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.

Layered Terrain in Aeolis Planum:   ESP_018181_1730   ESP_018893_1730   (Interval in Earth days: 55)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-6.83

152.

-5.0

11.41

58.6

56.8

Flank and Summit of Low Shield Volcano East of Jovis Tholus:   ESP_018283_1980   ESP_019272_1980   (Interval in Earth days: 77)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.89

243.

8.11

-7.55

45.8

50.6

Mass Wasting on Steep North-Polar Boundary Scarp:   ESP_018115_2640   ESP_018932_2640   (Interval in Earth days: 63)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
83.82

121.

-0.2

13.54

59.8

65.3

Cerberus Fossae Fissure and Lava Flows:   ESP_018141_1965   ESP_018774_1965   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
16.06

160.

6.15

-13.7

46.3

49.4

North Polar Layered Deposits:   ESP_018192_2680   ESP_019048_2680   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.96

177.

-17.

-10.5

63.7

70.6

Pattern with Cracks and Fans Similar To Those in the South Defrosted:   ESP_018275_2570   ESP_018644_2570   (Interval in Earth days: 29)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
76.60

89.5

-4.7

9.675

56.3

58.0

Well-Preserved 5-Kilometer Diameter Crater South of Isidis Planitia:   ESP_018447_1750   ESP_018948_1750   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-5.18

90.0

-4.4

18.17

57.6

55.4

Cones at Edge of North Polar Layered Deposits:   ESP_018333_2605   ESP_018926_2605   (Interval in Earth days: 46)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
80.20

295.

6.93

22.29

58.1

62.3

Pitted Terrain North of Hrad Vallis:   ESP_018168_2160   ESP_019012_2160   (Interval in Earth days: 65)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
35.59

141.

-3.2

-24.7

43.1

50.1

Exposure of Putative Deformation in North Polar Layers:   ESP_018361_2655   ESP_018810_2655   (Interval in Earth days: 35)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
85.20

242.

-4.5

-18.9

62.0

66.4


  


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