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Mars Odyssey Orbiter, 3D Model

April 27, 2019

Click (or touch) and drag to interact with this 3D model of Mars Odyssey.

Learn more about the mission at mars.nasa.gov/odyssey/

Credits

NASA/JPL-Caltech

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Part of a multispectral THEMIS infrared image of Nili Patera caldera on Syrtis Major has been superimposed on a high-resolution THEMIS visual image.
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Part of a multispectral THEMIS infrared image of Nili Patera caldera on Syrtis Major has been superimposed on a high-resolution THEMIS visual image.
Nili Patera and Dacite Lava Flow
This view combines information from two instruments on NASA's Mars Reconnaissance Orbiter to map color-coded composition over the shape of the ground in a small portion of the Nili Fossae plains re...
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This view combines information from two instruments on a NASA Mars orbiter to map color-coded composition over the shape of the ground within the Nili Fossae plains region of Mars. Carbonate-rich deposits in this area (coded green) hold some carbon formerly in the atmosphere's carbon dioxide.
Rocks Here Sequester Some of Mars' Early Atmosphere
Although this may look like a hostile alien life form, it's actually a complex line of sand dunes near the northern ice cap of Mars.
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Although this may look like a hostile alien life form, it's actually a complex line of sand dunes near the northern ice cap of Mars.
Mars Odyssey All Stars: Reptilian Dunes
This image of Phobos is one product of the first pointing at that Martian moon by the THEMIS camera on NASA's Mars Odyssey orbiter.  The Sept. 29, 2017, observation also provided information about ...
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Martian Moon Phobos Observed by NASA's Odyssey
Martian Moon Phobos Observed by NASA's Odyssey
A false-color mosaic focuses on one junction in Noctis Labyrinthus where Mars canyons meet to form a depression 4,000 meters (13,000 feet) deep.
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A false-color mosaic focuses on one junction in Noctis Labyrinthus where Mars canyons meet to form a depression 4,000 meters (13,000 feet) deep.
Canyon Junction
Wind shadow and real shadow combine to give a striking image of a comet.
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Wind shadow and real shadow combine to give a striking image of a comet.
THEMIS Images as Art
This false color image shows a region with craters of different ages located at the margin of Acidalia Planitia. This image was collected during the Northern Spring season.
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This false color image shows a region with craters of different ages located at the margin of Acidalia Planitia. This image was collected during the Northern Spring season. The THEMIS VIS camera is capable of capturing color images of the Martian surface using five different color filters. In this mode of operation, the spatial resolution and coverage of the image must be reduced to accommodate the additional data volume produced from using multiple filters. To make a color image, three of the five filter images (each in grayscale) are selected. Each is contrast enhanced and then converted to a red, green, or blue intensity image. These three images are then combined to produce a full color, single image. Because the THEMIS color filters don't span the full range of colors seen by the human eye, a color THEMIS image does not represent true color. Also, because each single-filter image is contrast enhanced before inclusion in the three-color image, the apparent color variation of the scene is exaggerated. Nevertheless, the color variation that does appear is representative of some change in color, however subtle, in the actual scene. Note that the long edges of THEMIS color images typically contain color artifacts that do not represent surface variation.
Cratered Acidalia Planitia
A "Grand Canyon of Mars" slices across the Red Planet near its equator.
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1128_LA_Basin.jpg
Mars Canyon with Los Angeles for Scale
Just as on Earth, volcanism and tectonism are found together on Mars. Here is an example: the ridges and fractures of Claritas Fossae are affecting or perhaps hosting the volcanic flows of Solis Pl...
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Just as on Earth, volcanism and tectonism are found together on Mars. Here is an example: the ridges and fractures of Claritas Fossae are affecting or perhaps hosting the volcanic flows of Solis Planum.
Volcanism & Tectonism
Newly detailed mapping of local variations in Mars' gravitational pull on orbiters (center), combined with topographical mapping of the planet's mountains and valleys (left), yields the best-yet ma...
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Newly detailed mapping of local variations in Mars' gravitational pull on orbiters (center), combined with topographical mapping of the planet's mountains and valleys (left), yields the best-yet mapping of Mars' crustal thickness (right).
Using Gravity and Topography to Map Mars' Crustal Thickness
Bacolor Crater is a magnificent impact feature about 20 kilometers (12 miles) wide.
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Bacolor Crater is a magnificent impact feature about 20 kilometers (12 miles) wide.
Mars Odyssey All Stars: Bacolor Crater
