter
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Mars Reconnaissance Orbiter is Already Breaking Records! |
| Description |
The Mars Reconnaissance Orbiter set the record for interplanetary missions, sending back the most data in a single day! An unprecedented amount of data - the equivalent of 13 CDs - was returned by the Mars Reconnaissance Orbiter mission in a single day! NASA's latest mission to Mars sent 75 gigabits of data back to Earth from millions of miles away, including beautiful pictures of the Moon. A preview of what's to come with this mighty mission, the spacecraft calibrated its high-resolution camera, using the Moon as its subject. Calibrations of space cameras are, essentially, adjustments to ensure optimal picture taking. On Sept. 8, 2005, the Moon - half bathed in the sun's glow and half draped in darkness - showed off all of its pocks and dimples for the powerful HiRISE camera. The successful calibration bodes well for the capture of stunning and enlightening images at the red planet. The camera took the shot while at a distance of about 10 million kilometers (6 million miles) from the Moon. The dark feature on the right is Mare Crisium. From that distance, the Moon would appear as a star-like point of light to the unaided eye. The test verified the camera's focusing capability and provided an opportunity for calibration. The spacecraft's Context Camera and Optical Navigation Camera also performed as expected during the test. The Mars Reconnaissance Orbiter, launched on Aug. 12, 2005, is on course to reach Mars on March 10, 2006. After gradually adjusting the shape of its orbit for half a year, it will begin its primary science phase in November 2006. From the mission's planned science orbit about 300 kilometers (186 miles) above the surface of Mars, the high resolution camera will be able to discern features as small as one meter or yard across. Credit: NASA/JPL-Caltech/University of Arizona |
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Full-Frame Reference for Tes
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Full-Frame Reference for Test Photo of Moon |
| Description |
This pair of views shows how little of the full image frame was taken up by the Moon in test images taken Sept. 8, 2005, by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. The Mars-bound camera imaged Earth's Moon from a distance of about 10 million kilometers (6 million miles) away -- 26 times the distance between Earth and the Moon -- as part of an activity to test and calibrate the camera. The images are very significant because they show that the Mars Reconnaissance Orbiter spacecraft and this camera can properly operate together to collect very high-resolution images of Mars. The target must move through the camera's telescope view in just the right direction and speed to acquire a proper image. The day's test images also demonstrate that the focus mechanism works properly with the telescope to produce sharp images. Out of the 20,000-pixel-by-6,000-pixel full frame, the Moon's diameter is about 340 pixels, if the full Moon could be seen. The illuminated crescent is about 60 pixels wide, and the resolution is about 10 kilometers (6 miles) per pixel. At Mars, the entire image region will be filled with high-resolution information. The Mars Reconnaissance Orbiter, launched on Aug. 12, 2005, is on course to reach Mars on March 10, 2006. After gradually adjusting the shape of its orbit for half a year, it will begin its primary science phase in November 2006. From the mission's planned science orbit about 300 kilometers (186 miles) above the surface of Mars, the high resolution camera will be able to discern features as small as one meter or yard across. The Mars Reconnaissance Orbiter mission is managed by NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, for the NASA Science Mission Directorate. Lockheed Martin Space Systems, Denver, prime contractor for the project, built the spacecraft. Ball Aerospace & Technologies Corp., Boulder, Colo., built the High Resolution Imaging Science Experiment instrument for the University of Arizona, Tucson, to provide to the mission. The HiRISE Operations Center at the University of Arizona processes images from the camera. Credit: NASA/JPL/University of Arizona |
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High-Resolution Mars Camera
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| title |
High-Resolution Mars Camera Test Image of Moon (Blue-Green) |
| Description |
This crescent view of Earth's Moon in blue-green wavelengths comes from a camera test by NASA's Mars Reconnaissance Orbiter spacecraft on its way to Mars. The mission's High Resolution Imaging Science Experiment camera took the image on Sept. 8, 2005, while at a distance of about 10 million kilometers (6 million miles) from the Moon. The dark feature on the right is Mare Crisium. From that distance, the Moon would appear as a star-like point of light to the unaided eye. The test verified the camera's focusing capability and provided an opportunity for calibration. The spacecraft's Context Camera and Optical Navigation Camera also performed as expected during the test. The Mars Reconnaissance Orbiter, launched on Aug. 12, 2005, is on course to reach Mars on March 10, 2006. After gradually adjusting the shape of its orbit for half a year, it will begin its primary science phase in November 2006. From the mission's planned science orbit about 300 kilometers (186 miles) above the surface of Mars, the high resolution camera will be able to discern features as small as one meter or yard across. Credit: NASA/JPL/University of Arizona |
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High-Resolution Mars Camera
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| title |
High-Resolution Mars Camera Test Image of Moon (Infrared) |
| Description |
This crescent view of Earth's Moon in infrared wavelengths comes from a camera test by NASA's Mars Reconnaissance Orbiter spacecraft on its way to Mars. The mission's High Resolution Imaging Science Experiment camera took the image on Sept. 8, 2005, while at a distance of about 10 million kilometers (6 million miles) from the Moon. The dark feature on the right is Mare Crisium. From that distance, the Moon would appear as a star-like point of light to the unaided eye. The test verified the camera's focusing capability and provided an opportunity for calibration. The spacecraft's Context Camera and Optical Navigation Camera also performed as expected during the test. The Mars Reconnaissance Orbiter, launched on Aug. 12, 2005, is on course to reach Mars on March 10, 2006. After gradually adjusting the shape of its orbit for half a year, it will begin its primary science phase in November 2006. From the mission's planned science orbit about 300 kilometers (186 miles) above the surface of Mars, the high resolution camera will be able to discern features as small as one meter or yard across. Credit: NASA/JPL/University of Arizona |
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New Mars Camera's First Imag
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| title |
New Mars Camera's First Image of Mars from Mapping Orbit |
| Description |
