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.

Aram Chaos Mineralogical Variability:   PSP_006953_1840   ESP_085467_1840   (Interval in Earth days: 6117)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
3.900

339.

4.39

-14.5

38.8

38.0

Sinuous Pits on the Northeast Flank of Ascreaus Mons:   PSP_004899_1940   PSP_005387_1935   (Interval in Earth days: 38)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
13.58

257.

6.80

-28.3

50.2

46.4

Distal Rampart Flow Ejecta of Bacolor Crater:   PSP_006750_2130   PSP_007462_2130   (Interval in Earth days: 55)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
32.51

118.

0.23

-9.07

43.2

41.8

Wallrock and Plains Contact South of Ius Chasma:   PSP_006784_1715   PSP_006929_1715   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-8.35

276.

-7.3

5.296

41.4

42.3

Exposure of High-Latitude Polar Layered Deposits Not Well Observed:   PSP_005971_0890   PSP_005957_0910   (Interval in Earth days: 1)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-88.7

251.

18.6

19.51

83.1

82.5

Deeply-Penetrating Structure within Polar Layered Deposits:   PSP_005076_0940   PSP_005207_0940   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-86.1

172.

-8.4

5.833

69.3

69.2

Layering in Northwest-Trending Sinuous Ridge:   PSP_006875_1255   ESP_011358_1255   (Interval in Earth days: 349)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-54.0

317.

1.97

-22.9

70.7

74.6

Sinuous Features in Light-Toned Material:   PSP_006583_1775   PSP_010789_1775   (Interval in Earth days: 328)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-2.28

3.05

0

-17.1

37.2

58.5

Lobate Margin of Impact Ejecta:   PSP_006835_2085   PSP_007481_2085   (Interval in Earth days: 50)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
28.13

319.

-5.9

4.424

41.5

40.0

Valley Network along Melas Chasma Wallrock:   PSP_005663_1700   ESP_012493_1700   (Interval in Earth days: 532)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.67

282.

-4.4

-21.3

33.4

54.0


  


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