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Mountains and buried ice on Mars
 
2 December 2011

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Phlegra Montes is a range of gently curving mountains and ridges on Mars. They extend from the northeastern portion of the Elysium volcanic province to the northern lowlands. This image is centred at 33°N/162°E. The High-Resolution Stereo Camera (HRSC) on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465. The images have a ground resolution of about 16 m per pixel.

Credits: ESA/DLR/FU Berlin (G. Neukum)
 
 
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A wider contextual image of the region surrounding Phlegra Montes. The smaller rectangle shows the region covered in this Mars Express HRSC image release.

Credits: NASA MGS MOLA Science Team
 
 
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Phlegra Montes is a range of gently curving mountains and ridges on Mars. Flow patterns attributable to water are widely visible across the image. Linear flow patterns can be seen inside the valley (Box 1). Nearly every mountain is surrounded by an apron of rocky debris (Box 2). Over time, this debris appears to have moved down the mountainside and looks similar to the debris found covering glaciers here on Earth. Lobe-shaped structures seen inside impact craters in the region (Box 3) are known as concentric crater fill and are perhaps another indication of subsurface water ice. The High-Resolution Stereo Camera on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465.

Credits: ESA/DLR/FU Berlin (G. Neukum)
 
 
Download:
 HI-RES JPEG (Size: 1027 kb)  HI-RES TIFF (Size: 70 510 kb)
Phlegra Montes is a range of gently curving mountains and ridges on Mars. They extend from the northeastern portion of the Elysium volcanic province to the northern lowlands. This image is centred at 33°N/162°E. The image was created using a Digital Terrain Model (DTM) obtained from the High-Resolution Stereo Camera on ESA’s Mars Express spacecraft. Elevation data from the DTM is colour coded: purple indicates the lowest lying regions and grey the highest. The scale is in metres. The High-Resolution Stereo Camera (HRSC) on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465.

Credits: ESA/DLR/FU Berlin (G. Neukum)
 
 
Download:
 HI-RES JPEG (Size: 755 kb)  HI-RES TIFF (Size: 24 462 kb)
Phlegra Montes is a range of gently curving mountains and ridges on Mars. They extend from the northeastern portion of the Elysium volcanic province to the northern lowlands. The High-Resolution Stereo Camera on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465. The images have a ground resolution of about 16 m per pixel. It was derived from the nadir channel, which provides the highest detail of all the channels.

Credits: ESA/DLR/FU Berlin (G. Neukum)
 
 
Download:
 HI-RES JPEG (Size: 829 kb)  HI-RES TIFF (Size: 25 361 kb)
Phlegra Montes is a range of gently curving mountains and ridges on Mars. They extend from the northeastern portion of the Elysium volcanic province to the northern lowlands. The High-Resolution Stereo Camera on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465. This perspective view has been calculated from the Digital Terrain Model derived from the stereo channels.

Credits: ESA/DLR/FU Berlin (G. Neukum)
 
 
Download:
 HI-RES JPEG (Size: 792 kb)  HI-RES TIFF (Size: 25 879 kb)
Phlegra Montes is a range of gently curving mountains and ridges on Mars. They extend from the northeastern portion of the Elysium volcanic province to the northern lowlands. The High-Resolution Stereo Camera on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465. This perspective view has been calculated from the Digital Terrain Model derived from the stereo channels.

Credits: ESA/DLR/FU Berlin (G. Neukum)
 
 
Download:
 HI-RES JPEG (Size: 1061 kb)  HI-RES TIFF (Size: 51 734 kb)
Phlegra Montes is a range of gently curving mountains and ridges on Mars. They extend from the northeastern portion of the Elysium volcanic province to the northern lowlands. The High-Resolution Stereo Camera on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465. The image combines data from the nadir channel and one stereo channel to produce this 3D image. Stereoscopic glasses are required to see the 3D effect.

Credits: ESA/DLR/FU Berlin (G. Neukum)
 
 
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