The high resolution camera on NASA's Mars Reconnaissance Orbiter captured its first image of Mars in the mapping orbit, demonstrating the full resolution capability, on Sept. 29, 2006. The High Resolution Imaging Science Experiment (HiRISE) acquired this image at 8:16 AM (Pacific Time), and parts of the image became available to the HiRISE team at 1:30 PM. With the spacecraft at an altitude of 280 kilometers (174 miles), the image scale is 29.7 centimeters per pixel (about 12 inches per pixel). This sub-image covers a small portion of the floor of Ius Chasma, one branch of the giant Valles Marineris system of canyons. The image illustrates a variety of processes that have shaped the Martian surface. There are bedrock exposures of layered materials, which could be sedimentary rocks deposited in water or from the air. Some of the bedrock has been faulted and folded, perhaps the result of large-scale forces in the crust or from a giant landslide. The darker unit of material at right includes many rocks. The image resolves rocks as small as small as 90 centimeters (3 feet) in diameter. At bottom right are a few dunes or ridges of windblown sand. If a person was located on this part of Mars, he or she would just barely be visible in this image. Image TRA_000823_1720 was taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard the Mars Reconnaissance Orbiter spacecraft on September 29, 2006. Shown here is a small portion of the full image. The full image is centered at minus 7.8 degrees latitude, 279.5 degrees East longitude. The image is oriented such that north is to the top. The range to the target site was 297 kilometers (185.6 miles). At this distance the image scale is 29.7 centimeters per pixel (with one-by-one binning) so objects about 89 centimeters (35 inches) across are resolved. The image was taken at a local Mars time of 3:30 PM and the scene is illuminated from the west with a solar incidence angle of 59.7 degrees, thus the sun was about 30.3 degrees above the horizon. At an LsubS of 113.6 degrees, the season on Mars is Northern Summer / Southern Winter. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace Corporation and is operated by the University of Arizona. Credit: NASA/JPL/UA |
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The Mars Reconnaissance Orbi
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The Mars Reconnaissance Orbiter "Follow the Water" theme |
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This artist's concept represents the "Follow the Water" theme of the Mars Reconnaissance Orbiter mission (MRO). MRO's science instruments monitor the present water cycle in the Mars atmosphere and the associated deposition and sublimation of water ice on the surface, while probing the subsurface to see how deep the water ice reservoir detected by Mars Odyssey extends. At the same time, MRO will search for surface features and minerals (e.g., carbonates and sulfates) that record the extended presence of liquid water on its surface earlier in the history of the planet. The instruments involved are the shallow radar SHARAD, the CRISM spectrometer, the MARCI weather camera, the HiRISE high-resolution camera, the CTX context camera and the Mars Climate Sounder (MCS). To the far left, the SHARAD antenna beams down and "sees" into the first few hundreds of feet (up to 1 kilometer) of Mars' crust. Just to the right of that, the next beam highlights the data received from the CRISM spectrometer that identifies minerals on the surface. The next beam over represents the HiRISE camera which can "zoom in" on local targets, providing the highest-resolution orbital images yet of features like craters and gullies and rocks. The beam that shines almost horizontally is that of the Mars Climate Sounder. This instrument is critical to analyzing the current climate of Mars since it observes the temperature, humidity, and dust content of the martian atmosphere, their seasonal and year-to-year variations. Meanwhile, the MARCI images ice clouds, dust clouds and hazes, and the ozone distribution, producing daily global maps in multiple colors to monitor daily weather and seasonal changes. The electromagnetic spectrum is represented on the top right and individual instruments are placed where their capability lies. |
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HiRISE Team Anxiously Awaits
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HiRISE Team Anxiously Awaits Images |
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Sleep is secondary to Dr. Alfred McEwen and his HiRISE team. They are eager to see what their instrument is seeing from orbit around Mars. Scientists and engineers at the University of Arizona's Lunar and Planetary Laboratory are gearing up for the first test images of Mars taken by the High Resolution Imaging Science Experiment (HiRISE) camera. The camera team expects to begin receiving the images early Friday (March 24, 2006). The Mars Reconnaissance Orbiter will be farther from Mars when the camera takes these test images than it will be when the mission's main science phase begins next fall, so the resolution of features in the images will not match what is anticipated later. However, this week's testing is the only planned use of the camera until the science phase begins. Stay tuned for the first test images! Team members for the High Resolution Imaging Science Experiment camera on NASA's Mars Reconnaissance Orbiter enjoy seeing the first Mars images from the camera, at the instrument's operations center on the University of Arizona campus, Tucson, early Friday, March 24, 2006. Standing, left to right: Eric Eliason, Alfred McEwen. Seated, top to bottom: Ingrid Dauber, Chris Schaller, Anjani Polit, Maria Banks Credit: NASA/JPL/University of Arizona |
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Testing HiRISE
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Testing HiRISE |
| Description |
Scientists and engineers at the University of Arizona are gearing up to see the first test images of Mars taken by the High Resolution Imaging Science Experiment (HiRISE) camera. The camera team expects to begin receiving the images early Friday (March 24, 2006). The Mars Reconnaissance Orbiter will be farther from Mars when the camera takes these test images than it will be when the mission's main science phase begins next fall, so the resolution of features in the images will not match what is anticipated later. However, this week's testing is the only planned use of the camera until the science phase begins. Stay tuned for the first test images! Credit: NASA/JPL-Caltech |
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The Mars Reconnaissance Orbi
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The Mars Reconnaissance Orbiter |
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This artist's concept of the Mars Reconnaissance Orbiter features the spacecraft's main bus facing down, toward the red planet. The large silver circular feature above the spacecraft bus is the high-gain antenna, the spacecraft's main means of communicating with both Earth and other spacecraft. The long, thin pole behind the bus is the SHARAD antenna. Seeking liquid or frozen water, SHARAD will probe the subsurface using radar waves at a 15-25 MHz frequency band, "seeing" in the first few hundreds of feet (up to 1 kilometer) of Mars' crust. The large instrument (covered in black thermal blanketing) in the center is the HiRISE camera. This powerful camera will provide the highest-resolution images from orbit to date. The other easily visible instruments are: the Electra telecommunications package which is the gold-colored instrument directly left of the HiRISE camera. It will act as a communications relay and navigation aid for Mars spacecraft. To the right of the HiRISE camera is the Context Imager (CTX). |
