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.

Gullies and Bedrock Exposures in Impact Crater Wall:   PSP_008153_1480   PSP_009155_1480   (Interval in Earth days: 78)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-31.4

337.

4.51

-12.3

70.8

76.3

Fresh Rayed Crater:   PSP_007707_1600   ESP_071927_1600   (Interval in Earth days: 5003)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-19.5

274.

-2.6

15.67

58.5

65.0

Lineated Valley Fill in Deuteronilus Mensae:   PSP_007795_2175   PSP_009588_2175   (Interval in Earth days: 140)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
37.35

24.6

-4.2

7.505

42.0

44.3

Central Peak of Large 40-Kilometer Diameter Crater:   PSP_007592_1995   ESP_045595_1995   (Interval in Earth days: 2961)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
19.25

169.

-0.9

19.06

40.8

43.5

Large Dunes Possibly of Aqueous Origin in Gale Crater:   PSP_007356_1750   PSP_008147_1750   (Interval in Earth days: 62)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-5.19

137.

-4.1

6.367

46.5

53.3

Blocky Deposit and Valley Networks Along Melas Chasma Wallrock:   PSP_007443_1705   PSP_007733_1705   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.17

282.

-9.1

5.346

49.8

52.0

Light-Toned Rock Exposures:   PSP_007101_1730   ESP_019311_1730   (Interval in Earth days: 952)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-6.99

260.

-7.9

3.361

44.7

56.7

Craters and Mounds in Utopia Planitia:   PSP_007081_2190   PSP_009876_2190   (Interval in Earth days: 218)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
38.57

80.3

0.48

17.95

44.1

45.1

Hellas Planitia:   PSP_007913_1370   ESP_016642_1370   (Interval in Earth days: 680)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-42.6

52.4

1.81

18.41

76.8

74.9

Unnamed Well-Preserved Crater in Terra Cimmeria:   PSP_007000_1475   PSP_007145_1475   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-32.0

141.

-1.0

10.11

57.0

58.6


  


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