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.

Interaction between Unnamed Crater Ejecta and Pre-Exsisting Terrain:   PSP_007681_2000   PSP_008406_2000   (Interval in Earth days: 57)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
19.66

259.

-6.6

23.65

41.5

41.9

Central Peak and South Rim of Large Fresh Crater in Isidis Basin:   PSP_007107_1900   PSP_009823_1900   (Interval in Earth days: 211)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
10.02

94.3

0.07

-12.8

39.2

52.4

Hellas Planitia:   PSP_007781_1410   PSP_008137_1410   (Interval in Earth days: 28)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-38.4

55.7

6.07

-3.19

72.0

76.2

Very Recent Small Crater in Dejnev Crater:   PSP_008145_1545   ESP_027067_1545   (Interval in Earth days: 1474)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-25.0

195.

-8.7

6.238

66.9

69.0

Inner Channel Deposit in Kasei Vallis:   PSP_007825_2010   ESP_035463_2010   (Interval in Earth days: 2153)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
20.84

287.

-3.9

12.13

41.7

43.8

Slope Streaks Beginning at Stratigraphic Layers:   PSP_007473_1850   PSP_008264_1850   (Interval in Earth days: 62)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
4.996

181.

-5.4

5.46

43.6

48.7

Thermally-Distinct Ridges Seen in THEMIS Images I09390002 and V24116005:   PSP_007838_1555   PSP_008840_1555   (Interval in Earth days: 78)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-24.0

297.

3.49

-19.3

62.6

70.9

Large Yardangs Cut by Smaller Yardangs:   PSP_007460_1675   ESP_060021_1675   (Interval in Earth days: 4096)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-12.5

177.

2.01

-13.6

51.1

45.6

Sample South Wall of Olympus Mons Caldera:   PSP_007023_1980   PSP_007168_1980   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.81

226.

-0.2

12.29

38.7

38.1

Small Fresh Primary or Large Secondary Crater From Gratteri Crater:   PSP_007209_1565   PSP_008290_1565   (Interval in Earth days: 84)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-23.3

194.

-6.7

16.15

54.8

65.4


  


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