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.

Margin of Smooth Lobate Deposit in Nereidum Montes:   ESP_086259_1405   ESP_085824_1405   (Interval in Earth days: 34)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-39.1

321.

-1.8

-16.3

61.6

55.3

Mesa Stratigraphy at Terby Crater:   ESP_086268_1525   ESP_086835_1525   (Interval in Earth days: 44)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-27.1

73.7

3.54

-8.39

53.5

62.3

Layers in Crater in Northeast Sinus Meridiani:   ESP_086244_1805   ESP_086666_1805   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
0.362

5.66

2.87

-23.9

40.6

46.6

Hillslope Morphologies Southeast of Ostrov Crater:   ESP_086219_1520   ESP_085375_1520   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-27.5

332.

-6.1

8.78

53.6

40.3

Possible Thin Glacial Lobe in Young Crater:   ESP_086309_1490   ESP_086810_1490   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-30.4

35.6

-7.9

3.638

56.9

63.4

A Slice through the Layercake:   ESP_084979_1975   ESP_085045_1975   (Interval in Earth days: 6)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.49

336.

16.6

-4.34

44.6

45.3

Transverse Dunes West of Argyre Planitia:   ESP_085825_1300   ESP_085759_1300   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-49.8

294.

-2.2

12.44

61.9

59.9

Possible Esker in Phlegra Montes:   ESP_085948_2165   ESP_086673_2165   (Interval in Earth days: 56)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
36.15

164.

-8.9

24.11

48.0

41.2

Giant Polygon Terminus:   ESP_085849_2205   ESP_086996_2205   (Interval in Earth days: 90)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
39.92

346.

2.02

17.45

50.4

42.0

Diverse Materials in Western Jezero Crater Rim:   ESP_085714_1985   ESP_085859_1985   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
18.41

77.2

-23.

-5.54

42.3

40.4


  


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