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.

Eastern Side of Melas Region Basin with Light-Toned Layering:   ESP_012005_1700   ESP_012638_1700   (Interval in Earth days: 50)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.81

283.

1.82

-19.8

55.7

52.4

Iron and Magnesium Phyllosilicates in Terra Sabaea Crater Wall:   ESP_012278_1695   ESP_066132_1695   (Interval in Earth days: 4196)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-10.2

31.3

-3.6

-22.5

54.2

48.1

Streamlined Form and Channel Floor in Athabasca Valles:   ESP_011825_1895   ESP_012814_1895   (Interval in Earth days: 77)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
9.439

156.

-3.5

-16.8

59.8

59.0

Unusual and Pristine Crater Morphology:   ESP_011717_1910   ESP_012429_1910   (Interval in Earth days: 55)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
10.63

224.

-6.7

14.06

59.9

59.2

Light-Toned Outcrops:   ESP_011937_1970   ESP_012214_1970   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
16.73

337.

3.54

-22.5

61.9

64.8

Layered Deposit in an Arabia Region Crater:   ESP_012385_1825   ESP_030648_1825   (Interval in Earth days: 1423)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
2.668

350.

-23.

-0.71

58.9

50.7

Grand Canyon of Gale Crater:   ESP_012340_1750   ESP_012195_1750   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-5.18

137.

5.40

-12.9

54.3

56.5

Folded Layered Deposits:   ESP_012305_1865   ESP_012371_1865   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
6.390

11.8

1.20

-19.8

58.6

60.1

Oudemans Crater Central Uplift:   ESP_011676_1700   ESP_028449_1700   (Interval in Earth days: 1307)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.84

267.

-22.

7.568

59.1

56.2

Well-Preserved 6-Kilometer Diameter Impact Crater with Gullies:   ESP_012300_1440   ESP_020871_1440   (Interval in Earth days: 668)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-35.7

154.

-7.5

9.261

53.3

53.5


  


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