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.

How Did Valles Marineris Form?:   ESP_025415_1675   ESP_026259_1675   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-12.3

294.

0

-17.9

53.1

60.5

A Volcanic Pit Chain and Dust Avalanches :   ESP_026249_2025   ESP_026750_2025   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
22.26

202.

-7.3

17.82

42.6

41.8

Intersection of Ridges in Pavonis Mons:   ESP_025997_1850   ESP_026630_1850   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
4.788

244.

0

-19.2

47.9

51.6

Cut Crater and Fault Scarp along Candor Chasma:   ESP_026114_1745   ESP_025547_1745   (Interval in Earth days: 44)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-5.51

290.

5.32

-4.4

53.9

50.6

Oudemans Crater Layered Central Uplift:   ESP_026194_1700   ESP_026339_1700   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.86

268.

-8.2

8.812

57.9

57.5

Terrain with Layered Material and Circular Pits:   ESP_025976_2290   ESP_026464_2290   (Interval in Earth days: 38)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
48.73

91.1

1.38

-19.8

42.0

43.7

Fan with Light-Toned Deposits:   ESP_025990_1995   ESP_026135_1995   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
19.10

76.1

-27.

-15.8

44.5

43.8

Source Area for Channel Network Near Gigas Sulci:   ESP_025905_1980   ESP_026327_1980   (Interval in Earth days: 32)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.74

232.

19.4

5.703

40.5

43.1

Light-Toned Material along Coprates Chasma Wallrock and Plateau:   ESP_025929_1645   ESP_026430_1645   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-15.5

303.

-6.5

17.74

60.0

61.1

Dark Slope Streak Extending to Channel Floor:   ESP_026064_2045   ESP_026697_2045   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
24.17

212.

0

-15.4

41.0

44.0


  


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