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.

Loose Cluster of Zunil Crater Secondary Craters:   PSP_003874_1815   PSP_004375_1815   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
1.259

162.

4.39

27.49

53.1

47.0

Low Shield with Radial Flows East of the Olympica Fossae:   PSP_003818_2040   PSP_004108_2040   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
23.71

249.

-3.0

23.54

66.1

63.7

Light-Toned Layering in Ius Chasma:   PSP_003593_1725   ESP_058000_1725   (Interval in Earth days: 4239)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-7.48

275.

4.77

-11.1

51.7

34.5

Gullies Produced by Possible Snow/Ice Melting:   PSP_004192_2195   ESP_012446_2195   (Interval in Earth days: 643)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
38.96

116.

-0.0

13.62

75.6

74.8

Glacial-Like Fractures in Proposed Glacial Ice in Arsia Mons Depression:   PSP_004201_1735   PSP_005256_1735   (Interval in Earth days: 83)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-6.62

236.

8.32

-25.5

46.4

37.5

Boulders on Lobate Ejecta:   PSP_003484_1305   PSP_003563_1305   (Interval in Earth days: 7)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-49.3

18.5

-7.9

19.01

55.3

52.1

Geologic Contact Between Wallrock and Light-Toned Layered Deposits:   PSP_004344_1715   PSP_005623_1715   (Interval in Earth days: 100)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-8.25

293.

-3.3

15.97

44.8

32.1

Rotational Landslides or Slumps along the Walls of Bahram Vallis:   PSP_003460_2015   PSP_003605_2015   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
21.26

303.

-1.0

12.74

64.1

63.5

Phyllosilicate-Rich Area:   PSP_004329_2045   ESP_013282_2045   (Interval in Earth days: 698)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
24.37

338.

-2.8

-25.9

64.5

65.4

Western Region of Zunil Crater:   PSP_004309_1880   ESP_020211_1880   (Interval in Earth days: 1239)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
7.728

166.

4.71

29.29

53.1

52.5


  


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