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HiRISE Comparison
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HiRISE Comparison |
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The HiRISE camera will provide the highest-resolution images yet from martian orbit. These high resolution images will enable scientists to resolve 1-meter (about 3-foot) sized objects on Mars and to study the morphology (surface structure) in a much more comprehensive manner than ever before. |
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Smooth Sailing
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Smooth Sailing |
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The Mars Reconnaissance Orbiter began its cruise phase and successfully completed the first two vital tasks. The word cruise is a deceptive one, at least in the context of navigating spacecraft. During cruise, or the period after launch and before the final approach to Mars, the spacecraft and its support team are very busy. This is no time to lounge with a frosty tropical drink or strike up a conga line around the pool deck. After the cheers died down following the successful August launch, it was time to get to work again, reserving the ultimate celebration for the orbiter's first return of unprecedented martian data. Tasks one and two on the orbiter's cruise "to do" list were the first trajectory correction maneuver and the initial check of the science instruments. Trajectory correction maneuvers are common, planned course adjustments that navigators perform on most interplanetary missions. In order to set the Mars Reconnaissance Orbiter on its precise path to Mars, engines are fired to tweak the direction. On August 27, 2005 a 44.5-second burn placed the spacecraft almost exactly where navigators intended. The instrument turn on and initial check was performed on August 30-31, 2005. The instruments were powered sequentially and all instruments turned on and returned instrument housekeeping data. Most objectives were achieved, although both the HiRISE camera and CRISM spectrometer terminated activities early due to internal temperature checks that indicated irregular conditions. For the HiRISE camera, the team conferred and decided to adjust thermal conditions - kind of like lowering the temperature on the thermostat to kick on the air conditioning - to make the instrument more comfortable. After that procedure, the camera checkout was positive. Turning on the coolers in the instrument cooling system for the CRISM spectrometer caused a sensor on the instrument to go into safe mode because it thought it was too cold. That issue has been resolved and the complete check of the instrument will be conducted in December. The MARCI and Context Camera each took a single image (of space), which were successfully returned. MARCI also took calibration images of the Earth and Moon three days after launch. All other instruments checkouts went well. Credit: NASA/JPL |
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Landscape West of Bosporos R
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Landscape West of Bosporos Rupes |
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This image was taken in the mid-latitudes of Mars' southern hemisphere near the giant Argyre impact basin. It is located just to the west of a prominent scarp known as Bosporos Rupes. The left side of the image shows cratered plains. Some of the craters are heavily mantled and indistinct, whereas others exhibit sharp rims and dramatic topography. The largest crater in this half of the image is about 2.5 kilometers (1.5 miles) wide. Mounds and ridges, which may be remnants of an ice-rich deposit, are visible on its floor. Three sinuous valleys occupy the center of the image. Valleys such as these were first observed in data returned by the NASA Mariner 9 spacecraft, which reached Mars in 1971. The right side of the image shows part of an impact crater that is approximately 20 kilometers (12 miles) in diameter. The furrowed appearance of the crater's inner wall suggests that it has been extensively modified, perhaps by landslides and flowing water. Like other craters in the area, the floor of this crater has a rough and dissected texture that is often attributed to the loss of ice-rich material. Image AEB_000001_0050_Red was taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard NASA's Mars Reconnaissance Orbiter spacecraft on March 24, 2006. The image is centered at 40.64 degrees south latitude, 303.49 degrees east longitude. The image is oriented such that north is 7 degrees to the left of up. The range to the target was 2,044 kilometers (1,270 miles). At this distance the image scale is 2.04 meters (6.69 feet) per pixel, so objects as small as 6.1 meters (20 feet) are resolved. In total this image is 40.90 kilometers (25.41 miles) or 20,081 pixels wide and 11.22 kilometers (6.97 miles) or 5,523 pixels high. The image was taken at a local Mars time of 07:30 and the scene is illuminated from the upper right with a solar incidence angle of 81.4 degrees, thus the sun was about 8.6 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona |
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North Polar Layered Deposits
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North Polar Layered Deposits in Summer |
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The High Resolution Imaging Science Experiment (HiRISE) on NASA's Mars Reconnaissance Orbiter acquired this image during its first day of test imaging from the spacecraft's low-altitude mapping orbit, Sept. 29, 2006. This image of Mars' north polar layered deposits was taken during the summer season (solar longitude of 113.6 degrees), when carbon dioxide frost had evaporated from the surface. The bright spots seen here are most likely patches of water frost, but the location of the frost patches does not appear to controlled by topography. Layers are visible at the bottom of the image, mostly due to difference in slope between them. The variations in slope are probably caused by differences in the physical properties of the layers. Thinner layers that have previously been observed in these deposits are visible, and may represent annual deposition of water ice and dust that is thought to form the polar layered deposits. These deposits are thought to record global climate variations on Mars, similar to ice ages on Earth. HiRISE images such as this should allow Mars' climate record to be inferred and compared with climate changes on Earth. Image TRA_000825_2665 was taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard the Mars Reconnaissance Orbiter spacecraft on September 29, 2006. Shown here is the full image, centered at 86.5 degree latitude, 172.0 degrees east longitude. The image is oriented such that north is to the top. The range to the target site was 298.9 kilometers (186.8 miles). At this distance the image scale is 59.8 centimeters (23.5 inches) per pixel (with two-by-two binning} so objects about 1.79 meters (70 inches) across are resolved. In total the original image was 12.2 kilometers 7.58 mile, 10024 pixels) wide and 6.1 kilometers (3.79 miles, 5000 pixels) long. The image was taken at a local Mars time of 3:30 PM and the scene is illuminated from the southwest with a solar incidence angle of 63.5 degrees, thus the sun was about 26.5 degrees above the horizon. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace Corporation and is operated by the University of Arizona. Credit: NASA/JPL/UA |
