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.

Mass Movement on Wall of Crater in Lyot Crater Ejecta Blanket:   ESP_019438_2340   ESP_027231_2340   (Interval in Earth days: 607)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
53.55

26.3

-5.5

13.83

57.7

44.7

Fresh 3-Kilometer Diameter Rayed Crater:   ESP_019346_1690   ESP_020190_1690   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-11.0

25.8

3.75

-16.5

58.4

57.3

Alpine Glacier:   ESP_019213_2210   ESP_019503_2210   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
40.86

51.3

-8.0

14.46

51.2

52.7

Possible Fluvial Features in West Hellas Planitia:   ESP_019042_1450   ESP_019187_1450   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-34.8

48.5

4.88

17.60

73.2

71.3

Dunes on Cemented Substrate:   ESP_019130_2600   ESP_019157_2600   (Interval in Earth days: 2)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
79.98

122.

27.5

2.09

64.3

66.1

North Polar Trough Stratigraphy:   ESP_019102_2660   ESP_018496_2660   (Interval in Earth days: 47)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
85.86

179.

-12.

-22.1

69.8

64.4

North Polar Layered Deposits:   ESP_018961_2670   ESP_019145_2670   (Interval in Earth days: 15)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
86.71

73.6

-18.

-9.58

68.9

70.7

Change Detection in Aeolis Planum:   ESP_019038_1740   ESP_019882_1740   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-6.07

153.

9.19

-15.2

56.3

56.9

Steep North-Polar Boundary Scarp:   ESP_018905_2650   ESP_019222_2650   (Interval in Earth days: 25)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.99

151.

-3.6

-15.5

66.5

71.1

Possible Future Landing Site in Antoniadi Crater:   ESP_018883_2010   ESP_019305_2010   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
20.51

63.0

-1.7

-16.7

47.8

51.3


  


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