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.

Possible Mud Volcanoes Located in Acidalia Planitia:   ESP_024227_2240   ESP_024359_2240   (Interval in Earth days: 10)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
43.66

318.

23.1

-2.47

48.5

48.7

Lava Flow Oozing into a Crater:   ESP_024587_1465   ESP_024877_1465   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-33.2

222.

7.47

28.63

55.5

58.7

Field of Transverse Aeolian Ridges in Proctor Crater:   ESP_024449_1320   ESP_024515_1320   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-47.7

31.0

21.9

4.433

63.1

65.1

Mawrth Vallis Stratigraphy Exposed:   ESP_024200_2045   ESP_024055_2045   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
24.47

341.

1.71

-15.1

39.2

41.2

Gullies on the South Wall of Dao Vallis near the Confluence with Niger Vallis:   ESP_024315_1435   ESP_031818_1435   (Interval in Earth days: 584)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-36.1

90.2

-5.0

8.408

53.9

35.4

Colorful Central Peak in an Unnamed Crater:   ESP_023674_1590   ESP_024597_1595   (Interval in Earth days: 72)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-20.5

306.

6.77

24.62

34.8

46.2

Rugged Banded Material in Crater in Northwest Hellas Planitia:   ESP_023789_1420   ESP_024066_1420   (Interval in Earth days: 21)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-37.7

47.4

21.8

0.082

44.7

50.6

Libya Montes Layered Cliffs:   ESP_023827_1835   ESP_024671_1835   (Interval in Earth days: 65)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
3.427

85.9

11.0

-9.63

32.7

38.9

Gullies with Debris Aprons:   ESP_023810_1395   ESP_023955_1395   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-40.4

196.

0.83

14.61

48.1

49.7

South Polar Residual Cap in Late Summer:   ESP_023677_0920   ESP_023781_0920   (Interval in Earth days: 8)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-88.0

298.

11.1

22.62

84.1

84.5


  


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