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.

Exposure of North Polar Layered Deposits:   ESP_035567_2650   ESP_035909_2650   (Interval in Earth days: 27)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.92

294.

0.21

15.65

60.1

60.9

Crater on Wall in Mamers Valles:   ESP_035341_2195   ESP_035631_2195   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
39.35

16.4

3.18

25.38

41.5

40.2

Landform Transition from Chaos Terrain to Outflow Channel:   ESP_035475_1830   ESP_036042_1830   (Interval in Earth days: 44)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
2.839

323.

-6.8

6.109

53.2

53.2

Possible Phyllosilicates in Nili Fossae:   ESP_035484_2025   ESP_037106_2025   (Interval in Earth days: 126)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
22.44

74.9

1.37

-18.5

44.3

53.9

Characterize Distal Alluvial Fan Slopes:   ESP_035468_1755   ESP_045398_1755   (Interval in Earth days: 773)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-4.70

154.

6.76

-20.1

56.5

54.1

Cratered Cones in Western Elysium Planitia:   ESP_035521_1825   ESP_043987_1825   (Interval in Earth days: 659)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
2.375

146.

8.82

22.29

52.4

48.1

Possible Small Exhumed Craters in Aeolis Dorsa:   ESP_035389_1740   ESP_037301_1740   (Interval in Earth days: 149)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-5.79

153.

-11.

-0.59

58.2

57.4

Exposure of North Polar Layered Deposits:   ESP_035530_2665   ESP_044841_2665   (Interval in Earth days: 725)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
86.61

200.

0.27

-9.62

61.5

63.4

Candidate Future Landing Site in Jezero Crater:   ESP_035563_1990   ESP_035629_1990   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
18.61

77.9

10.8

-9.74

45.0

46.8

Western Half of Well-Preserved Gullied Crater:   ESP_035448_2175   ESP_035527_2175   (Interval in Earth days: 6)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
37.34

335.

2.41

28.32

41.9

39.6


  


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