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.

Delta Structure in Eberswalde Crater:   PSP_001336_1560   PSP_001534_1560   (Interval in Earth days: 15)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-23.8

326.

-0.2

-15.6

67.2

67.2

Cratered Cones in the Cydonia Region:   ESP_025439_2210   ESP_025518_2210   (Interval in Earth days: 6)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
40.75

352.

1.78

27.34

40.9

38.3

Dark Deposits around a Volcanic Fissure Adjacent to Tharsis Tholus:   ESP_030440_1945   ESP_030862_1945   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
14.06

268.

-8.4

-24.4

59.2

57.1

Layers in a Crater in Nilosyrtis:   ESP_025001_2255   ESP_025911_2255   (Interval in Earth days: 71)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
44.91

69.8

-1.9

-24.2

44.4

43.3

Gullies in Southern Mid-Latitude Crater:   ESP_029963_1385   ESP_030596_1385   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-41.2

337.

8.17

-18.4

50.6

43.6

Valleys with Layered Sediments along Uplands at Ladon Valles Basin:   ESP_029871_1615   ESP_031084_1615   (Interval in Earth days: 94)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-18.5

326.

5.61

27.24

50.1

34.7

Breach between Two Troughs in Dao Vallis:   ESP_030117_1455   ESP_030895_1455   (Interval in Earth days: 60)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-34.2

92.6

-1.6

-16.8

47.9

39.1

Gullies in Southern Mid-Latitude Crater:   ESP_030016_1415   ESP_031229_1415   (Interval in Earth days: 94)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-37.9

331.

-5.4

14.22

50.2

34.8

Sediments within Valleys in Uplands Near Ladon Valles:   ESP_030082_1615   ESP_030161_1615   (Interval in Earth days: 6)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-18.4

326.

-9.9

24.27

49.2

45.6

Well-Preserved Crater Is Southern Highlands:   ESP_030111_1365   ESP_030612_1365   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-43.2

258.

-6.5

7.553

50.0

41.9


  


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