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.

Central Structure of Large Crater in Northern Plains:   PSP_009332_2360   ESP_018048_2360   (Interval in Earth days: 679)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
55.61

171.

0

16.37

46.4

44.1

Bedrock Layers Exposed in Northern Hellas Basin:   PSP_009389_1510   PSP_010022_1510   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-28.8

67.0

0

-18.6

73.7

73.1

Fresh Santa Fe Crater in Chryse Planitia:   PSP_009749_1995   PSP_010382_1995   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
19.36

312.

3.75

-11.7

47.9

52.2

Look for Change Caused By Mass Wasting Since 2007:   PSP_009648_2650   PSP_010097_2650   (Interval in Earth days: 35)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.99

151.

2.16

-12.3

62.3

67.1

Head of Small Chasma on Edge of North Polar Layered Deposits:   PSP_010079_2625   PSP_010105_2625   (Interval in Earth days: 2)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
82.53

284.

-8.6

4.489

65.1

64.6

Landslide Deposit in Ophir Chasma:   PSP_009750_1760   PSP_009895_1760   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-3.80

288.

-4.3

12.25

58.0

56.8

High-Latitude Exposure of North Polar Layered Deposits:   PSP_010080_2680   PSP_010856_2720   (Interval in Earth days: 61)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
87.79

209.

-8.2

-6.88

68.7

80.5

Exposure of North Polar Basal Unit:   PSP_009945_2645   PSP_010063_2645   (Interval in Earth days: 9)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.40

343.

-12.

3.559

65.2

65.5

Western Rim and Ejecta of Very Young 12-Kilometer Diameter Crater:   PSP_009810_2140   PSP_010443_2140   (Interval in Earth days: 50)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
33.45

84.2

7.72

-5.93

45.6

51.8

Southern Highlands High Thermal Inertia and Spectrally Distinct Materials:   PSP_010326_1560   PSP_010471_1560   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-23.7

44.9

4.00

18.94

67.2

65.4


  


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