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.

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

Channels in Tharsis Region:   ESP_018349_2005   ESP_019338_2005   (Interval in Earth days: 77)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
20.50

241.

7.35

-7.99

45.2

50.8

Columbus Crater:   ESP_018351_1510   ESP_018496_1510   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-28.7

194.

-7.0

8.364

73.0

71.7

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

Cones at Edge of North Polar Layered Deposits:   ESP_018387_2600   ESP_026576_2600   (Interval in Earth days: 638)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
79.99

270.

-8.4

-24.5

59.2

58.2

Layered Flow Ejecta in Terra Cimmeria:   ESP_018379_1695   ESP_018880_1695   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-10.4

146.

6.62

27.95

60.0

57.5

Steep North-Polar Boundary Scarp:   ESP_018190_2640   ESP_018941_2640   (Interval in Earth days: 59)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.01

230.

1.83

15.95

60.1

65.4

Protonilus Mensae Fretted Terrain:   ESP_018448_2250   ESP_062913_2250   (Interval in Earth days: 3465)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
44.85

56.1

-3.9

7.677

45.1

46.8

Cones at Edge of North Polar Layered Deposits:   ESP_018109_2580   ESP_026654_2580   (Interval in Earth days: 666)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
77.90

298.

-0.4

-19.2

56.1

56.6

High-Latitude Exposure of North Polar Layered Deposits:   ESP_018380_2680   ESP_018605_2680   (Interval in Earth days: 18)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.84

70.4

-12.

-20.4

64.4

66.3


  


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