Possible Inverted Meanders in Filled Channel West of Ladon Valles
NASA/JPL/University of Arizona
Possible Inverted Meanders in Filled Channel West of Ladon Valles
ESP_014100_1600  Science Theme: Sedimentary/Layering Processes
This is a stereo pair with ESP_011476_1600.
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Acquisition date
30 July 2009

Local Mars time:

Latitude (centered)

Longitude (East)

Range to target site
264.5 km (165.3 miles)

Original image scale range
26.5 cm/pixel (with 1 x 1 binning) so objects ~79 cm across are resolved

Map projected scale
25 cm/pixel and North is up

Map projection

Emission angle:

Phase angle:

Solar incidence angle
33°, with the Sun about 57° above the horizon

Solar longitude
312.4°, Northern Winter

North azimuth:

Sub-solar azimuth:
Black and white
map projected  non-map

IRB color
map projected  non-map

Merged IRB
map projected

Merged RGB
map projected

RGB color
non-map projected

Black and white
map-projected   (980MB)

IRB color
map-projected   (405MB)

Black and white
map-projected  (485MB)
non-map           (534MB)

IRB color
map projected  (186MB)
non-map           (434MB)

Merged IRB
map projected  (254MB)

Merged RGB
map-projected  (244MB)

RGB color
non map           (455MB)
Map-projected, reduced-resolution
Full resolution JP2 download
Anaglyph details page

B&W label
Color label
Merged IRB label
Merged RGB label
EDR products

IRB: infrared-red-blue
RGB: red-green-blue
About color products (PDF)

Black & white is 5 km across; enhanced color about 1 km
For scale, use JPEG/JP2 black & white map-projected images

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NASA/JPL/University of Arizona

For information about NASA and agency programs on the Web, visit: http://www.nasa.gov. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, Calif., 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. The image data were processed using the U.S. Geological Survey’s ISIS3 software.