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Detail of First Mars Image f
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Detail of First Mars Image from Newly Arrived Camera |
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This view shows a full-resolution portion of the first image of Mars taken by the High Resolution Imaging Science Experiment camera (HiRISE) on NASA's Mars Reconnaissance Orbiter. The spacecraft, launched Aug. 12, 2005, began orbiting Mars on March 10, 2006. The image is of an area in Mars' mid-latitude southern highlands. HiRISE took this first test image from orbit on March 24, 2006, from an altitude of 2,489 kilometers (1,547 miles), achieving a resolution of 2.49 meters (98 inches) per pixel, or picture element. The smallest objects of discernable shape are about three pixels across. An image acquired at this latitude during the Mars Reconnaissance Orbiter's main science phase, beginning in fall 2006, would be taken from an altitude of about 280 kilometers (174 miles) and have a resolution of 28 centimeters (11 inches) per pixel. This view covers an area about 4.5 by 2.1 kilometers (1.6 by 1.3 miles), a subset of the broader image [ http://mars.jpl.nasa.gov/mro/gallery/calibration/pia08014-AEB1-full-reduced1.html ]. The quality of this test image is spectacular, with no hint to the eye of any smear or blurring. A high signal-to-noise ratio reveals fine details even in the shadows. Credit: NASA/JPL-Caltech/University of Arizona |
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Landscape Northeast of Halle
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Landscape Northeast of Halley Crater |
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. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona, This image shows a landscape west of Mars' Argyre impact basin and northeast of Halley Crater. The large but faint circular feature near the center of the image is an unnamed impact crater about 7.5 kilometers (4.7 miles) in diameter. It has been all but erased by geological (and probably ice-related) processes. In fact, the majority of impact craters in this image have been modified from their original shapes, some undoubtedly beyond recognition. Only a few small craters remain pristine. The most prevalent surface type in this image is rough, dissected terrain, which is characterized by a complex pattern of knobs, pits, ridges and valleys. In places the rough terrain has been covered by a younger material that appears flat, smooth and nearly featureless. The smooth material may have been emplaced as muddy or icy debris. It filled low-lying areas (most notably craters) and surrounded higher features, preserving islands of rough terrain. Wind-formed dunes have formed atop some of the smooth material, and diagonal streaks on the right side of the image may be due to the winds. Images such as this show the importance of water (liquid and/or ice), wind, and impacts in shaping the surface of Mars. Image AEB_000001_0100_Red was taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard NASA's Mars Reconnaissance Orbiter spacecraft on March 24, 2006. The image is centered at 47.14 degrees south latitude, 302.00 degrees east longitude. It is oriented such that north is 7 degrees to the left of up. The range to the target was 1,699 kilometers (1,056 miles). At this distance the image scale is 1.70 meter (5.58 feet) per pixel in the center portion of the image, so objects as small as 5.1 meter (16.7 feet) are resolved. In the side regions the pixels were binned 2x2 to a scale of 3.4 meters (11.2 feet) per pixel. The camera has a total of 10 red-bandpass CCD detectors, and in this image the first 4 CCDs on the left and the last 3 on the right were binned 2x2, while 3 in the middle returned data at full resolution. In total this image is 34.08 kilometers (21.18 miles) or 20,081 pixels wide and 8.50 kilometers (5.28 miles) or 5,164 pixels high. The image was taken at a local Mars time of 07:27 and the scene is illuminated from the upper right with a solar incidence angle of 84.5 degrees, thus the sun was about 5.5 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ] |
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Perspective Views of HiRISE
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Perspective Views of HiRISE First Image |
| Description |
This perspective view generated from digital topography provides an overview of the Mars terrain covered in the first color image of Mars from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. It has a field of view 55 degrees wide, and no vertical exaggeration. The overview illustrates how the ridge has deformed several valleys and impact craters. The image is a subset of the first HiRISE image from Mars [ http://photojournal.jpl.nasa.gov/catalog/PIA08014 ], which was taken on March 24, 2006. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78.1 degrees, thus the sun was about 11.9 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the HiRISE and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona/USGS |
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High-Resolution Mars Camera
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High-Resolution Mars Camera Test Image of Moon (Red) |
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This crescent view of Earth's Moon in red wavelengths comes from a camera test by NASA's Mars Reconnaissance Orbiter spacecraft on its way to Mars. The mission's High Resolution Imaging Science Experiment camera took the image on Sept. 8, 2005, while at a distance of about 10 million kilometers (6 million miles) from the Moon. The dark feature on the right is Mare Crisium. From that distance, the Moon would appear as a star-like point of light to the unaided eye. The test verified the camera's focusing capability and provided an opportunity for calibration. The spacecraft's Context Camera and Optical Navigation Camera also performed as expected during the test. The Mars Reconnaissance Orbiter, launched on Aug. 12, 2005, is on course to reach Mars on March 10, 2006. After gradually adjusting the shape of its orbit for half a year, it will begin its primary science phase in November 2006. From the mission's planned science orbit about 300 kilometers (186 miles) above the surface of Mars, the high resolution camera will be able to discern features as small as one meter or yard across. Credit: NASA/JPL/University of Arizona |
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Stellar Calibration, HiRISE!
