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.

Layered Deposits along Floor of Melas Chasma:   ESP_016673_1700   ESP_017952_1700   (Interval in Earth days: 100)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-9.67

284.

-5.2

5.092

53.8

59.7

Cone Field in Phlegra Dorsa:   ESP_016334_2090   ESP_016479_2090   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
28.57

174.

-6.3

7.838

40.7

39.6

Contact Between Different Lava Types on Olympus Mons:   ESP_016820_1950   ESP_017888_1950   (Interval in Earth days: 83)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
14.85

227.

-1.4

13.61

43.2

45.7

Collapse Features on Hrad Vallis Mudflow:   ESP_016467_2155   ESP_016533_2155   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
35.13

141.

0.42

-15.9

41.1

42.4

Relatively Fresh Crater Cut by Erosion:   ESP_016738_1730   ESP_019296_1730   (Interval in Earth days: 200)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-7.05

309.

-7.3

16.52

53.0

55.8

Source Region for Branch of Auqakuh Vallis:   ESP_016826_2080   ESP_016971_2080   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
27.47

62.7

-7.7

5.246

41.4

40.6

Very Recent Small Impact Crater:   ESP_016630_1720   ESP_030291_1720   (Interval in Earth days: 1064)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-8.08

17.6

-3.5

8.058

52.4

48.4

Small Volcano in Northern Syria Planum:   ESP_016318_1710   ESP_016951_1710   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-8.76

254.

6.70

-9.92

48.9

55.9

Isolated Layered Mound in Trough Between Layered Benches in Terby Crater:   ESP_016628_1520   ESP_016773_1520   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-27.6

74.4

0.18

16.62

64.9

65.4

Columnar Jointing in West Wall of Crater in Marte Vallis:   ESP_016360_2020   ESP_016505_2020   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
21.55

184.

7.23

21.49

39.4

38.5


  


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