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.

Basal Unit and Dunes:   PSP_009913_2635   PSP_010019_2635   (Interval in Earth days: 9)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
83.51

118.

8.64

-5.81

63.1

64.9

Multiple Unconformities in the Upper North Polar Layered Deposits:   PSP_010181_2600   PSP_010234_2600   (Interval in Earth days: 4)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
79.74

23.4

-6.9

-18.7

64.6

66.2

Possible Intravalley Paleolake in Shalbatana Vallis:   PSP_009683_1830   PSP_010316_1830   (Interval in Earth days: 49)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
2.989

316.

-5.0

-21.7

54.6

56.7

Stratigraphy of Potential Crater Hydrothermal System:   PSP_010228_1490   ESP_016320_1490   (Interval in Earth days: 475)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-30.6

202.

-7.4

12.70

72.4

62.4

Exposure of North Polar Layered Deposits for Stratigraphic Analysis:   PSP_009999_2670   PSP_010132_2670   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
86.94

279.

-5.6

-20.5

67.0

69.1

Impact Crater on Lava Flow Front in Amazonis Planitia:   PSP_010109_1975   ESP_053848_1975   (Interval in Earth days: 3408)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
17.14

204.

-6.4

7.576

50.7

44.4

Junction of Three Polar Troughs:   PSP_010030_2670   PSP_010532_2670   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
86.74

162.

-8.8

-21.4

67.2

74.3

Graben in Memnonia Fossae:   PSP_010346_1570   PSP_010491_1570   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-23.0

219.

-5.8

9.284

67.3

65.6

Volcanic Fissure Vent in Elysium Planitia:   PSP_010269_1900   PSP_010414_1900   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
9.630

157.

-2.2

14.68

52.9

52.0

Stratigraphy of the North Polar Deposits:   PSP_010198_2645   PSP_010014_2645   (Interval in Earth days: 15)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
84.38

253.

7.14

-7.89

66.8

65.5


  


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