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Stellar Calibration, HiRISE! |
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As part of a calibration test conducted on December 14, 2005, the HiRISE camera on Mars Reconnaissance Orbiter snapped this image of part of Jewel Box, an open star cluster. Jewel Box was so named by Sir John Herschel because of the variety of star colors in the cluster, including the large red giant seen near the bottom of this image."The images we've acquired of stars and the Moon have been very sharp," said Dr. Alfred McEwen, the camera's principal investigator. "The camera and spacecraft work great, so we are really looking forward to imaging Mars." HiRISE can image in three colors: green, red, and near-infrared, so the colors are not exactly as we see them with our eyes. Jewel Box, also called Kappa Crucis, is about 10 million years old, so it is much younger than our Sun at 4600 million years old. The Jewel Box cluster lies about 7,500 light years away, so the light we see today left the stars at the time of Earth's Neolithic ages, when farming was first being practiced. The image shown here is a small portion of the full image, which is 20,000 x 35,000 pixels or 700 mega-pixels. Credit: NASA/JPL-Caltech |
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Perspective Views of HiRISE
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Perspective Views of HiRISE First Image |
| Description |
This perspective view generated from digital topography provides an overview of a portion of the Mars terrain covered in the first color image of Mars from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. It has a field of view 55 degrees wide, and no vertical exaggeration. The overview illustrates how the ridge has deformed several valleys and impact craters. The image is a subset of the first HiRISE image from Mars [ http://photojournal.jpl.nasa.gov/catalog/PIA08014 ], which was taken on March 24, 2006. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78.1 degrees, thus the sun was about 11.9 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the HiRISE and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona/USGS |
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Perspective Views of HiRISE
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| title |
Perspective Views of HiRISE First Image |
| Description |
This perspective view generated from digital topography provides an overview of a portion of the Mars terrain covered in the first color image of Mars from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. It has a field of view 55 degrees wide, and no vertical exaggeration. The overview illustrates how the ridge has deformed several valleys and impact craters. The image is a subset of the first HiRISE image from Mars [ http://photojournal.jpl.nasa.gov/catalog/PIA08014 ], which was taken on March 24, 2006. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78.1 degrees, thus the sun was about 11.9 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the HiRISE and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona/USGS |
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Sample of the Argyre Impact
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Sample of the Argyre Impact Basin Rim |
| Description |
http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona, This image shows part of a low mountain belt that rings the Argyre impact basin in Mars' southern hemisphere. The mountains or hills seen here are located in the northwestern part of the Charitum Montes. Taken just minutes after the sun had risen over the horizon, only the sun-facing slopes are well illuminated and much of the scene is in shadow, but the camera has nevertheless captured many details of the surface that are only dimly illuminated. There are terrains that are both smooth and rough at this scale (2.94 meters or 9.65 feet per pixel). The rough terrain is littered with blocks roughly 10 meters (30 feet) across, and the smooth material has a uniform appearance broken by subtle, undulating ridges. The rough terrains usually occur at relatively high elevations, and smooth material occupies the lowest areas. In some locations it is evident that boulders from the rough terrain have tumbled downhill onto the smooth material. The smooth material is younger than the rough terrain, and some of it may have formed when water-rich or ice-rich debris flooded low-lying areas. In other areas the smooth material mantles the topography like deposits of airborne dust. Further upslope, the mountain flanks have a variety of rough textures. In places the terrain has been eroded into streamlined forms and striations, suggestive of glacial erosion. Gullies formed in one spot near bottom center. Perhaps the most striking aspect of this image is the dearth of fresh impact craters. The Argyre basin is thought to be billions of years old, but much more recent processes have greatly modified the surface. Image AEB_000001_0150_Red was taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard NASA's Mars Reconnaissance Orbiter spacecraft on March 24, 2006. The image is centered at 52.20 degrees south latitude, 300.75 degrees east longitude. It is oriented such that north is 7 degrees to the left of up. The range to the target was 1,470 kilometers (913 miles). With 2x2 pixel binning, the scale of the image is 2.94 meters (9.65 feet) per pixel, so objects as small as 8.82 meters (28.94 feet) are resolved. In total this image is 29.47 kilometers (18.31 miles) or 10,040 pixels wide and 76.44 kilometers (47.50 miles) or 26,011 pixels long. The image was taken at a local Mars time of 07:24 and the scene is illuminated from the upper right with a solar incidence angle of 87.1 degrees, thus the sun was about 2.9 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: |
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First Color HiRISE Image of
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First Color HiRISE Image of Mars |
| Description |
. JPL, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona, This is the first color image of Mars from the High Resolution Imaging Science Experiment on NASA's Mars Reconnaissance Orbiter. At the center portion of the camera's array of light detectors there are extra detectors to image in green and near-infrared color bandpasses, to be combined with the black-and-white images (from red-bandpass detectors) to create color images. This is not natural color as seen by human eyes, but infrared color -- shifted to longer wavelengths. This image also has been processed to enhance subtle color variations. The southern half of the scene is brighter and bluer than the northern half, perhaps due to early-morning fog in the atmosphere. Large-scale streaks in the northern half are due to the action of wind on surface materials. The blankets of material ejected from the many small fresh craters are generally brighter and redder than the surrounding surface, but a few are darker and less red. Two greenish spots in the middle right of the scene may have an unusual composition, and are good future targets for the Compact Reconnaissance Imaging Spectrometer for Mars, a mineral-identifying instrument on Mars Reconnaissance Orbiter (http://crism.jhuapl.edu/ [ http://crism.jhuapl.edu/ ]). In the bottom half of the image we see a redder color in the rough areas, where wind and sublimation of water or carbon dioxide ice have partially eroded patches of smooth-textured deposits. Image AEB_000001_0000_Color was taken by HiRISE on March 24, 2006. The image is centered at 33.65 degrees south latitude, 305.07 degrees east longitude. It is oriented such that north is 7 degrees to the left of up. The range to the target was 2,493 kilometers (1,549 miles). At this distance the image scale is 2.49 meters (8.17 feet) per pixel, so objects as small as 7.5 meters (24.6 feet) are resolved. In total this image is 49.92 kilometers (31.02 miles) or 20,081 pixels wide and 23.66 kilometers (14.70 miles) or 9,523 pixels long. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78 degrees, thus the sun was 12 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ] |
