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.

Northern Plains Craters:   ESP_026446_2305   ESP_027158_2305   (Interval in Earth days: 55)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
50.09

219.

0

16.82

42.3

43.0

Complex Superposition of Fractures:   ESP_026286_2235   ESP_026563_2235   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
43.31

269.

-3.0

-21.3

41.0

43.0

Fresh Crater:   ESP_026365_2260   ESP_027710_2260   (Interval in Earth days: 105)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
45.42

271.

1.37

20.86

41.0

45.7

Exposure of Nili Fossae Megabreccias:   ESP_026346_2000   ESP_026491_2000   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
19.73

74.0

1.32

16.62

42.9

42.0

Bedform Changes Southwest of Schiaparelli Crater:   ESP_026322_1720   ESP_027166_1720   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-7.72

13.0

-3.6

-18.2

56.9

59.2

Southern Ladon Basin near the Mouth of Ladon Valles:   ESP_026139_1600   ESP_027616_1600   (Interval in Earth days: 115)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-19.8

329.

5.17

-12.8

63.6

65.3

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

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

Light-Toned Hydrated Material along Melas Chasma Wallrock and Floor:   ESP_026088_1710   ESP_026022_1710   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.11

282.

-11.

12.10

57.1

55.2


  


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