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.
| Mawrth Vallis Streamlined Islands: PSP_007968_2045 PSP_009972_2045 (Interval in Earth days: 156) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.33 | 341. | 3.52 | 19.63 | 41.2 | 46.4 |
| Flow-Banded Deformed Terrain of Hellas Basin Floor: PSP_007201_1405 PSP_007491_1405 (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 | -38.9 | 54.9 | -7.0 | 3.906 | 65.3 | 68.9 |
| Upper Section of Northern Olympus Mons Basal Scarp: PSP_007445_2035 PSP_008447_2035 (Interval in Earth days: 78) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.90 | 223. | -1.4 | -13.8 | 40.1 | 44.4 |
| Gullies Possibly Produced by Snow or Ice Melting: PSP_007270_2240 PSP_010487_2240 (Interval in Earth days: 251) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 43.42 | 319. | -2.8 | 11.76 | 45.5 | 52.4 |
| Light-Toned Tilted Layering in Central Peak of Oudemans Crater: PSP_007694_1700 ESP_027882_1700 (Interval in Earth days: 1574) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.92 | 268. | 1.09 | -17.4 | 52.3 | 59.3 |
| 3-Kilometer Diameter Crater with Good Bedrock Exposures in Upper Walls: PSP_007892_1865 ESP_079800_1865 (Interval in Earth days: 5603) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 6.625 | 259. | 4.25 | -7.35 | 45.6 | 54.0 |
| Clinoforms in Melas Chasma: PSP_007878_1700 PSP_008735_1700 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.75 | 283. | 4.89 | -23.0 | 53.8 | 61.4 |
| Western Rim and Ejecta of Largest Rayed Crater Known on Mars: PSP_007949_1970 ESP_024814_1970 (Interval in Earth days: 1315) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 16.90 | 141. | -0.8 | -28.1 | 42.9 | 39.9 |
| Small Fresh Primary or Large Secondary Crater From Gratteri Crater: PSP_007209_1565 PSP_008290_1565 (Interval in Earth days: 84) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.3 | 194. | -6.7 | 16.15 | 54.8 | 65.4 |
| Faults in Claritas Rupes: PSP_007655_1555 PSP_007945_1555 (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 | -24.3 | 255. | -0.5 | 14.07 | 61.0 | 63.3 |
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