Stereo Pairs 
An explanation of stereo pairs and their use (PDF)  

Planned stereo pairs have suitable stereo convergence angles and illumination by design. In addition to planned stereo pairs, the Pairendipity software can identify overlapping HiRISE images that are serendipitously suitable for stereo processing and find stereo pairs within the CTX dataset.

Planned HiRISE stereo pairs are listed in the “Stereo Pair List (CSV)” link below. Since this list is based on produced stereo anaglyphs it also contains a few serendipitous pairs that underwent special processing. Most serendipitous HiRISE stereo pairs are listed in the “Pairendipity Stereo” link, while CTX stereo pairs are listed in “Pairendipity CTX Stereo”.

Images taken close together in time minimize illumination and frost differences and are especially useful (see the Delta-Days column in the Pairendipity files or difference the orbit numbers in the image IDs in the Stereo Pair List file). Stereo pairs with both images planned within the same 14-day (168-orbit) operations cycle are known as SPORCs.

Layering in Wall of Orson Welles Crater:   ESP_065396_1800   ESP_073600_1800   (Interval in Earth days: 639)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-0.16

315.

-2.7

8.009

56.8

56.9

Dune Field in Nili Fossae:   ESP_065418_2015   ESP_065352_2015   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
21.13

74.2

-24.

-10.0

68.2

67.0

Hydrous Mineral-Rich Terrain:   ESP_065417_1800   ESP_065760_1800   (Interval in Earth days: 27)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
0.044

101.

0.01

-19.4

56.5

55.8

Gullies and Arcuate Ridges in Nereidum Montes:   ESP_065502_1400   ESP_065436_1400   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-39.5

307.

-8.7

5.813

50.6

50.5

Layers in Valles Marineris Wall:   ESP_065449_1675   ESP_066135_1675   (Interval in Earth days: 53)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-12.1

309.

-0.0

-25.1

52.4

47.6

Terrain Sample:   ESP_065392_1590   ESP_065735_1590   (Interval in Earth days: 27)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-20.6

67.5

-8.7

-26.7

52.0

49.9

Sinuous Channel Form on South Rim of Baldet Crater:   ESP_065339_2015   ESP_066236_2015   (Interval in Earth days: 70)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
21.43

65.7

24.4

12.89

64.7

62.1

Gullies with Terminal Ridges in Terra Cimmeria:   ESP_065323_1330   ESP_065732_1330   (Interval in Earth days: 32)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-46.4

153.

-0.8

-27.4

53.8

50.3

Possible Phyllosilicate-Rich Terrain in Nirgal Vallis and Gully Monitoring:   ESP_065330_1505   ESP_065752_1505   (Interval in Earth days: 32)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-29.0

320.

-8.0

15.14

52.1

45.2

Layers in Crater:   ESP_065354_1890   ESP_065974_1890   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
8.820

20.8

-6.1

-22.4

60.8

58.8


  


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