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TOPIC: Mars Reconnaissance orbiter


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RE: Mars Reconnaissance orbiter
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New images for 27 May 2008

Phoenix Lander Hardware: EDL +22
Phoenix Lander Hardware: EDL +22 (PSP_008591_2485)
HiRISE camera has acquired an image of the Phoenix landing site 22 hours after landing.

Phoenix Lander Hardware: EDL +11
Phoenix Lander Hardware: EDL +11 (PSP_008585_2915)
This is the first HiRISE observation of the Phoenix lander material on the surface, taken 11 hours after touchdown.

Descent of the Phoenix Lander
Descent of the Phoenix Lander (PSP_008579_9020)
Breathtaking image of the Phoenix Lander passing in front of Heimdall Crater on the way to its picture perfect landing.



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New images for 21 May 2008

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Polygons at the Phoenix Landing Site
Polygons at the Phoenix Landing Site (PSP_008301_2480)
Among the many science goals, Phoenix will analyse the surface dust as well as dig into an ice-rich layer.
Ridges in Huo Hsing Vallis
Ridges in Huo Hsing Vallis (PSP_008189_2080)
If water played a role in the erosion of the rock and exposure of these ridges, it would have flowed thousands or millions of years ago.
Young Impact Crater in Isidis
Young Impact Crater in Isidis (PSP_008017_2020)
The crater is fresh enough to preserve some fine textures that are eroded around other craters.
Channel into Jezero Crater Delta
Channel into Jezero Crater Delta (PSP_007925_1990)
These clues in the form and composition of the Martian surface provide insights into an ancient era when liquid water may have been more common at the surface.
Gullies of Crater Wall in Terra Sirenum
Gullies of Crater Wall in Terra Sirenum (PSP_006760_1370)
Gullies are young features that are widely thought to form from fluvial processes involving liquid water.




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New images for 14 May 2008

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Slope Streaks in the Olympus Mons Aureole
Slope Streaks in the Olympus Mons Aureole (PSP_008144_2055)
Slope streaks are features commonly found throughout the equatorial regions of Mars.

Wrinkle Ridge in Hesperia Planum
Wrinkle Ridge in Hesperia Planum (PSP_008082_1560)
Features in this image have been identified on many planets, such as Venus and Mercury, as well as on the Moon.

Light-Toned Rocks Exposed inside Crater
Light-Toned Rocks Exposed inside Crater (PSP_008075_1590)
Distinct materials within impact craters suggest that the crust on Mars may contain many units of variable composition.

Meridiani Region Layers and Phyllosilicates
Meridiani Region Layers and Phyllosilicates (PSP_008060_1770)
Aeolian processes are active here, which are visible in dunes and ripples, most likely made of basaltic sand.

Catastrophic Flood Channel of Ares Valles
Catastrophic Flood Channel of Ares Valles (PSP_007810_1885)
This image reveals unprecedented detail of an enigmatic feature on the Martian surface.

Well Preserved Impact Crater of Alba Patera
Well Preserved Impact Crater of Alba Patera (PSP_006745_2250)
The mounds of material located adjacent to the walls probably fell there during the late-stages of crater formation.






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New images for 7 May 2008

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Rayed Crater in Tharsis Region
Rayed Crater in Tharsis Region (PSP_008011_1975)
In addition to fine material, large boulders are visible in the rays surrounding this crater.

Lava Stratigraphy in the Flanks of Olympus Mons
Lava Stratigraphy in the Flanks of Olympus Mons (PSP_007946_2035)
This scarp was most likely produced by massive landslides as the volcano falls apart under its own weight.

Eroded Crater Slopes in Ancient Noachis Region
Eroded Crater Slopes in Ancient Noachis Region (PSP_007808_1575)
Valley networks often appear on the most ancient terrains, suggesting a very different world more than 3 billion years ago.

Changing Frost Patterns in Louth Crater
Changing Frost Patterns in Louth Crater (PSP_007805_2505)
This crater contains a mound covered by water frost that persists throughout the year, which is unusual for this latitude.

Jointed Rocks Near Nilosyrtis Mensae
Jointed Rocks Near Nilosyrtis Mensae (PSP_007701_2095)
An interesting aspect of the rocks at the edge of the pit is the widespread fracturing.

Frosted Crater Near Mars North Pole
Frosted Crater Near Mars North Pole (PSP_007673_2575)
Ice on Mars does not melt in the current climate, but it does expand and contract with temperature variations.

