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.
| Loose Cluster of Zunil Crater Secondary Craters: PSP_003874_1815 PSP_004375_1815 (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 | 1.259 | 162. | 4.39 | 27.49 | 53.1 | 47.0 |
| Low Shield with Radial Flows East of the Olympica Fossae: PSP_003818_2040 PSP_004108_2040 (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 | 23.71 | 249. | -3.0 | 23.54 | 66.1 | 63.7 |
| Light-Toned Layering in Ius Chasma: PSP_003593_1725 ESP_058000_1725 (Interval in Earth days: 4239) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.48 | 275. | 4.77 | -11.1 | 51.7 | 34.5 |
| Gullies Produced by Possible Snow/Ice Melting: PSP_004192_2195 ESP_012446_2195 (Interval in Earth days: 643) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 38.96 | 116. | -0.0 | 13.62 | 75.6 | 74.8 |
| Glacial-Like Fractures in Proposed Glacial Ice in Arsia Mons Depression: PSP_004201_1735 PSP_005256_1735 (Interval in Earth days: 83) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.62 | 236. | 8.32 | -25.5 | 46.4 | 37.5 |
| Boulders on Lobate Ejecta: PSP_003484_1305 PSP_003563_1305 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -49.3 | 18.5 | -7.9 | 19.01 | 55.3 | 52.1 |
| Geologic Contact Between Wallrock and Light-Toned Layered Deposits: PSP_004344_1715 PSP_005623_1715 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.25 | 293. | -3.3 | 15.97 | 44.8 | 32.1 |
| Rotational Landslides or Slumps along the Walls of Bahram Vallis: PSP_003460_2015 PSP_003605_2015 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 21.26 | 303. | -1.0 | 12.74 | 64.1 | 63.5 |
| Phyllosilicate-Rich Area: PSP_004329_2045 ESP_013282_2045 (Interval in Earth days: 698) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.37 | 338. | -2.8 | -25.9 | 64.5 | 65.4 |
| Western Region of Zunil Crater: PSP_004309_1880 ESP_020211_1880 (Interval in Earth days: 1239) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 7.728 | 166. | 4.71 | 29.29 | 53.1 | 52.5 |
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