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.

A North Polar Crater:   PSP_009689_2645   PSP_010084_2645   (Interval in Earth days: 31)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.33

120.

-1.7

12.07

62.3

65.3

High-Latitude Exposure of North Polar Layered Deposits:   PSP_009309_2725   PSP_009589_2675   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.52

327.

-4.7

-14.4

64.2

64.4

Basal Unit and North Polar Layered Deposits in Chasma Boreale Scarp:   PSP_009995_2650   PSP_010128_2650   (Interval in Earth days: 10)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
85.06

0.70

19.4

5.177

65.3

66.6

Fresh Irregular Crater in Tyrrhena Terra :   PSP_010113_1575   ESP_062503_1575   (Interval in Earth days: 4082)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-22.0

100.

-3.9

8.055

67.6

67.0

Survey Layering and Faulting in Layered Deposits in Candor Chasma:   PSP_009328_1755   PSP_010172_1755   (Interval in Earth days: 66)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-4.38

288.

5.36

-21.3

57.5

59.5

Possible Pingos in Gusev Crater:   PSP_009385_1655   PSP_009886_1655   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-14.2

175.

-18.

5.226

65.1

63.0

High-Latitude Exposure of North Polar Layered Deposits:   PSP_009584_2675   PSP_009757_2675   (Interval in Earth days: 13)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.31

77.4

-4.6

-21.6

64.0

65.8

North Polar Terrain:   PSP_009914_2750   PSP_010682_2650   (Interval in Earth days: 59)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.90

334.

0

18.02

69.7

73.7

Slope Streaks on Nicholson Crater Mound:   PSP_009371_1800   PSP_009516_1800   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-0.00

195.

-5.9

9.471

55.9

55.0

Western Half of Heimdal Crater:   PSP_009580_2485   PSP_009778_2485   (Interval in Earth days: 16)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
68.34

235.

4.49

-17.3

52.3

55.5


  


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