Layered Rock in Noctis Labyrinthus
Layered Rock in Noctis Labyrinthus (PSP_006745_1715)
These layers might be the same as those seen in the canyons of Valles Marineris; their origin is currently unresolved.

Mantled Craters in Terra Cimmeria
Mantled Craters in Terra Cimmeria (PSP_006736_1325)
The two craters are covered in a mantling material, which gives them a smooth appearance.




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New images for 30 April 2008

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Lava Flows at the Summit of Olympus Mons
Lava Flows at the Summit of Olympus Mons (PSP_007959_1980)
Lava Flows from Pavonis Mons
Lava Flows from Pavonis Mons (PSP_007840_1800)
Ejecta Blanket of an Impact Crater
Ejecta Blanket of an Impact Crater (PSP_007822_1415)
Defrosting Dunes in the North Polar Sand Sea
Defrosting Dunes in the North Polar Sand Sea (PSP_007801_2610)
Segment of a Crater Ray
Segment of a Crater Ray (PSP_007751_1640)
Exposed Layers in Crater Wall Near Mawrth Vallis
Exposed Layers in Crater Wall Near Mawrth Vallis (PSP_007744_2055)
North Polar Layered Deposits in Springtime
North Polar Layered Deposits in Springtime (PSP_007712_2670)



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New images for 23 April 2008

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Dissected Mantle Terrain and Scallops in Tempe Terra
Dissected Mantle Terrain and Scallops in Tempe Terra (PSP_007930_2310)
Formation of scalloped depressions may be a process that is still active today.
Layered Sediments in Hellas Planitia
Layered Sediments in Hellas Planitia (PSP_007820_1505)
The floor of Hellas includes the lowest parts of the Martian surface, and has been proposed as the site of ancient lakes or seas.

Proposed MSL Landing Site: Eberswalde Crater
Proposed MSL Landing Site: Eberswalde Crater (PSP_007270_1560)
This image covers a portion of Eberswalde Crater which has an ancient deltaic depositional setting and is a possible site for the Mars Science Laboratory.

Proposed MSL Landing Site: Mawrth Vallis - Ellipse 4
Proposed MSL Landing Site: Mawrth Vallis - Ellipse 4 (PSP_007243_2050)
The surface of Mawrth Vallis, with its rich mineral diversity including clay minerals, is scientifically compelling for the Mars Science Laboratory.

Proposed MSL Site: Holden Crater
Proposed MSL Site: Holden Crater (PSP_007191_1535)
A candidate site for the Mars Science Laboratory, the rover would drive across traversable ripples where inverted channels are evidence for past water activity.

Craters Within a Crater
Craters Within a Crater (PSP_006726_1830)
Within Schroeter Crater is another full, possibly younger crater with a sharp rim and filled with dunes.



-- Edited by Blobrana at 08:00, 2008-04-24

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New images for 16 April 2008

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North Polar Dunes
North Polar Dunes (PSP_007779_2570)
A vast sea of basaltic sand dunes surrounds the north pole in this observation.

Disappearing Dunes
Disappearing Dunes (PSP_007726_2565)
This image is of a location where the first significant change to sand dunes was reported on Mars.

Proposed MSL Landing Site in Mawrth Vallis - Ellipse 2
Proposed MSL Landing Site in Mawrth Vallis - Ellipse 2 (PSP_007612_2045)
Mawrth Vallis has a rich mineral diversity, including clay minerals that formed by the chemical alteration of rocks or loose regolith by water.

Proposed MSL Landing Site in Eberswalde Crater
Proposed MSL Landing Site in Eberswalde Crater (PSP_007481_1560)
The delta, meandering channels and the detection of phyllosilicates provides evidence for possible persistent aqueous activity on Mars.

Proposed MSL Landing Site in Mawrth Vallis - Ellipse 1
Proposed MSL Landing Site in Mawrth Vallis - Ellipse 1 (PSP_007388_2050)
Large Southern Hemisphere Gully
Large Southern Hemisphere Gully (PSP_007126_1210)
Such gullies are among the most recent landforms on Mars, and were probably carved by liquid water.

Gullies in Utopia Planitia
Gullies in Utopia Planitia (PSP_006724_2165)
Gullies are rarer in the northern hemisphere, possibly because there are fewer slopes for them on which to form.

Aeolian Playground in Smith Crater
Aeolian Playground in Smith Crater (PSP_006284_1145)
The dark color of the dunes here are probably made of basaltic sand, a volcanic rock common on Mars.




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