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.

Double Crater on Cerberus Plains:   PSP_009860_1805   ESP_042892_1805   (Interval in Earth days: 2574)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
0.433

164.

-5.2

-19.3

56.0

46.7

Mounds in Ulysses Fossae:   PSP_009409_1860   PSP_009554_1860   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
5.804

237.

-7.2

8.646

53.1

52.1

High-Latitude Exposure of North Polar Layered Deposits:   PSP_010163_2675   PSP_010230_2675   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.26

123.

-8.3

-20.4

69.1

70.5

Pit and Channel on Southwestern Pavonis Mons:   PSP_009923_1785   PSP_010213_1785   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-1.67

246.

-21.

14.06

58.1

55.7

Light-Toned Layering in Plains South of Melas Chasma:   PSP_009948_1700   ESP_015961_1700   (Interval in Earth days: 469)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.89

282.

5.17

-11.2

60.5

46.6

Distributaries From Athabasca Valles:   PSP_009768_1880   PSP_010045_1880   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
7.721

154.

7.98

-19.7

51.6

54.3

Bedrock Layers Exposed in Northern Hellas Basin:   PSP_009389_1510   PSP_010022_1510   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-28.8

67.0

0

-18.6

73.7

73.1

Cones at Edge of North Polar Layered Deposits:   PSP_009947_2590   PSP_009710_2590   (Interval in Earth days: 18)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
78.66

285.

8.81

-10.7

60.4

59.6

Sample Artynia Catena:   PSP_009646_2265   ESP_016305_2265   (Interval in Earth days: 519)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
46.32

240.

0

16.73

45.9

43.9

High-Latitude Exposure of North Polar Layered Deposits:   PSP_010139_2675   PSP_010483_2675   (Interval in Earth days: 27)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.32

55.3

-8.6

-21.3

68.8

73.9


  


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