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First HiRISE Image of Mars:
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First HiRISE Image of Mars: Topographic Model from Photoclinometry |
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http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona/USGS, This is a topographic map of part of the area covered by the first image of Mars obtained by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter spacecraft. The image was processed at the U.S. Geological Survey, Flagstaff, by a technique called photoclinometry (or, more descriptively, "shape-from-shading"). This method allows elevations to be reconstructed from a single image by noting how surfaces sloping toward the sun appear brighter than areas that slope away from it. This image is almost ideal for such interpretation because the low sun angle reveals even subtle slopes with dramatic contrast, and variations in the brightness of surface materials (which could be confused with slopes) are minimal. At left is the region of the image that was analyzed, tinted to approximate the visual appearance of the Martian surface. This region is a square 20.4 kilometers (12.7 miles) wide (8,192 pixels by 8,192 pixels at a scale of 2.49 meters or 8.17 feet per pixel). At right is a color-coded topographic contour map of the same area. The total range of elevations is 1.6 kilometers (1 mile), with low areas shown in purple and high areas in red. Contours mark each 20-meter (66-foot) change in elevation. Photoclinometry gives relative rather than absolute heights, but the overall height and shape of features in this map, such as the ridge Ogygis Rupes in the center, agree reasonably well with results from the Mars Orbiter Laser Altimeter on NASA's Mars Odyssey spacecraft, an instrument with high absolute accuracy but relatively low spatial resolution. The real value of mapping by photoclinometry, however, is that it reveals the details of the smallest topographic features resolved by the image. In this example, the image was resampled by a factor of 2 before processing, so the topographic map has a scale of 5 meters (16 feet) per pixel and resolves features as small as 15 meters (49 feet). Computer-generated three-dimensional close-ups of the surface provide one way to visualize these small but important clues to Martian geologic history. This illustration shows a subset of AEB_000001_0000_Red, which was taken by the HiRISE camera on March 24, 2006. The image is oriented such that north is 7 degrees to the left of up. The range to the target was 2,493 kilometers (1,549 miles). At this distance the image scale is 2.49 meters (8.17 feet) per pixel, so objects as small as 7.5 meters (24.6 feet) are resolved. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78.1 degrees, thus the sun was about 11.9 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: |
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First HiRISE image of Mars
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First HiRISE image of Mars |
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. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona, The first image of Mars by the High Resolution Imaging Science Experiment (HiRISE) on NASA's Mars Reconnaissance Orbiter shows a story of geologic change in the eastern Bosporos Planum region. Old stream valleys cut into the flanks of a gently sloping mountain range in the center of the image. Layers of smooth-textured deposits have mantled the stream valleys and many impact craters. Wind and sublimation of water or carbon dioxide ice have partially eroded patches of the smooth-textured deposits, leaving behind areas of layered and hummocky terrain. A prominent ridge that extends from the top to the bottom of the image dominates the scene. This ridge formed above a thrust fault, a type of fault that occurs when the surface of a planet is compressed. On planetary surfaces, such fault-related ridges are termed "wrinkle ridges." They are commonly observed on Mars, as well as on Earth's moon and on Venus and Mercury. The wrinkle ridge imaged here is named Ogygis Rupes. This wrinkle ridge has deformed several valleys and impact craters. Throughout the scene, geologically young sand dunes are present within stream valleys and some impact craters. The area is also sprinkled with many small young impact craters, which are distinguished by sharp crater rims and bright or dark halos of ejected material. This image demonstrates how a single HiRISE image can capture a multitude of geologic processes. Image AEB_000001_0000_Red was taken by HiRISE on March 24, 2006. The image is centered at 33.65 degrees south latitude, 305.07 degrees east longitude. It is oriented such that north is 7 degrees to the left of up. The range to the target was 2,493 kilometers (1,549 miles). At this distance the image scale is 2.49 meters (8.17 feet) per pixel, so objects as small as 7.5 meters (24.6 feet) are resolved. In total this image is 49.92 kilometers (31.02 miles) or 20,081 pixels wide and 23.66 kilometers (14.70 miles) or 9,523 pixels long. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78 degrees, thus the sun was 12 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ] |
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Perspective Views of HiRISE
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Perspective Views of HiRISE First Image |
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This perspective view generated from digital topography provides an overview of a portion of the Mars terrain covered in the first color image of Mars from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. It has a field of view 55 degrees wide, and no vertical exaggeration. The overview illustrates how the ridge has deformed several valleys and impact craters. The image is a subset of the first HiRISE image from Mars [ http://photojournal.jpl.nasa.gov/catalog/PIA08014 ], which was taken on March 24, 2006. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78.1 degrees, thus the sun was about 11.9 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the HiRISE and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona/USGS |
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A Myriad of Geologic Process
