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.

Two Generations of Windblown Sediments:   ESP_033262_1725   ESP_033684_1725   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-7.28

264.

-8.9

-24.9

40.7

46.9

Terraced Craters and Layered Targets:   ESP_033014_2260   ESP_034082_2260   (Interval in Earth days: 84)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
45.64

188.

-8.0

6.102

52.5

43.4

Steep Inner Wall of Cone in Amenthes Region:   ESP_032859_1975   ESP_033070_1975   (Interval in Earth days: 17)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.12

103.

7.41

-6.07

37.0

37.7

Central Uplift of Impact Crater North of Eos Chasma:   ESP_032759_1685   ESP_032970_1685   (Interval in Earth days: 16)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-11.2

317.

1.86

-8.48

35.6

38.7

Fresh Shallow Valleys in Electris Region:   ESP_032580_1350   ESP_032725_1350   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-44.5

169.

-3.5

8.663

50.8

52.6

Rugged Banded Material in Crater in Northwest Hellas Planitia:   ESP_032769_1420   ESP_033191_1420   (Interval in Earth days: 33)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-37.7

47.8

-0.0

-19.1

49.1

57.3

Layered Materials on Northeast Hellas Region Rim:   ESP_032636_1525   ESP_032781_1525   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-27.3

78.1

-7.4

7.913

41.3

42.4

Bright Dunes in Syria Planum:   ESP_032814_1670   ESP_032880_1670   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-12.8

254.

22.5

-0.47

35.1

37.6

Light-Toned Deposits in Crater North of Eberswalde Crater:   ESP_032706_1575   ESP_040605_1575   (Interval in Earth days: 616)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-22.0

326.

-10.

4.419

39.8

33.3

Streamlined Forms in Athabasca Valles:   ESP_032699_1875   ESP_033200_1875   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
7.582

153.

-6.5

8.57

35.5

35.7


  


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