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.

South Polar Layered Deposits:   PSP_005011_0885   PSP_005023_0915   (Interval in Earth days: 1)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-88.4

191.

16.5

16.24

69.4

68.8

Light-Toned Layers in Crater South of Crommelin Crater:   PSP_003788_1820   ESP_020679_1820   (Interval in Earth days: 1316)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
2.194

351.

0

13.94

54.3

54.3

Pit Crater Chain in Cutting Lava Flow in Southwest Alba Patera:   PSP_003515_2155   PSP_004359_2155   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
35.08

240.

-1.9

-21.1

71.8

72.8

Fault in South Polar Layered Deposits:   PSP_004218_1070   PSP_005194_1070   (Interval in Earth days: 76)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-73.0

146.

-2.0

-23.4

56.0

60.0

Glacial-Like Fractures in Proposed Glacial Ice in Arsia Mons Depression:   PSP_004201_1735   PSP_005256_1735   (Interval in Earth days: 83)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-6.62

236.

8.32

-25.5

46.4

37.5

Odd Layered and Eroding Crater Fill in Deeply Eroded Craters:   PSP_003773_1630   PSP_003918_1630   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-16.8

42.7

1.82

18.06

48.1

45.3

Geologic Contact Between Wallrock and Light-Toned Layered Deposits:   PSP_004344_1715   PSP_005623_1715   (Interval in Earth days: 100)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-8.25

293.

-3.3

15.97

44.9

32.1

Rotational Landslides or Slumps along the Walls of Bahram Vallis:   PSP_003460_2015   PSP_003605_2015   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
21.26

303.

-1.0

12.74

64.0

63.4

Gullies:   PSP_003954_1445   PSP_004231_1445   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-34.9

144.

-5.8

-28.8

45.1

43.4

Fine Textures Near Headwaters of Warrego Valles:   PSP_003633_1385   PSP_004266_1385   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-41.1

267.

5.7

-9.82

49.8

42.3


  


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