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 MSL Landing Site in Gale Crater:   ESP_018854_1755   ESP_018920_1755   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-4.58

137.

5.54

-18.0

56.2

57.8

Pits North of Alba Patera:   ESP_018955_2310   ESP_018256_2310   (Interval in Earth days: 54)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
50.63

254.

-14.

11.85

51.4

43.8

Well-Preserved Crater Northeast of Hellas Planitia:   ESP_019120_1585   ESP_027678_1585   (Interval in Earth days: 667)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-21.2

77.3

3.42

-7.57

64.5

65.6

Cerberus Fossae near Head of Athabasca Valles:   ESP_018985_1900   ESP_019618_1900   (Interval in Earth days: 50)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
9.954

157.

17.7

-2.49

49.1

52.8

Steep North Polar Boundary Scarp:   ESP_018928_2640   ESP_019034_2640   (Interval in Earth days: 8)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
83.79

237.

7.24

-7.09

65.4

67.3

Abrupt Transition in Expression of North Polar Basal Stratigraphy:   ESP_018898_2645   ESP_019215_2645   (Interval in Earth days: 24)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.25

342.

0

-13.9

65.7

70.4

Possible Fluvial Features in West Hellas Planitia:   ESP_019042_1450   ESP_019187_1450   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-34.8

48.5

4.88

17.60

73.2

71.3

Thermally-Distinct Material at Distal Coogoon Valles:   ESP_019084_1980   ESP_060437_1980   (Interval in Earth days: 3222)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.85

336.

-5.5

5.547

49.5

37.7

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

North Polar Trough Stratigraphy:   ESP_019102_2660   ESP_018496_2660   (Interval in Earth days: 47)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
85.86

179.

-12.

-22.1

69.8

64.4


  


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