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A Myriad of Geologic Processes in Terra Cimmeria |
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This scene in a region of Mars named Terra Cimmeria shows a variety of ancient and recent geologic processes. In the upper portion of the image, a twisting ridge of raised ground may outline the location of a subsurface thrust fault. This type of fault results in the compression and crumpling of a planet's surface. This crumpling of the planet's surface has squeezed two originally circular craters on the ridge into oval-shaped craters. Valleys are also present throughout the image, suggesting that water flowed across this area a long time ago. Many valleys and craters in the image are now filled by deposits of dust or debris. This debris mantle is common over the middle latitudes of Mars and is a geologically recent deposit. Image AEB_000002_0050_Red was taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard NASA's Mars Reconnaissance Orbiter spacecraft on March 25, 2006. The image is centered at 40.64 degrees south latitude, 144.39 degrees east longitude. It is oriented such that north is 7 degrees to the left of up. The range to the target was 2,038 kilometers (1,266 miles). At this distance the image scale is 2.04 meters (6.69 feet) per pixel, so objects as small as 6.1 meters (20 feet) are resolved. In total this image is 12.34 kilometers (7.67 miles) or 6,045 pixels wide and 34.68 kilometers (21.55 miles) or 17,003 pixels long. The image was taken at a local Mars time of 07:28 and the scene is illuminated from the upper right with a solar incidence angle of 82.0 degrees, thus the sun was about 8.0 degrees above the horizon. At an Ls of 30 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona |
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Twilight Imaging of Kepler C
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Twilight Imaging of Kepler Crater Floor |
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This image of the floor of Kepler crater in early morning twilight highlights the quality of images from the High Resolution Imaging Science Experiment (HiRISE) camera even under extremely minimal lighting conditions. At the time that this image was acquired, the sun had just barely risen over the horizon. This faint illumination reveals a terrain dotted by numerous exhumed impact craters. These impact craters once dominated the landscape of this region until they were buried under a blanket of soil. Subsequent wind action and perhaps sublimation of subsurface water and carbon-dioxide ice has etched pits and grooves into the blanket of soil, revealing the older impact craters below. These exhumed impact craters can be recognized as circular depressions or plateaus. Also present in this scene are multitudes of dunes that have formed as sand has blown across the terrain. Dunes have accumulated in depressions, such as the pits and grooves associated with the exhumed impact craters, as well as on the floors of some of the larger craters. Image AEB_000002_0100_Red was taken by HiRISE camera onboard NASA's Mars Reconnaissance Orbiter spacecraft on March 25, 2006. The image is centered at 47.14 degrees south latitude, 142.90 degrees east longitude. It is oriented such that north is 7 degrees to the left of up. The range to the target was 1,694 kilometers (1,053 miles). Because the image was acquired by mixing the resolution levels of HiRISE detectors, the scale of the image is 6.76 meters (22.18 feet) per pixel, so objects as small as 27.04 meters (88.71 feet) are resolved. In total this image is 33.88 kilometers (21.05 miles) or 5,017 pixels wide and 37.18 kilometers (23.10 miles) or 5,636 pixels long. The image was taken at a local Mars time of 07:25 and the scene is illuminated from the upper right with a solar incidence angle of 85.1 degrees, thus the sun was about 4.9 degrees above the horizon. At an Ls of 30 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona |
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Sample of Mid-latitude South
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Sample of Mid-latitude Southern Highlands |
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http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona, This image shows terrain northeast of Martz Crater in the southern highlands of Mars. It is a landscape dominated by impact craters, scarps and ridges. The plethora of craters and the overprinting of younger craters on older craters indicate that this is an ancient surface. Curvilinear ridges called "wrinkle ridges" are common landforms on Mars. They form when layers of rock and sediment break and fold under compression. Multiple wrinkle ridges are captured in this image, the most prominent of which is a curving structure oriented approximately north-south. A 2.8-kilometer-wide (1.7-mile-wide) impact crater is superimposed on this north-south wrinkle ridge. Gullies, perhaps carved by water or muddy debris, are visible inside this crater. They are partly in shadow, but can be shown clearly by adjusting the contrast of the full-resolution image. Several of the smaller craters in this image contain dune fields, which attest to the presence of wind-blown sediments. In the lower portion of the image a few cliffs or scarps can be seen. While their origin is uncertain, they may have formed by some combination of flowing water and mass wasting. If one looks carefully at this image, it is possible to find horizontal blurred zones about 100 pixels tall. During these times the spacecraft was executing a test of how much the motion of another instrument would shake the spacecraft. These blurred regions also introduce geometric distortions, so the match between the three CCD images utilized for this observation is sometimes poor. The MRO spacecraft includes a high-stability mode that should minimize these problems. Image AEB_000002_0000_Red was taken by the High Resolution Imaging Science Experiment (HiRISE) camera onboard NASA's Mars Reconnaissance Orbiter spacecraft on March 25, 2006. The image is centered at 33.66 degrees south latitude, 145.97 degrees east longitude. It is oriented such that north is 7 degrees to the left of up. The range to the target was 2,485 kilometers (1,544 miles). At this distance the image scale is 2.49 meters (8.17 feet) per pixel, so objects as small as 7.5 meters (24.6 feet) are resolved. In total this image is 15.01 kilometers (9.33 miles) or 6,045 pixels wide and 57.27 kilometers (35.59 miles) or 23,024 pixels long. The image was taken at a local Mars time of 07:30 and the scene is illuminated from the upper right with a solar incidence angle of 78.7 degrees, thus the sun was about 11.3 degrees above the horizon. At an Ls of 30 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the High Resolution Imaging Science Experiment and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: |
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Perspective Views of HiRISE
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Perspective Views of HiRISE First Image |
