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.

Contact between Polygon and Massif:   PSP_005700_2200   ESP_011818_2200   (Interval in Earth days: 477)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
39.77

346.

0

-24.3

59.2

72.7

Polar Layered Deposit Stratigraphy Near Chasma Australe:   PSP_004840_0940   PSP_005078_0940   (Interval in Earth days: 19)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-86.1

94.2

20.6

6.758

64.4

67.7

Lobate Crater Ejecta:   PSP_005867_1330   ESP_011431_1330   (Interval in Earth days: 434)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-46.4

118.

0

14.15

48.3

67.4

Streamlined Hills in the Western Charitum Montes:   PSP_006902_1275   ESP_011398_1275   (Interval in Earth days: 350)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-52.1

301.

-7.0

7.062

70.2

70.9

Light-Toned Layered Rock Outcrop in Hellas Region:   PSP_006700_1385   ESP_016141_1385   (Interval in Earth days: 736)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-41.1

53.1

5.27

-12.5

58.1

68.9

Light-Toned Layered Rock Outcrop in Ladon Vallis:   PSP_006637_1590   ESP_023383_1590   (Interval in Earth days: 1305)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-20.8

330.

7.10

20.68

44.1

31.2

Mawrth Vallis Phillosilicate Layers:   PSP_005819_2050   PSP_006742_2050   (Interval in Earth days: 72)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
24.68

339.

3.35

-7.74

46.6

40.7

Layered Bedrock Exposed in the Central Uplift of Martin Crater:   PSP_005610_1585   PSP_005887_1585   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-21.4

290.

1.73

-24.8

33.4

37.3

Seasonal Monitoring:   PSP_005340_0930   PSP_005523_0930   (Interval in Earth days: 14)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-87.0

170.

0.24

20.31

72.8

73.3

Exposure of South Polar Layered Deposits:   PSP_004994_1040   PSP_005297_1040   (Interval in Earth days: 24)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-75.7

201.

2.74

25.62

58.6

60.5


  


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