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.

Fractured Lava Dome in Eastern Tharsis Region:   ESP_013904_1970   ESP_013970_1970   (Interval in Earth days: 6)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
16.62

275.

-4.7

-25.2

51.1

51.6

Possible Olivine-Rich Terrain in Ejecta of a Gullied Crater:   ESP_012761_1430   ESP_013117_1430   (Interval in Earth days: 28)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-36.8

167.

6.94

17.27

45.6

40.1

Comparative Gully Morphology:   ESP_013934_1335   ESP_014000_1335   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-46.0

183.

6.35

-11.3

40.0

41.5

Flood Lava Passing through a Constriction in Amazonis Planitia:   ESP_014184_2070   ESP_020276_2070   (Interval in Earth days: 475)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
26.88

190.

-8.6

13.66

54.9

58.4

3 Kilometer Diameter Crater on Edge of South Polar Layered Deposits:   ESP_013344_0990   ESP_013463_0990   (Interval in Earth days: 9)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-80.7

112.

-6.3

-22.2

60.8

62.4

Gullies in Dunes:   ESP_014151_1325   ESP_021509_1325   (Interval in Earth days: 573)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-47.1

19.5

5.65

-10.1

42.1

48.1

Crater between Branches of Athabasca Valles:   ESP_013460_1900   ESP_013737_1900   (Interval in Earth days: 21)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
9.648

157.

4.42

-23.9

51.5

50.0

Central Structure of Verlaine Crater:   ESP_013213_1705   ESP_013635_1705   (Interval in Earth days: 32)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.25

64.1

-1.2

-15.7

44.8

40.8

Enigmatic Crater Fill:   ESP_013055_1010   ESP_012818_1010   (Interval in Earth days: 18)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-78.8

68.2

20.0

-4.42

58.4

61.9

Columbus Crater Wall with Possible Kaolinite Exposure:   ESP_013327_1510   ESP_013960_1510   (Interval in Earth days: 50)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-28.8

193.

8.88

-14.5

38.1

35.7


  


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