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.

Jezero Crater:   ESP_088707_1985   ESP_088773_1985   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
18.47

77.5

0.57

-21.6

47.7

49.7

Contact between Crater and Flood Lava:   ESP_088744_1845   ESP_089034_1845   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
4.224

148.

3.14

26.44

53.6

52.0

Ridged Flow-Like Features in Deuteronilus Mensae:   ESP_088445_2225   ESP_088511_2225   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
42.33

26.8

8.67

-8.24

42.8

44.5

Pitted Cones in Aurorae Chaos:   ESP_088540_1720   ESP_089107_1720   (Interval in Earth days: 44)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-7.77

320.

3.86

-8.75

60.1

60.9

Steep Sandy Slopes in Coprates Chasma:   ESP_088554_1660   ESP_088620_1660   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-13.7

298.

11.2

-14.2

63.4

65.0

Monitoring Gullied Crater:   ESP_088568_2310   ESP_088634_2310   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
50.71

266.

8.41

-6.17

44.4

45.9

Gullies on Western Wall of Nier Crater:   ESP_088574_2230   ESP_088640_2230   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
42.77

105.

-0.5

-17.0

44.0

45.8

Aeolis Dorsa Inverted Deposits:   ESP_088612_1735   ESP_088823_1735   (Interval in Earth days: 16)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-6.35

154.

-1.4

-14.9

59.6

60.6

North Polar Layered Deposits Structural Geology in Icy Layers:   ESP_088653_2625   ESP_088693_2625   (Interval in Earth days: 3)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
82.34

81.4

8.18

-8.30

58.5

59.6

Channel Entering Sklodowska Crater:   ESP_088512_2130   ESP_088578_2130   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
32.92

358.

15.6

-3.74

42.6

44.5


  


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