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.

Very Bright and Sun-Facing Gully Deposits in Hale Crater:   ESP_014008_1430   ESP_014153_1430   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-36.4

322.

-1.9

12.21

36.7

36.3

Recent Gullies in a Crater in Noachis Terra:   ESP_013222_1410   ESP_013288_1410   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-38.8

182.

0.69

-18.8

40.4

41.3

Recent Gullies in Well-Preserved Crater:   ESP_013667_1345   ESP_013944_1345   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-45.2

274.

-4.5

-28.7

40.0

42.2

Landforms in Southern Tartarus Colles:   ESP_012642_1895   ESP_013710_1895   (Interval in Earth days: 83)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
9.266

170.

0.88

24.43

58.7

46.9

Well Preserved 20 Kilometer Diameter Impact Crater:   ESP_013684_1455   ESP_020910_1455   (Interval in Earth days: 563)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-34.0

168.

-2.8

19.71

36.4

51.7

Basal Exposure of South Polar Layered Deposits:   ESP_013857_1070   ESP_014015_1070   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-72.6

135.

-5.1

19.52

57.3

57.5

Central Structure of an Impact Crater in Terra Cimmeria:   ESP_013092_1630   ESP_013514_1630   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-16.8

129.

-6.4

-22.9

44.0

40.3

Layered Bedrock in Northeast Hellas Planitia:   ESP_013964_1490   ESP_020267_1490   (Interval in Earth days: 491)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-30.7

82.9

1.84

19.77

34.9

58.9

Steep Lobate Scarps in Kasei Valles:   ESP_012717_1910   ESP_013139_1910   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
10.88

282.

2.07

-8.93

59.1

56.6

Light-Toned Layered Material in Trough on North Melas Chasma Wall:   ESP_013495_1720   ESP_014128_1720   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-7.82

284.

6.24

-18.3

41.5

36.9


  


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