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.

High-Latitude Exposure of North Polar Layered Deposits:   ESP_019117_2720   ESP_019050_2720   (Interval in Earth days: 6)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.74

6.00

-13.

-23.1

73.5

73.7

Central Structure of Jorn Crater:   ESP_019186_1525   ESP_025199_1525   (Interval in Earth days: 469)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-27.1

76.4

0

-29.5

67.8

62.4

Translucent Ice on Dunes:   ESP_019006_2550   ESP_019243_2550   (Interval in Earth days: 18)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
74.97

300.

-21.

3.245

63.1

64.3

Gemina Lingula Scarp with Outcrop of Layered Deposits and Unconformities:   ESP_018844_2605   ESP_019081_2605   (Interval in Earth days: 19)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
80.37

27.0

1.70

16.54

62.6

64.5

Steep North Polar Boundary Scarp:   ESP_018943_2655   ESP_019181_2655   (Interval in Earth days: 19)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
85.36

186.

0

-13.2

67.0

70.6

Well-Preserved Impact Crater in Arabia Terra:   ESP_019162_1975   ESP_019439_1975   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.23

5.48

7.48

-19.6

48.9

52.7

Steep North-Polar Boundary Scarp:   ESP_018957_2655   ESP_019195_2655   (Interval in Earth days: 19)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
85.25

160.

3.29

-9.91

67.0

70.5

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

Cluster of Zunil Crater Secondaries:   ESP_019064_1835   ESP_019209_1835   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
3.656

163.

2.92

17.53

52.6

51.6

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


  


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