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This perspective view generated from digital topography provides an overview of the Mars terrain covered in the first color image of Mars from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. It has a field of view 55 degrees wide, and no vertical exaggeration. The overview illustrates how the ridge has deformed several valleys and impact craters. The image is a subset of the first HiRISE image from Mars [ http://photojournal.jpl.nasa.gov/catalog/PIA08014 ], which was taken on March 24, 2006. The image was taken at a local Mars time of 07:33 and the scene is illuminated from the upper right with a solar incidence angle of 78.1 degrees, thus the sun was about 11.9 degrees above the horizon. At an Ls of 29 degrees (with Ls an indicator of Mars' position in its orbit around the sun), the season on Mars is southern autumn. Images from the HiRISE and additional information about the Mars Reconnaissance Orbiter are available online at: http://www.nasa.gov/mro [ http://www.nasa.gov/mro ] or http://HiRISE.lpl.arizona.edu [ http://HiRISE.lpl.arizona.edu ]. For information about NASA and agency programs on the Web, visit: http://www.nasa.gov [ http://www.nasa.gov ]. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. Credit: NASA/JPL/University of Arizona/USGS |
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First Mars Image from Newly
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First Mars Image from Newly Arrived Camera |
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This view shows the ground covered in the first image of Mars taken by the High Resolution Imaging Science Experiment camera (HiRISE) on NASA's Mars Reconnaissance Orbiter. The spacecraft, launched Aug. 12, 2005, began orbiting Mars on March 10, 2006. HiRISE took this first test image from orbit on March 24, 2006, from an altitude of 2,489 kilometers (1,547 miles). Images taken during the mission's main science phase, beginning in fall 2006, will be from an altitude about one-tenth as far from the ground, gaining even higher resolution. This image is a mosaic combining 10 side-by-side exposures taken through red filters, presented at greatly reduced scale. The full product would be 20,000 pixels wide by 9,500 pixels high. The white box at lower right indicates the position of a sample image [ http://mars.jpl.nasa.gov/mro/gallery/calibration/pia08013-AEB1-cut-full1.html ] offered in full resolution. The quality of this test image is spectacular, with no hint to the eye of any smear or blurring. A high signal-to-noise ratio reveals fine details even in the shadows. The scene covers an area 49.8 kilometers (30.9 miles) wide and 23.6 kilometers (14.7 miles) high, of landscape typical of Mars' mid-latitude southern highlands. The location is 34 degrees south latitude, 305 degrees east longitude. An old, muted crater lies at the middle of the scene, with sets of channels to the left and right. Superimposed on parts of this terrain is a much younger, layered mantle of debris. The debris mantle is smooth in places but rough in other areas where it may have partially sublimated. This suggests that the debris mantle is (or was) rich in volatiles such as ices of water, carbon dioxide or both. Also superimposed on the landscape are many small sharp-rimmed impact craters and wind-blown dunes. This image illustrates processes that may have involved water both on ancient Mars (channels and eroded craters) and much more recently in Mars' history (volatile-rich debris mantle). The radiometric and geometric processing of this image is very preliminary. In particular there are mismatches visible at full resolution along the seams between the 10 side-by-side images from separate CCDs (charge-coupled devices, which are electronic optical sensors). Credit: NASA/JPL-Caltech/University of Arizona |
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Dr. Alfred McEwen gives a "h
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Dr. Alfred McEwen gives a "high-five" to Eric Eliason |
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Dr. Alfred McEwen, Principal Investigator for the High Resolution Imaging Science Experiment (HiRISE) camera, gives a "high-five" to Eric Eliason, HiRISE Ground Operations Manager, upon the announcement that the Mars Reconnaissance Orbiter spacecraft has successfully entered Mars' orbit! Credit: Maria Schuchardt, University of Arizona's Space Imagery Center (UA/SIC) |
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Pre-launch Press Conference
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Pre-launch Press Conference |
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Mars Reconnaissance Orbiter project scientist Rich Zurek and HiRISE principal investigator Alfred McEwen field questions from reporters after a pre-launch press conference at Kennedy Space Center in Florida. Credit: NASA/JPL |
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Browse Image | Medium Image (129 kB) | Large (20.4 MB) Hi-Res (NASA's Planetary Photojournal) [ http://photojournal.jpl.nasa.gov/catalog/PIA08813 ] |
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Tracks left by NASA's Mars Exploration Rover Opportunity as it traveled along the rim of Victoria Crater can be seen clearly in this image taken by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter spacecraft. This is a subframe of a larger image that the camera acquired on June 26, 2007. The larger image will be released as HiRISE catalogue number PSP_004289_1780 after geometric processing. Opportunity first approached Victoria Crater at an alcove informally named "Duck Bay" (see tracks at left). It then drove along the crater's sinuous edge in a clockwise direction before heading back to Duck Bay, where it is expected to enter the crater in early July 2007. |
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Browse Image | Medium Image (62 kB) | Large (326 kB) |
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Area "c" of the image shows Spirit's heat shield at the edge of Bonneville Crater. Area "d" of the image shows the current location of Spirit. Toward the top of the image is "Home Plate," a plateau of layered rocks that Spirit explored during the early part of its third year on Mars. Spirit itself is clearly seen just southeast of Home Plate. Also visible are the tracks made by the rover before it arrived at its current location. This image is a small portion of an image catalogued as PSP_001513_1655 [ http://hiroc.lpl.arizona.edu/images/PSP/PSP_001513_1655/ ] taken by the High Resolution Imaging Science Experiment camera on Sept. 29, 2006. The full image is centered at minus 7.8 degrees latitude, 279.5 degrees east longitude. The image is oriented such that north is toward the top. The range to the target site was 297 kilometers (185.6 miles). At this distance the image scale is 29.7 centimeters (11.7 inches) per pixel (with 1 by 1 binning), so objects as small as about 89 centimeters (35 inches) across are resolved. The image was taken at 3:30 p.m. local Mars time. The scene is illuminated from the west with a solar-incidence angle of 59.7 degrees, which means the sun was about 30.3 degrees above the horizon. When the image was taken, the season on Mars was southern winter. |
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