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.
| Sublimation Process / Spider Evolution: PSP_003312_0930 PSP_003325_0930 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -86.9 | 91.3 | 1.36 | 3.43 | 76.2 | 75.8 |
| Sample Gigas Fossae: PSP_003410_1840 PSP_003832_1840 (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 | 3.778 | 230. | 7.27 | -6.05 | 55.8 | 55.2 |
| Pit Crater Chain in Cutting Lava Flow in Southwest Alba Patera: PSP_003515_2155 PSP_004359_2155 (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 | 35.08 | 240. | -1.9 | -21.1 | 71.8 | 72.8 |
| Fault in South Polar Layered Deposits: PSP_004218_1070 PSP_005194_1070 (Interval in Earth days: 76) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -73.0 | 146. | -2.0 | -23.4 | 56.0 | 60.0 |
| Ridges East of the Nectaris Fossae: PSP_003948_1540 PSP_004370_1540 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -25.6 | 306. | 0.21 | -12.1 | 44.8 | 40.5 |
| Gullies and Mantling Material: PSP_004113_1425 PSP_005036_1425 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.1 | 123. | -5.9 | 7.401 | 43.2 | 35.4 |
| 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 |
| Gullies in Crater in South Aonia Terra : PSP_003698_1295 ESP_014009_1295 (Interval in Earth days: 804) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -50.0 | 294. | 5.99 | 23.69 | 51.1 | 41.4 |
| 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 | 44.9 | 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 | 64.0 | 63.4 |
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