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.

Heavily Pitted Streamlined Ejecta Lobe Originating from Mojave Crater:   ESP_020548_1875   ESP_028539_1875   (Interval in Earth days: 623)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
7.169

328.

-7.9

11.85

56.9

51.8

Crater Floors with Possible Clays:   ESP_020857_1440   ESP_065454_1440   (Interval in Earth days: 3475)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-35.7

177.

-2.3

-12.0

54.5

51.1

Ridges in Meridiani Planum:   ESP_020573_1805   ESP_021562_1805   (Interval in Earth days: 77)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
0.248

6.10

3.45

-11.8

54.8

52.5

Ejecta of Very Well-Preserved Crater:   ESP_020723_2235   ESP_064845_2235   (Interval in Earth days: 3438)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
43.26

225.

-4.6

28.28

72.1

71.8

Central Uplift in 20-Kilometer Diameter Crater:   ESP_020472_1475   ESP_068024_1475   (Interval in Earth days: 3705)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-32.3

247.

5.07

-11.7

58.2

51.4

Light-Toned Layering in Ladon Valles:   ESP_020759_1595   ESP_029238_1595   (Interval in Earth days: 660)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-20.3

329.

13.8

-4.99

52.3

56.2

Ridges in Meridiani Planum:   ESP_020560_1835   ESP_028551_1835   (Interval in Earth days: 623)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
3.475

0.44

5.90

25.06

55.1

51.1

Crater Fill Deposit:   ESP_020532_1465   ESP_020677_1465   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-33.1

50.6

-7.0

7.211

58.6

55.7

Possible Carbonate-Rich Terrain in Central Stucture of Leighton Crater:   ESP_020492_1830   ESP_021481_1830   (Interval in Earth days: 77)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
3.023

57.7

-3.5

-19.7

55.7

54.9

Finely Stratified Units in Northeast of Gale Crater with Possible Clays:   ESP_020555_1755   ESP_047139_1755   (Interval in Earth days: 2071)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-4.48

138.

3.93

24.21

54.3

49.2


  


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