NASA's Mars Odyssey spacecraft passes above Mars' south pole in this artist's concept illustration. The spacecraft has been orbiting Mars since October 24, 2001.
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NASA's Mars Odyssey spacecraft passes above Mars' south pole in this artist's concept illustration. The spacecraft has been orbiting Mars since October 24, 2001.
Odyssey over Mars' South Pole
This THEMIS visible image shows a close-up view of the ridged plains in Hesperia Planum. This region is the classic locality for martian surfaces that formed in the "middle ages" of martian history.
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This THEMIS visible image shows a close-up view of the ridged plains in Hesperia Planum. This region is the classic locality for martian surfaces that formed in the "middle ages" of martian history. The absolute age of these surfaces is not well known. However, using the abundance of impact craters, it is possible to determine that the Hesperian plains are younger than the ancient cratered terrains that dominate the southern hemisphere, and are older than low-lying plains of the northern hemisphere. In this image it is possible to see that this surface has a large number of 1-3 km diameter craters, indicating that this region is indeed very old and has subjected to a long period of bombardment. A large (80 km diameter) crater occurs just to the north (above) this image. The material that was thrown out onto the surface when the crater was formed ("crater ejecta") can be seen at the top of the THEMIS image. This ejecta material has been heavily eroded and modified since its formation, but there are hints of lobate flow features within the ejecta. Lobate ejecta deposits are thought to indicate that ice was present beneath the surface when the crater was formed, leading to these unusual lobate features. Many of the Hesperian plains are characterized by ridged surfaces. These ridges can be easily seen in the MOLA context image, and several can be seen cutting across the lower portion of the THEMIS image. These "wrinkle" ridges are thought to be the result of compression (squeezing) of the lavas that form these plains.
Hesperia Planum
Martian surface frost, made up largely of carbon dioxide, appears blueish-white in these images from the Thermal Emission Imaging System (THEMIS) camera aboard NASA’s 2001 Odyssey orbiter. THEMIS t...
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Martian surface frost, made up largely of carbon dioxide, appears blueish-white in these images from the Thermal Emission Imaging System (THEMIS) camera aboard NASA’s 2001 Odyssey orbiter. THEMIS takes images in both visible light perceptible to the human eye and heat-sensitive infrared.
Four Images of Morning Frost on Mars
Mars Odyssey Project Manager Gaylon McSmith, of NASA's Jet Propulsion Laboratory
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Mars Odyssey Project Manager Gaylon McSmith, of NASA's Jet Propulsion Laboratory
Mars Odyssey Project Manager Gaylon McSmith
A group of small, unnamed craters in the martian southern hemisphere is the first site captured by a group of middle school students who are operating the camera system onboard NASA's Mars Odyssey ...
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Students looking at a computer while participating in the Mars Student Imaging Project
Students participating in the Mars Student Imaging Project
Large fractures have formed 'steps' in this region of Tempe Terra.
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Large fractures have formed 'steps' in this region of Tempe Terra.
Tempe Terra
Download a PDF of the Mars as Art Booklet.
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Mars as Art
Mars as Art (2013)
Geological faulting has opened cracks in the Cerberus region that slice through flat plains and mesas alike.
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Geological faulting has opened cracks in the Cerberus region that slice through flat plains and mesas alike.
Mars Odyssey All Stars: Cerberus Crack
THEMIS Support for Landing Site Selection
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THEMIS Support for Landing Site Selection
THEMIS Support for Landing Site Selection
Western flank of Elysium Mons.
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Western flank of Elysium Mons.
Elysium Mons
This region of Terra Sabaea contains areas with high densities of small craters.
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This region of Terra Sabaea contains areas with high densities of small craters.
Lot of Craters in Terra Sabaea
This lava channel is part of the Elysium Mons flows.
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This lava channel is part of the Elysium Mons flows.
Lava Channel
Seen shortly after local Martian sunrise, clouds gather in the summit pit, or caldera, of Pavonis Mons, a giant volcano on Mars, in this image from the Thermal Emission Imaging System (THEMIS) on N...
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Seen shortly after local Martian sunrise, clouds gather in the summit pit, or caldera, of Arsia Mons, a giant volcano on Mars, in this image from the Thermal Emission Imaging System (THEMIS) on NASA's Mars Odyssey orbiter.
Morning Clouds Atop Martian Mountain
Five decades of successful NASA missions to the Red Planet, 1965-2015.
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50 Years of Mars Exploration
50 Years of Mars Exploration

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