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.

Possible MSL Landing Site in Gale Crater:   ESP_018854_1755   ESP_018920_1755   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-4.58

137.

5.54

-18.0

56.2

57.8

Channelized Lava Flow through a Constriction with Well-Preserved Highstands:   ESP_018945_2050   ESP_019235_2050   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
24.82

171.

-15.

9.257

48.8

48.4

Central Structure of Jorn Crater:   ESP_019186_1525   ESP_025199_1525   (Interval in Earth days: 469)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-27.1

76.4

0

-29.5

67.8

62.4

Well-Preserved Crater Northeast of Hellas Planitia:   ESP_019120_1585   ESP_027678_1585   (Interval in Earth days: 667)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-21.2

77.3

3.42

-7.57

64.5

65.6

Layered Terrains in Aeolis Planum:   ESP_018972_1755   ESP_019605_1755   (Interval in Earth days: 50)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-4.27

154.

15.7

-5.86

55.1

56.0

Cluster of Zunil Crater Secondaries:   ESP_019064_1835   ESP_019209_1835   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
3.656

163.

2.92

17.53

52.6

51.6

Steep North Polar Boundary Scarp:   ESP_018928_2640   ESP_019034_2640   (Interval in Earth days: 8)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
83.79

237.

7.24

-7.09

65.4

67.3

Abrupt Transition in Expression of North Polar Basal Stratigraphy:   ESP_018898_2645   ESP_019215_2645   (Interval in Earth days: 24)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.25

342.

0

-13.9

65.7

70.4

Syrtis Major Planum Channel and Depression:   ESP_018988_1980   ESP_042882_1980   (Interval in Earth days: 1861)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.54

76.5

0

-26.9

48.6

42.2

Central Chasma Boreale Scarp:   ESP_018859_2645   ESP_019043_2645   (Interval in Earth days: 14)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.57

343.

-15.

-1.04

66.4

67.7


  


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