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.
Exposure of Polar Layered Deposits: ESP_017937_2680 ESP_018162_2680 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.13 | 304. | -19. | -25.9 | 63.3 | 64.3 |
Lava in Olympus Mons Aureole: ESP_018033_2045 ESP_018323_2045 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.47 | 228. | 3.37 | 27.97 | 43.6 | 42.2 |
Mounds and Polygonal Features in Crater: ESP_018078_2445 ESP_018210_2445 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 64.31 | 70.3 | 10.5 | -7.11 | 48.1 | 50.0 |
Rampart Crater Sample: ESP_018010_2455 ESP_018656_2455 (Interval in Earth days: 51) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 65.42 | 128. | 2.96 | 17.4 | 49.0 | 51.6 |
Intact Stratigraphy in Crater Central Peak in Thaumasia Planum: ESP_018044_1540 ESP_018466_1540 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -25.7 | 295. | -3.9 | -17.4 | 71.1 | 71.3 |
Exposure of Polar Layered Deposits: ESP_018043_2715 ESP_018084_2685 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.51 | 196. | -13. | -12.9 | 64.5 | 63.9 |
Valley-Crater Intersection with Exposed Layers: ESP_018055_2120 ESP_018899_2120 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 31.60 | 346. | 3.16 | -20.2 | 42.5 | 48.6 |
Northern Hemisphere Gully Alcoves Seen in MOC Image R16-01542: ESP_017778_2200 ESP_018279_2200 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.87 | 349. | -7.4 | 8.255 | 42.5 | 42.6 |
Very Well-Preserved 10-Kilometer Diameter Impact Crater: ESP_017901_2375 ESP_017980_2375 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 57.35 | 225. | 8.89 | 25.25 | 44.9 | 43.6 |
Small Rayed Crater in Elysium Planitia: ESP_017785_1975 ESP_018418_1975 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.20 | 160. | 5.75 | -15.8 | 45.1 | 48.3 |
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