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.

Pit Crater:   ESP_013167_1785   ESP_013589_1785   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-1.32

239.

-7.4

-22.9

49.4

45.4

Phyllosilicate and Possible Chlorite Prehnite Northwest of Hellas Region:   ESP_012765_1535   ESP_013477_1535   (Interval in Earth days: 55)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-26.2

56.4

7.51

22.87

45.6

35.6

Layering on Floor of Noctis Labyrinthus Pit:   ESP_014076_1680   ESP_021513_1680   (Interval in Earth days: 579)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-11.8

263.

-5.4

13.21

35.2

46.5

Possible Rootless Cones in Hydraotes Chaos:   ESP_013177_1800   ESP_021458_1800   (Interval in Earth days: 645)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
0.053

326.

-4.9

-21.2

49.8

53.9

Phyllosilicate Diversity North of Mawrth Vallis:   ESP_013150_2070   ESP_014139_2070   (Interval in Earth days: 77)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
26.60

340.

-8.4

-22.7

66.9

56.2

Well-Preserved 8 Kilometer Diameter Crater:   ESP_013650_1230   ESP_013927_1230   (Interval in Earth days: 21)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-56.4

20.2

1.13

-19.3

45.0

47.6

Central Structure of a Large Impact Crater:   ESP_013134_1610   ESP_021494_1610   (Interval in Earth days: 652)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-18.6

62.6

-6.3

14.94

43.1

44.9

Layered Sinuous Ridge in Argyre Planitia:   ESP_012848_1235   ESP_012782_1235   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-56.2

316.

-7.0

6.567

50.2

50.1

Gullies:   ESP_012722_1400   ESP_012867_1400   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-39.6

153.

-6.2

7.111

47.5

44.4

Relatively Fresh 1-Kilometer Diameter Crater in South Polar Region :   ESP_013699_1055   ESP_013923_1055   (Interval in Earth days: 18)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-74.1

130.

-4.9

10.22

57.2

58.2


  


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