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.

Layers in Crater in Protonilus Mensae:   ESP_026518_2280   ESP_027863_2280   (Interval in Earth days: 105)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
47.87

53.4

5.71

26.90

41.3

47.3

Exposure of Nili Fossae Megabreccias:   ESP_026346_2000   ESP_026491_2000   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
19.73

74.0

1.32

16.62

42.9

42.0

Meridiani Planum Terrain Sample:   ESP_026283_1810   ESP_026415_1810   (Interval in Earth days: 10)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
1.156

354.

26.9

-16.8

49.2

52.9

Eastern Rim of Karzok Crater:   ESP_026314_1985   ESP_026670_1985   (Interval in Earth days: 28)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
18.39

228.

-5.3

6.588

43.7

43.8

Dune Changes in North Polar Crater:   ESP_026404_2565   ESP_026457_2565   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
76.14

270.

13.7

-2.98

53.3

54.3

Bedrock Stratigraphy Exposed in Crater Wall:   ESP_026333_2015   ESP_026478_2015   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
21.35

68.7

0.94

15.99

42.4

41.5

Olympica Fossae:   ESP_026287_2050   ESP_025654_2050   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
24.58

245.

-11.

3.311

42.4

39.5

Craters and Mesas in Northeast Arabia Terra:   ESP_026254_2085   ESP_026399_2085   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
28.09

65.4

-7.4

6.562

41.3

40.5

Southern Ladon Basin near the Mouth of Ladon Valles:   ESP_026139_1600   ESP_027616_1600   (Interval in Earth days: 115)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-19.8

329.

5.17

-12.8

63.6

65.3

How Did Valles Marineris Form?:   ESP_025415_1675   ESP_026259_1675   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-12.3

294.

0

-17.9

53.1

60.5


  


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